chang

含义不同 1.exchange:释义：n.交换，互换，交流，掉换，交谈。 2.change:释义：n.改变，变化，变更，变革。 扩展资料 　　用法不同: 　　1.exchange:用法：exchange的基本意思是“交换”,可以表示以贸易手段以一物换取另一物; 　　也可指一般的.一物与另一物相交换; 　　有时还指在两个或更多人之间换东西。引申可表示“交流”经验、思想等。 　　例句：We exchanged addresses and Christmas cards.我们交换了地址和圣诞贺卡。 　　2.change:用法：change的基本意思是使事物变得与以往不同,指事物发生了本质的变化或指一事物取代了另一事物。 　　例句：The ambassador appealed for a change in US policy.大使呼吁美国在政策上作出改变。 　　侧重点不同: 　　1.exchange:解析：exchange我给你A你给我B。 　　2.change:解析：change没有交换的意思换车是指你一开始称一号线到某站换二号线吧。

exchange 是交换改变的意思，必须有两个主体，一般用在交易东西change没这种要求，更广一些

he is a exchange student

改期的话，只要不是特价票是就可以。

转换，变换

不能 在这里 exchanged 是作为形容词出现，形容student，exchange为动词或名词，这里不能用

exchange用作动词，既可用作及物动词，也可用作不及物动词，表示交换，兑换等含义。用作名词时表示交易所，兑换等含义。1.exchange的基本含义是“交换”,可以表示以贸易手段以一物换取另一物; 也可指一般的一物与另一物相交换; 有时还指在两个或更多人之间换东西。引申可表示“交流”经验、思想等。 2.exchange既可用作不及物动词,也可用作及物动词。 （1）用作及物动词时,接名词或代词作宾语,且所接的名词一般为复数。 They exchanged addresses.他们交换了地址。 You two boys exchange places.你们两个孩子交换一下位置。 （2）用作不及物动词 This currency exchanges at par.这货币平价兑换。 3.exchange宾语后常接介词for,表示“以…换取”; 接介词with表示“与某人交换(某物)”。 4.exchange后可接单数或是复数，一般在行动上，会有单数形式出现。 They exchanged caps.他们俩交换帽子。 They exchanged a smile.他们俩交换笑容。 5.exchange for (v.+prep.)用…换取 I"d like to exchange a watch for a camera. 我想用表换相机。 She exchanged honour for wealth. 她牺牲荣誉以换取财富。 6.exchange with (v.+prep.) 与(某人)交换… They exchanged hostages with each other. 他们彼此交换了人质。 Tom exchanged gifts with John at Christmas. 汤姆与约翰在圣诞节交换礼物。

to

exchange用作动词，既可用作及物动词，也可用作不及物动词，表示交换，兑换等含义。用作名词时表示交易所，兑换等含义。1.exchange的基本含义是“交换”,可以表示以贸易手段以一物换取另一物; 也可指一般的一物与另一物相交换; 有时还指在两个或更多人之间换东西。引申可表示“交流”经验、思想等。 2.exchange既可用作不及物动词,也可用作及物动词。 （1）用作及物动词时,接名词或代词作宾语,且所接的名词一般为复数。 They exchanged addresses.他们交换了地址。 You two boys exchange places.你们两个孩子交换一下位置。 （2）用作不及物动词 This currency exchanges at par.这货币平价兑换。 3.exchange宾语后常接介词for,表示“以…换取”; 接介词with表示“与某人交换(某物)”。 4.exchange后可接单数或是复数，一般在行动上，会有单数形式出现。 They exchanged caps.他们俩交换帽子。 They exchanged a smile.他们俩交换笑容。 5.exchange for (v.+prep.)用…换取 I"d like to exchange a watch for a camera. 我想用表换相机。 She exchanged honour for wealth. 她牺牲荣誉以换取财富。 6.exchange with (v.+prep.) 与(某人)交换… They exchanged hostages with each other. 他们彼此交换了人质。 Tom exchanged gifts with John at Christmas. 汤姆与约翰在圣诞节交换礼物。

1、exchange的意思：n.交换; 互换; 交流; 掉换; 交谈; 对话; 争论; 兑换; 汇兑; 交流，互访; 交易所;vt.交换; 交流; 掉换; 兑换; 交易; 更换; 交换(尤指房屋或土地买卖的契约); 2、exchange的读音：英[ɪksˈtʃeɪndʒ]美[ɪksˈtʃeɪndʒ] 3、第三人称单数：exchanges 复数：exchanges 现在分词：exchanging 过去式：exchanged 过去分词：exchanged

ex+change，望采纳

exchange 英 [ɪks"tʃeɪndʒ; eks-] 美 [ɪks"tʃendʒ] n. 交换；交流；交易所；兑换vt. 交换；交易；兑换vi. 交换；交易；兑换

exchange 英 [ɪksˈtʃeɪndʒ] 美 [ɪksˈtʃendʒ] n. 交换; 交易所; 交易; 兑换（率）; vt. 兑换; 交换，互换; 交换，调换; vi. 交换，替换; 进行易货贸易，作物物交换; [金融业] （货币） 交换，兑换; [例句]We exchanged addresses and Christmas cards.我们交换了地址和圣诞贺卡。[其他] 第三人称单数：exchanges 复数：exchanges 现在分词：exchanging 过去式：exchanged 过去分词：exchanged

Exchange [iks"tʃeindʒ] 如果要我用中文标，那就是“一可是前几”（无奈啊，这种方法N久没用了，怕你不会音标，所以还是写了）

exchange英[ɪksˈtʃeɪndʒ]美[ɪksˈtʃendʒ]n.交换; 交易所; 交易; 兑换（率）vt.兑换; 交换，互换; 交换，调换vi.交换，替换; 进行易货贸易，作物物交换; [金融业]（货币）交换，兑换网络邮件服务器; 货币兑换; 汇票第三人称单数：exchanges复数：exchanges现在分词：exchanging过去式：exchanged过去分词：exchanged形近词：Exchangesexchangesexchangeintrachange数据来源：金山词霸双语例句柯林斯词典英英释义百度百科百度知道新1Free exchange of goods was advantageous to all.商品自由交换惠泽八方。

n.交换；交流；交易所；兑换vt.交换；交易；兑换vi.交换；交易；兑换专业用法： 交易[经] ; 交换[计] ; 互通[法]过去式exchanged过去分词exchanged现在分词exchanging复数exchanges第三人称单数exchanges

楼上的 人家问的是怎么读 复制啥百度翻译。。。怎么读是吧 听好了~“诶克斯趁治”

英:[ɪksˈtʃeɪndʒ]美:[ɪksˈtʃendʒ]释义：n. 交换;交易;交易所;兑换（率）vt. 交换，互换;兑换;交换，调换vi. 交换，替换;进行易货贸易，作物物交换;[金融业]（货币）交换，兑换变形：复数. exchanges第三人称单数. exchanges过去式. exchanged过去分词. exchanged现在分词. exchanging短语：exchange contracts(英)（买方）与财产或土地的卖方签订合同以使交易具有法律效力in exchange作为交换

表示一种状态。。。

作名词时译为“交换；交流；交易所；兑换”，作动词时译为“交换；交易；兑换”。exchange 变化形式：复数： exchanges第三人称单数： exchanges过去式： exchanged过去分词： exchanged现在分词： exchangingexchange 用法和例句：Knowledge exchange is never a one-way street .交流知识绝不是一条单行道。Thain forced the exchange to embrace electronic trading .塞恩迫使该交易所采取电子交易系统。So exchange groups must look elsewhere for their rewards .因此交易所集团必须从其它地方寻找回报。The columbian exchange continues to this day .哥伦布大交换现今仍在继续着。But he declined to characterize the exchange .但是，洛文杰决绝就汇率问题做出评价。

　　exchange英 [ɪksˈtʃeɪndʒ] 美 [ɪksˈtʃendʒ]　　n.交换; 交易所; 交易; 兑换(率)　　vt.兑换; 交换，互换; 交换，调换;　　vi.交换，替换; 进行易货贸易，作物物交换; [金融业] (货币) 交换，兑换;　　[例句]Free exchange of goods was advantageous to all.　　商品自由交换惠泽八方。　　[其他]第三人称单数：exchanges 复数：exchanges 现在分词：exchanging 过去式：exchanged 过去分词：exchanged 形近词： sexchange sexchange intrachange

exchange的过去式和过去分词 事物或者货币的已经交换或者已经兑换等

exchange[英][ɪks"tʃeɪndʒ][美][ɪksˈtʃendʒ]n.交换; 交易; 交易所; 兑换（率）; vt.交换，互换; 兑换; 交换，调换; vi.交换，替换; 进行易货贸易，作物物交换; [金融业]（货币）交换，兑换; 第三人称单数：exchanges过去分词：exchanged复数：exchanges现在进行时：exchanging过去式：exchanged~如果你认可我的回答，请及时点击【采纳为满意回答】按钮~~手机提问的朋友在客户端右上角评价点【满意】即可。~你的采纳是我前进的动力~~O(∩_∩)O，互相帮助，祝共同进步！

proposed-changes拟议中的变化.很高兴为你解答！如有不懂，请追问。 谢谢！

Great changes have （been去掉） taken place in our school。When entering the school，you （will）see a big garden in middle of it，with rows of trees anywhere（改为everywhere）。And there are buildings for teaching，experimenrs and dormitories，that（改为which） are all equipped with the most advanced equipment。After class，we also do some sports in the newly（改为new） stadium or on the playground。Every moring，the loud voice of reading book（改为books） can be heard in the school。What"s more，students can be seen together discussing some learning problems or exchange ideas.So（改为but） what appeals to（去掉） us most is the smiling faces in(改为of) teachers and students.We are living like members of a big family.In a word,I enjoyed(改为enjoy) my school life so much共十处，修改的内容在括号中，供参考。

有两点不同1 change 可以重命名列名，也可能修改列的数据类型，而modify只能修改列的数据类型。2 两者写法不同,举例:--changeALTER TABLE t1 CHANGE b a BIGINT NOT NULL;--如果只需要修改类型ALTER TABLE t1 CHANGE b b BIGINT NOT NULL;--modifyALTER TABLE t1 MODIFY b BIGINT NOT NULL;

比较明显的区别：如果是只改变列的类型不改变名称时，用change为ALTER TABLE t1 CHANGE b b BIGINT NOT NULL;用modify 为alter table t1 modify b bingint not null;　－－不需要写两个相同的列名当需要修改字段名称时使用change；当需要修改字段类型时使用modify，毕竟modify还是比change少写个字段名称的，因次还是比较节约系统资源的额 ^_^

将表格修改为下面第二个表格形式。 用一条ALTER语句实现。 CHANGE:如果我们不只是修改单一列，而是用一条语句改变两个列，我们需要修改列的名称，同时更改他们的数据类型，这时就需要我们用到关键字CHANGE,可以在一条语句中放入多个CHANGE,在中间加上分隔的逗号即可。 比如原来的表两列，类型为VARCHAR(50),和VARCHAR(10),现在不止要更改列名，还要更改这两列的类型。 程序如下： MODIFY:使用它可以只修改列的类型而不会干涉它的名称，假设要把proj_desc列的字符长度修改为VARCHAR(120)以容纳更多的说明文字，只要这么做就可以。 总结如下; (1)既更改列名也更改类型，用CHANGE (2)只修改类型，用MODIFY,但这种方法比较慢，我们用另一种方法直接修改.frm文件，而不改动表本身。

change, alter, vary, convert, modify, transform, turn这些动词均含有"变化，改变"之意。change: 指任何变化，完全改变，强调与原先的情况有明显的不同。alter: 常指轻微的改变，强调基本上保持原物、原状的情况下所进行的部分改变。vary: 暗示不规则或断断续续地变。convert: 指进行全部或局部改变以适应新的功能或用途。指信仰或态度时，强调较激烈、大的改变。modify: 强调起限定作用的变化或变更。指细小的变化，常含"缓和、降调"的意味。transform: 指人或物在形状、外观、形式、性质等方面发生的彻底变化，失去原状成为全新的东西。turn: 指外形、颜色、气味、性质等方面的变化，比change更通俗。

change意为改变,modify意为修改简单地说,change 可以将这个字段名字 属性 和 注释全给改了而modify不可以改字段名字例如:alter table test change id changeid int;上面是将id字段名改为changeid,类型改为int型alter table test modify id int;上面将id的类型改为int型,却无法修改id的名字

modify

大无缝

change：不管要修改的是类型还是字段名都必须把字段名列出来，比如：ALTER TABLE t1 CHANGE b b BIGINT NOT NULL; 用modify的话直接是 alter table t1 modify b bigint not null;

　　CHANGE 对列进行重命名或更改列的类型，需给定旧的列名称和新的列名称、当前的类型MODIFY 可以改变列的类型，此时不需要重命名（不需给定新的列名称）

convert ，change ，modify， transform ，alter的区别为意思不同、用法不同、侧重点不同，用法如下：一、意思不同1、convert：(使)转变，转换，转化，可转变为，可变换成。2、change：改变，变化，使不同，(使)变换。3、modify：调整，稍作修改，使更适合。4、transform：使改变形态，使改变外观(或性质)，使改观。5、alter：(使)改变，更改，改动。二、用法不同1、convert：常表示局部或表面的改变或变动，改变的范围或程度较小，而本质特性并未发生变化。2、change：change可用作不及物动词，也可用作及物动词。用作及物动词时，接名词或代词作宾语，可用于被动结构，用作不及物动词时，可表示“改变，换衣，换车”。3、modify：modify引申可表示“修饰”“限定”，尤指形容词或副词修饰另一词或限定另一词的意义。4、transform：transform一般用作及物动词接名词或代词作宾语。transform后接介词to或into表示“把?转变成?”，这时可省略用作宾语的oneself，而用作及物动词。5、alter：alter可用作不及物动词，也可用作及物动词，用作及物动词时，接名词或代词作宾语。三、侧重点不同1、convert：指为了能适应新的用途或目的而改变某物的状态、形态、特性等。2、change：指不规则的变化或断断续续的改变。3、modify：使用较为广泛，可指改变意见、计划、结构、体系、方法、内容等。4、transform：指事物的面貌、功能或性质发生深刻的变化，失去原状成为全新的东西。5、alter：指部分更改，仍保留本质和总体结构。

Many persons want to change the world, but from my perspective, if we don"t learn to change ourselves, how can we change the world.There are many things that need to be changed and progressed. Unchangeable life is just like a pool of dead water. Learning to change helps us to create a progressing and fresh life. Only by changing can we correct our weaknesses and perfect ourselves. Only by changing can we transform our attitude and see the beautiful side. Only by changing can we live a brand-new life and take another rhythm. It is changing that makes us become excellent persons. So please learn to change, to change the present situation and perfect yourself. In this way, you will have a better life and our world will be more beautiful.If you often throw away rubbish freely. Please change it and form good habits. then you will find the defects are fading, and you are going to be an polite person. our environment will be much cleaner.If you often argue with others about some little things, please change your attitude and make another thought, you will get different understanding and acquirement. And because of your changes, our world will become more harmonious.If you are tired of the present lifestyle, just change it and live another rhythm life. You can experiment with new ways of thinking and acting, complete tasks that are relaxing and educational. You will find a brand-new and meaningful life. At the same time, our world will be more beautiful.So my dear friends, never complain that life is boring and the world is disappointing. If you don"t like the taste of your life, just change it. If you want to change the world, please change yourself. Conquer your limitations and embrace new challenges. Maybe you will see a different sky.

参考mysql5.5手册，可以使用CHANGE old_col_name column_definition子句对列进行重命名。重命名时，需给定旧的和新的列名称和列当前的类型。事例：例如：要把一个INTEGER列的名称从a变更到b，您需要如下操作：mysql> ALTER TABLE t1 CHANGE a b INTEGER;如果您想要更改列的类型而不是名称， CHANGE语法仍然要求旧的和新的列名称，即使旧的和新的列名称是一样的。例如：mysql> ALTER TABLE t1 CHANGE b b BIGINT NOT NULL;您也可以使用MODIFY来改变列的类型，此时不需要重命名：mysql> ALTER TABLE t1 MODIFY b BIGINT NOT NULL;关于何时使用change，何时使用modify，其实都是无可厚非的，最主要是个人的习惯。当需要修改字段名称时使用change；当需要修改字段类型时使用modify，毕竟modify还是比change少写个字段名称的，因次还是比较节约系统资源

change,alter,vary,convert,modify,transform,turn这些动词均含有"变化，改变"之意。change:指任何变化，完全改变，强调与原先的情况有明显的不同。alter:常指轻微的改变，强调基本上保持原物、原状的情况下所进行的部分改变。vary:暗示不规则或断断续续地变。convert:指进行全部或局部改变以适应新的功能或用途。指信仰或态度时，强调较激烈、大的改变。modify:强调起限定作用的变化或变更。指细小的变化，常含"缓和、降调"的意味。transform:指人或物在形状、外观、形式、性质等方面发生的彻底变化，失去原状成为全新的东西。turn:指外形、颜色、气味、性质等方面的变化，比change更通俗。

这五个动词都含“改变”的意思：1、alter 指部分更改，仍保留本质和总体结构，其名词是 alteration。（ 1）The sleeves of the shirt are a bit too long. I"ll have to ask the tailor to alter them.这件衬衫的袖子太有长了点。我得请裁缝改改。（ 2）While frictions may cool their relationship, they will not alter the basic nature of their cooperation.尽管摩擦也许使他们的关系降温，但不会改变他们之间合作的基本性质。（3）In doing translation, one should not alter the meaning of the original to suit one" own taste.翻译时不应根据自己的好恶改变原文的意思.（4）The fact that she had become wealthy did not tempt her to alter her frugal way of life.她有钱了，可这丝毫没能让她改变节俭的生活习惯。（5）It is human nature that people don"t like anything that will causealterations in their lifestyle.这是人类的本性,人们不喜欢导致他们的生活方式改变任何事物。（6）Some alterations to our original plans might be necessary.可能需要的我们原计划作一些修改。2、vary 指不规则的变化或断断续续的改变，其名词是 variation。（1）The doses used for surgical anaesthesia vary between 2 and 10 mg / kg. 外科手术麻醉药的用量从每公斤2毫克到10毫克不等。（2）The nature of these ties must vary withthe different problems of different areas. 这一些结合的性质必须视不同地区的不同问题而有所变化。（3）As opinions vary on that point, no decision can be reached. 在那一点上, 大家意见纷纷，莫衷一是。（4）Estimates of risk aversion vary widely, and no quantitative guidelines are available. 对于风险的躲避的估算具有很大的差异, 而且也没有适用的数量指标。（5）It is difficult to describe the climate of England because the variations are so frequent and unpredictable.很难描述英格兰的气候,因为其变化频繁难以预测。（6）Currency exchange rates are always subject to variation.货币兑换率是经常变的。3、convert 指为了能适应新的用途或目的而改变某物的状态、形态、特性等，常用结构是 convert …… into ……. 名词形式是 conversion。（1）The solar cell can convert the energy of sunlight into electric energy.太阳能电池能把阳光的能量转化为电能。（2）Internal combustion engines convert the energy in gasoline"s molecular bonds into motion.内燃机的工作原理是将汽油中分子团的能量转化为动能。（3）What"s the formula for converting pounds into kilos?英镑转换成公斤的公式是什么?（4）They have converted the barn into an exhibiting hall.他们把仓库转换成一个展览大厅。（5）Now there is a large team of experts who devote themselves to the research on the conversion of water into fuel, which is obviously a complicated problem.现在有一大批专家致力于研究将水转换成燃料,这些显然是一个复杂的问题。（6）You may need this exchange memo for convertion when you leave America. 离开美国需要兑换时，你可能用得着这个兑换证书。4、modify 使用较为广泛，可指改变意见、计划、结构、体系、方法、内容等，其名词是 modification。（1）The Industrial Revolution modified the whole structure of the English society.工业革命变革了英国社会的整个结构。（2）And you must modify it all times, and add new code in it.你需要随时的它进行修改，添加新的代码。（3）Instead of simply punishing them, the system encourages offenders to modify their behaviour.这种体系不是简单地惩罚罪犯，而是鼓励他们改变自己的行为。（ 4）We have to modify our plan a little bit. 我们得对我们的计划稍加修改.（5）The architects made some modifications in the structure of the designed building.建筑师对设计好的大楼结构作了一些更改。（6）Modification of the engine to run on lead-free fuel is fairly simple.将发动改用无铅燃料是相当简单的。5、transform 指事物的面貌、功能或性质发生深刻的变化，失去原状成为全新的东西。其名词是transformation。（1）My hometown has tansformed into a modern town.我的家乡现在已经变成一个现代化的城镇。（2）After the Wilson family moved in, the eight children helped transform the neighborhood from dull to lively.威尔逊一家搬来后,他家8个孩子使原本死气沉沉街坊变得生气活泼。（3）A little paint will soon transform this old car. 只要喷上一点油漆就会马上使这部旧车变个模样。（4）We have transformed the hills nearby the village by afforestation. 通过治山造林我们已经改变了周围的山丘的面貌。（5）Going to college brought about a dramatic transformation in her outlook. 上大学使她的观念发生了巨大的变化。（6）But the breadth ofthe economic transformation can"t be measured by numbers alone. 巨大经济变化的程度单凭数据是不能衡量的。

歌曲名：《Try To Change》歌手：Mother Mother专辑：《O My Heart》发行时间：2010-04-19 流派：摇滚 发行公司：华纳音乐歌词：Try to change..I try to change..I make a list of all the ways to change my ways.But I stay the same,I stay the s-ame.Ohh..I will try and try to change but I just stay the same.Stay the same,I stay the same.In a decadent age I try to changeall my decadent ways but I just can"t help butstay the same.In a decadent age.Ohh..I will try and try to change but I just stay the same.The same..The same..The same..The same..Carry a cane.I carry a cane."cause I tried to changeand I tried too hardso I hurt my leg and well, overallI just stayed the same.Now I carry a cane.Ohh..I will try and try to changebut the list I made of changes to make,it bleww awaayy..blew away..blew away..blew away..Try to change,Try to change,I try to change,Try to change,Everybody be tryin" to change,tryin" to change,I try to change,I try, it"s safe to say, someDon"t change

6.删除改变“密码”选项 该策略可以防止用户通过任务管理器更改系统密码。 删除改变“密码”选项 该策略可以防止用户通过任务管理器更改系统密码位置：用户配置管理模板系统Ctrl+Alt+Del选项 这个设置停用Windows安全设置对话框上的“更改密码”按钮。但是，用户在得到系统提示时依旧可以更改密码。管理员要求新密码和密码作废时，系统会提示用户输入新密码。

Amid主语profound谓语changes of the international宾语

change和cancellations的区别change 是动词和名词vt.改变，变更;交换，替换;兑换;换衣服（床单）vi.改变，转变;交换，互换;换衣，更衣n.变化，改变;交换，交替;零钱，找头;代替物cancellation 是名词n. 取消; <数>（相）约; 被取消的事物; 作废;

bargain是讨价还价,exchange是交易,trade 是大宗贸易

中文歌词

在SAP中，某些业务对象会有状态的属性，用来控制和约束该业务当前的操作。比如PM模块的工单和PS模块的项目定义，状态这个属性并不存放在各个业务的业务表中，而是由SAP统一管理。【系统状态】 以I开头，主数据表是TJ02，描述表TJ02T 表TJ04可以据业务对象号(如WBS是PRN)，可以查出所有相关的状态【用户状态】 以E开头，每个用户状态都关联一个用户参数文件，相同的状态编码在不用的参数文件下意义不用， 主数据表为TJ30, 文本表是TJ30T 对于每笔业务，都有一个唯一的对象编号，字段名一般为OBJNR，存在在业务表中(AUFK, PROJ...) JEST：存放了该对象编号的当前状态 JCDS：存在对象状态修改的历史记录Function module： STATUS_READ 读出某个业务对象的当前状态(注意包括业务进行中BUFFER的状态) STATUS_UPDATE 修改状态(批量新增或者修改状态) I_CHANGE_STATUS 状态更新(取消一个当前状态，激活一个新的状态)补充一点，还有一个取项目的状态描述的FUNCTION是：STATUS_TEXT_EDIT在【ABAP】项目相关开发中的一些经验总结里有详细的用法介绍。

Hi,to change the billing plan for a position, we have used the following functionmodules:1. "SD_SALES_DOCUMENT_READ" - Reads the contract. 2. "SD_SALES_BILLINGPLAN_READ" - Reads the billing plan for a position 3. "SD_SALES_BILLINGPLAN_CHANGE" - Updates the billing plan. 4. "SD_SALES_DOCUMENT_SAVE" - Saves the contract 5. "BAPI_TRANSACTION_COMMIT" - commits changes to the database. Check the function modules in function group V45A for other functionality! I hope this will help you to find a solution! RegardsMichael Pedersen 到思互圈子网站查看回答详情>>

这个可以使用第三方接口T4S

创建计划单的BAPI没问题BAPI_PLANNEDORDER_CREATE为什么修改BAPI的就有问题呢？有用过的出来解答一下，谢谢了！！

歌曲名:Change Partners歌手:Ella Fitzgerald专辑:The Very Best Of The Irving Berlin Songbookwe were waltzin togetherto a dreamy melodywhen they called out "change partners"and you waltzed away from menow my arms feel so emptyas i gaze around the floorand ill keep on changing partnerstill i hold you once morethough we danced for one momentand too soon we had to partin that wonderful momentsomethin happened to my heartso ill keep changing partnerstill youre in my arms and thenoh, my darlin i will neverchange partners againthough we danced for one momentand too soon we had to partin that wonderful momentsomethin happened to my heartso ill keep changing partnerstill youre in my arms and thenoh, my darlin i will neverchange partners again陈永超谢谢http://music.baidu.com/song/7652870

歌曲名:Changing Partners歌手:Patti Page专辑:Patti Page"s Greatest HitsChanging PartnerWe were waltzing togetherto a dreamy melodyWhen they called out "Change partner!"And you waltz away from meNow my arms feel so emptyAs I gazed around the floorAnd I keep on changing partnersTill I hold you once moreThough we danced for one momentAnd too soon we had to partIn that wonderful momentSomething happened to my heartSo I keep changing partnersTill you"re in my arms, and thenOh my daringI will never change partner againMusic...Though we danced for one momentAnd too soon we had to partIn that wonderful momentSomething happened to my heartSo I keep changing partnersTill you"re in my arms, and thenOh my daringI will never change partner againhttp://music.baidu.com/song/31408838

英文歌曲：Changing Partners 歌词 We were waltzing together to a dreamy melodyWhen they called out "Change Partners."And you waltzed away from me.Now my arms feel so empty,As I gaze around the floor.And I"ll keep on changing partners,Till I hold you once more! Though we danced for one moment,And too soon we had to part. In that wonderful momentsomething happened to my heart!So I"ll keep changing partnerstill you"re in my arms and then, Oh! My darling I will never change partners again.(Repeat) 歌词大意 伴着如梦的旋律，我们相拥而舞。他们喊“交换舞伴”，你迈着舞步离我而去。我盯着地板，双臂失去了依托。于是我不停地交换舞伴，直到我们再度相逢。虽然我们只能共舞片刻，马上又要分离，但就在那美妙的一瞬，你已深深进入我的心中。于是我继续交换舞伴，直到再次被你拥入怀中。哦，我的舞伴将不再与人交换。

歌曲名:Changing Partners歌手:Kay Starr专辑:Capitol Collectors SeriesChanging PartnerEdit By Jude yuWe were waltzing togetherto a dreamy melodyWhen they called out "Change partner!"And you waltz away from meNow my arms feel so emptyAs I gazed around the floorAnd I keep on changing partnersTill I hold you once moreThough we danced for one momentAnd too soon we had to partIn that wonderful momentSomething happened to my heartSo I keep changing partnersTill you"re in my arms, and thenOh my daringI will never change partners againMusic...We were waltzing togetherto a dreamy melodyWhen they called out "Change partner!"And you waltz away from meNow my arms feel so emptyAs I gazed around the floorAnd I keep on changing partnersTill I hold you once moreThough we danced for one momentAnd too soon we had to partIn that wonderful momentSomething happened to my heartSo I keep changing partnersTill you"re in my arms, and thenOh my daringI will never change partners againOh my daringI will never change partners againhttp://music.baidu.com/song/2926207

　　《Change Partners》　　所属专辑：Come by Me　　演唱者：Harry Connick, Jr.　　作曲：Berlin　　歌曲时长：05:43　　具体歌词：　　Must you dance every dance　　With the same fortunate　　man　　You have danced with him since the music began　　Why don"t you change　　partners and dance with me　　Must you stand quite so close　　With your　　lips touching his face　　Can"t you see I"m longing to be in his place　　Why　　don"t you change partners and dance with me　　Ask him to sit this one　　out　　And while you"re alone　　I"ll tell the waiter to tell him　　He"s wanted　　on the telephone　　You"ve been locked in his arms　　Ever since heaven　　knows when　　Why don"t you change partners and then　　You may never want to　　change partners again

原句的意思是：你已经适应了变化了吗? 再帮你举几个例子： 1. You must accustom yourself to getting up early. 你必须使自己习惯于早起。 2. He had to accustom himself to the cold weather. 他不得不使自己习惯于寒冷的天气。 3. He soon gets accustom to dormitory life and make two or three friend. 他不久就逐渐习惯了宿舍的生活并交了两三个朋友。

CHANGETOAUTHORLIST的意思改变作者列表例句:1.Istoauthoraconspiracytheorywithoutbackground.就是报导一篇没有背景的阴谋。2.Moisnotthefirstchineseauthortogetthenobelnod.莫言并不是第一个获得诺贝尔文学奖的中国作家。3.Rosetremainisadifficultauthortopigeonhole.萝丝崔梅是一位难以定性的作家。4.Iaskedtheauthortoautographmybook.我请作者在书上亲笔签名。5.You"renottheonlyauthortowhomthishashappen.你不是唯一一个碰上这种事的作者。如果您有什么疑问和不解之处，欢迎追问我！！！如果您认可我的答案，请采纳。您的采纳，是我答题的动力，O(∩_∩)O谢谢

settlement of exchange英 [ˈsetlmənt ɔv iksˈtʃeindʒ] 美 [ˈsɛtlmənt ʌv ɪksˈtʃendʒ] 词典结汇

[金融] 结汇

世事难料，兵来将挡。意指事情千变万化，一定要懂得随机应变。

情况变了，我们得兵来将挡！Roll with the punches实际上是逆来顺受的意思，在这里兵来将挡这样翻译比较合适！

情况变了，我们得兵来将挡！Roll with the punches实际上是逆来顺受的意思，在这里兵来将挡这样翻译比较合适！

因为关于礼物的习俗已经改变了。

IOS中，网页的前进后退操作(包括 history.go() 、 history.back() 等)是直接进入其离开时的快照，不会重新触发页面的 load 事件。此时js从上次离开时的状态继续往下执行。 document.referrer 是一个字符串，内容为上一页面的URL 不同浏览器对load/unload/pageshow/pagehide表现不同，使用前需多加测试 第一次进入时，触发 pageshow ，此时 isPageHide 为 false 。离开页面时触发 pagehide ， isPageHide 变为 true 。第二次进入时再次触发 pageshow ，此时 isPageHide 为 true ，成功触发页面刷新。 pageshow / pagehide 会在页面跳转前后触发，而 visibilitychange 会在页面被隐藏或显示时(如浏览器tab切换、窗口被最小化等)触发，配合 Document.hidden 可以实现如"页面被切到后台时停止声音播放，切到前台时恢复播放"等功能。

人员，人事部门的改变，

personnel change人事调动Then they won"t be confused or frustrated if they try to reach you, and weren"ttold of the personnel change. 这样当他们试图联系您而且没有被告知人事变更的情况下，他们不至于感到困惑或不快。很高兴第一时间为您解答，祝学习进步如有问题请及时追问，谢谢~~O(∩_∩)O

这是被动语态，掌握住公式可以以不变应万变

In the Late Proterozoic，profound changes occurred that included the break-up of the supercontinent Rodinia，geographically extensive glaciations，dramatic isotope excursions of，for example，strontium and carbon Jacobsen and Kaufman，this volume on a scale unprecedented in the Phanerozoic，intervals with high abundance of acritarchs suggesting alternating periods of low and high organic productivity，and the emergence of trace，body and skeletonized fossils. Close to the Precambrian-Cambrian boundary， other dramatic biotic events continue that have been described as the Cambrian Explosion. Extensive biomineralization of soft tissue in many major groups of organisms resulted in diverse skeletonized faunas being preserved in the fossil record. Some new biochemical evidence suggests that the initial radiation of major clades of metazoans began about 1200 Ma rather than about 600 Ma ago. If so，what processes or threshold conditions existed to suppress the abundance，size，and diversity radiation for about 600 Ma from 1200 to 600 Ma? Answers may lie in the chemical nature of these oceans. Martin has argued for superoligotrophic oceans for most of the Early Paleozoic. He considered that the oceans were predominantly stratified and only sluggishly circulating; as a consequence there was limited mixing and transfer of nutrients from the deep ocean to surface waters for utilization by organisms ( Fig. 1) . If the oxygen and CO2levels of about 0. 2，2 and 20 times the present atmospheric levels，respectively，for the Cambrian are correct，as interpreted by Berner，then a critical threshold factor for respiration and for ecological expansion would have been the O2levels in the surface and deeper part of the oceans. The interplay of anoxic waters with surface waters somewhat enriched in oxygen is likely to have been a critical factor in the waves of extinctions evident in Cambrian and early Ordovician rocks. Such encroachment of anoxic waters onto carbonate platforms was considered by Zhuravlev and Wood to cause the mid-Early Cambrian Botomian extinction and later the periods of eutrophication to be characterized by phytoplankton blooms. Using Sr and C isotopes data from the Upper Cambrian，Saltzman et al. argued that catastrophic ocean overturning produced similar periodic，widespread，anoxic conditions. Such pulses may well explain the pattern of trilobite extinctions that were used to define biomere boundaries by Palmer.Progressive ventilation of the deeper oceans appears to have occurred through the Ordovician and Silurian. Attempts to deduce the pattern of oceanic circulation for intervals throughout these two periods have been made by Wilde and Wilde et al. ，respectively，using the paleogeographic reconstructions of Scotese and McKerrow. The superoligotrophic conditions of these oceans and the warm greenhouse climate state throughout the Early Paleozoic were only interrupted in the Ashgill and early Llandovery ( Late Ordovician—Early Silurian) when a continental glaciation developed across North Africa that was then located near the southern pole. The onset of aggressive thermohaline circulation both chilled and ventilated the deep ocean with several glacial phases occurring over about a 10 Ma interval，but with the main Hirnantian phase perhaps lasting only for a few hundred thousand years. The cause of this short-lived icehouse state within such a long 200 Ma period of greenhouse conditions is still speculative and some authors have related it to the passage of part of Gondwana over the south polar region or to the brief drawdown of atmospheric CO2. Even as greenhouse states prevailed through much of the Silurian，detailed analysis on conodont microfossil distributions and related microfacies changes have suggested to Jeppsson and Aldridge et al. that the Silurian ocean state and associated climate was characterized by alternating primo and secundo states with periodic，but rapid turnover intervals. The principal differences being a warm humid phase vs. a drier cooler phase that resulted in significantly different lithologies and reef tracts across the low latitude carbonate platforms. Fig. 1 Indices of ancient nutrient fluxes and productivity through the last 650 MaAnother seemingly important factor in paleoceanography is the changing pattern of eustasy. Sensitive records are preserved on the carbonate platforms and examination of several cratons allows a global pattern to emerge for the Ordovician and Silurian. Major transgressions produced as epicontinental seas that generated important sites of warm，dense hypersaline waters and the periodic development and then closure of this system with transgressive and then regressive events has not yet been fully accommodated into paleoceanographic models. Such oscillations certainly produced major global bio-events. For the Late Ordovician，the Caradoc transgression was the largest of the Phanerozoic and may have been generated by much higher rates of sea-floor spreading and / or the occurrence of a mantle superplume.There is a marked contrast in the studies of paleoceanography of the Early Paleozoic with those of the Mesozoic and Cenozoic as noted initially. The application of a wide range of isotope proxy data with DSDP and ODP core samples and detailed analysis of abundant cores and outcrop studies in well preserved sedimentary basins，such as the Western Interior Seaway of North America，have allowed increasingly sophisticated interpretations of paleoceanography. Periods of anoxia，of less than 1 Ma duration have been recognized in all major oceans for the Late Barremian to Late Aptian of the Early Cretaceous. Peak oxygen deficiency corresponded to highly eutrophic conditions whereas less intense dysoxic / anoxic intervals were characteristic of oligotrophic conditions. The Albian and part of the Cenomanian were the warmest parts of the Cretaceous at a time when there appears to have been four times the present atmospheric level of CO2. Some authors have argued that ready transfer of heat from the equator to the polar regions reduced the latitudinal gradient and fostered a warm green-house state. Larson advocated the presence of a mid-Cretaceous mantle superplume in the western Pacific that produced the Ontong Java Plateau and this model was elaborated upon by Caldeira and Rampino to explain the widespread black shales，high organic productivity and oil accumulation ( Fig. 2) . Even within the Cretaceous there are considerable changes in oceanic temperature gradients. Huber et al. showed that during the Coniacian—Santonian the difference between low and high latitude surface- water paleotemperatures was in the range of 0—4℃ . As cooling increased towards the end of the period，the temperature difference increased to about 14℃ . Detailed investigations of the Cretaceous biotas have revealed complex patterns of marine biogeography that primarily mirror the changing major water masses and current systems along with the modifications to the Tethys Seaway and the Western Interior Seaway of North America. The open equatorial circulation around much of the globe via the Tethyan Seaway and the presence of wide shallow shelves on which warm saline waters were generated seem to be critical components to maintain the ultra warm greenhouse state at this time.Fig. 2 Inferred mid-Cretaceous mantle superplume showing increased ocean crust generation， sea level，black shales and related increases in ocean temperature and oil generation. These changes correspond to an interval free of magnetic reversals.In addition to the Cretaceous deep oceans，particularly Tethys，Pacific and opening Atlantic， large shelf seas developed as in Europe and the Western. Interior Sea of North America. The latter has received considerable attention because of the large stratigraphic database developed through oil exploration. In the Western Canada Sedimentary Basin，over 150，000 wells have been drilled in Alberta alone，with many aimed at the Cretaceous or passing to Devonian targets. The Cretaceous Seaway initially spread north from the Gulf of Mexico and south from the Beaufort Sea， meeting in Albian time. The sea was constrained on the west by emerging tectonic forelands tied to major Cordilleran orogenic phases and terrane accretion on the Pacific margin; on the east it lapped progressively eastwards on a largely peneplained Canadian Shield. Tectonic deformation generated an asymmetrically subsiding foreland basin and an eastward migrating peripheral bulge. From sedimentological and paleontological studies the seaway is estimated to have been up to 1000 m deep in the west-central corridor. The western margin was subjected to much clastic fill from the deforming foreland，transported by complex river systems. Volcanoes contributed extensive， eastwardly transported ash falls with over 200 bentonites in the Cretaceous sequence，which，with detailed biostratigraphy，have provided a remarkably detailed chemostratigraphy to unravel the changes to the seaway through time.Within this overall framework，there have been several recent attempts to understand and model the paleoceanography of this north-south seaway. Kaufmann initially tried to discriminate the inflowing north and south waters from surface freshwater caps derived from rivers mainly flowing from the emerging Cordilleran foreland. More recent attempts have modelled current flows within the sea-way. Jewell noted that salinity stratification in the seaway could have been established rapidly. Slingerland et al. proposed that river flux was important and likely controlled the strong counterclockwise gyre occupying the entire north-south extent of the seaway.In the Cenozoic，an early phase of global warming ( Paleocene—Eocene) was followed by a progressive but variable decline in mean annual temperature ( Oligocene—Recent) . The onset of glaciation occurred first in Antarctica close to the Eocene—Oligocene boundary ( ca. 34 Ma) . Major Arctic glaciation appears to have been initiated in the late Pliocene ( ca. 2. 8 Ma) . The Cenozoic provides an opportunity to investigate the processes of changeover from a greenhouse to icehouse state. Fundamental questions remain unresolved about the initiation and maintenance of these two states and of the complex feedback loops in the climate system. Of particular interest are the processes of heat transfer to the high latitudes during a greenhouse state and their collapse during the icehouse state. Two possible principal causes have been advanced， possibly interrelated. Firstly，decreased atmospheric CO2partly derived from the weathering of uplifted crustal rocks during the late phases of alpine orogeny ( e. g. ， Himalayan， Alps， Andes， Cordillera) . Secondly，there was substantially altered ocean circulation，particularly the onset of the deep ocean conveyor belt with thermohaline circulation derived from sinking of cold water in the North Atlantic. In this latter case，the pattern of ocean circulation is strongly affected by paleogeographic barriers such as the opening of the Drake Passage or closing of the Panama Isthmus.For the early Cenozoic greenhouse state，O"Connell et al. modelled atmospheric circulation conditions. In one experiment，they showed that under extreme zonal conditions evaporation may have substantially exceeded precipitation leading to the generation of very saline water. Zachos et al. discussed early Cenozoic temperatures from the oceanographic view，and Hovan and Rea used ODP data to examine the particular changes at the Paleocene / Eocene boundary. Here，they noted the dramatic changes that occur over a period of about 1. 2 Ma including: extinction of some benthic foraminifera and changes in calcareous plankton assemblages，oceanic warming，decrease in carbon isotope ratios，reduction in wind strength，an increase in hydrothermal activity. This same change is found in the continental record and is marked by the first appearance of several important modern mammalian orders. The Paleocene and early Eocene climates were controlled primarily by large scale meridional energy transport through the oceans rather than the atmosphere and in part influenced by tectonic events. Hovan and Rea showed that a strong reduction in Paleocene / Eocene wind stress occurs in both hemispheres at the boundary，related to decreased latitudinal thermal gradients produced by a more effective poleward heat transport via the deep ocean.There were dramatic changes to these greenhouse conditions at the Eocene / Oligocene boundary，including: fall in oceanic bottom water temperatures; 1 km drop in the calcium compensation depth in the Pacific; increase in deep sea unconformities; extinctions of planktonic foraminifera. These were apparently related to sudden high latitude cooling and enhanced oceanic thermohaline circulation. The onset of Antarctic glaciation occurred at about 34. 5 Ma seemingly closely related to the opening of the Drake Passage ( between South America and Antarctica) : surface and intermediate water circulation is documented by paleontology at this time，with other geologic evidence suggesting complete opening and deepwater circulation by about 30 Ma. These circulation changes induced a new position for the polar front and strongly influenced the pattern of upwelling and productivity.The late Neogene marks the onset of Arctic glaciation and enhanced global cooling. A significant oceanographic circulation event during this time was the full closure，evaporation and then reflooding of the Mediterranean Sea; the Messinian Event ( ca. 8—5 Ma ) in the late Miocene. The more recent work based on defined sequence stratigraphy and chronostratigraphy has shown that there were two distinct phases of evaporite accumulation，each associated with a sea-level drop that were in turn likely to be of glacio-eustatic origin. Salt a

歌曲名:Changes歌手:2Pac专辑:The Best Of 2Pac - Pt. 1: Thug2pac -《Changes》Robin_SHICome on come onI see no changeswake up in the morning and I ask myselfis life worth living should I blast myself?I"m tired of bein" poor & even worse I"m blackmy stomach hurts so I"m lookin" for a purse to snatchCops give a damn about a negropull the trigger kill a nigga he"s a heroGive the crack to the kids who the hell caresone less hungry mouth on the welfareFirst ship "em dope & let "em deal the brothersgive "em guns step back watch "em kill each otherIt"s time to fight back that"s what Huey said2 shots in the dark now Huey"s deadI got love for my brotherbut we can never go nowhereunless we share with each otherWe gotta start makin" changeslearn to see me as a brotherinstead of 2 distant strangersand that"s how it"s supposed to beHow can the Devil take a brotherif he"s close to me?I"d love to go back to when we played as kidsbut things changed, and that"s the way it isCome on come onThat"s just the way it is"Changes"Things"ll never be the sameThat"s just the way it isaww yeahThat"s just the way it isThings"ll never be the sameThat"s just the way it isaww yeahI see no changesall I see is racist facesmisplaced hate makes disgrace to racesWe underI wonder what it takes to make thisone better place,let"s erase the wastedTake the evil out the people they"ll be acting right"cause both black and white is smokin" crack tonightand only time we chill is when we kill each otherit takes skill to be real, time to heal each otherAnd although it seems heaven sentWe ain"t ready, to see a black President, uhhIt ain"t a secret don"t conceal the factthe penitentiary"s packed,and it"s filled with blacksBut some things will never changetry to show another way but you stayin" in the dope gameNow tell me what"s a mother to dobein" real don"t appeal to the brother in youYou gotta operate the easy way"I made a G today" But you made it in a sleazy waysellin" crack to the kid. " I gotta get paid,"Well hey, well that"s the way it isCome on come onThat"s just the way it is"Changes"Things"ll never be the sameThat"s just the way it isaww yeahCome on come onThat"s just the way it isThings"ll never be the same"Things"ll never be the same.aww yeah"That"s just the way it isaww yeah"aww yeah"We gotta make a change...It"s time for us as a peopleto start makin" some changes.Let"s change the way we eat,let"s change the way we liveand let"s change the way we treat each other.You see the old way wasn"t working so it"s on us to dowhat we gotta do, to survive.And still I see no changescan"t a brother get a little peaceIt"s war on the streets & the war in the Middle EastInstead of war on poverty they got a war on drugsso the police can bother meAnd I ain"t never did a crime I ain"t have to doBut now I"m back with the blacks givin" it back to youDon"t let "em jack you up,back you up,crack you upand pimp slap you upYou gotta learn to hold ya ownthey get jealous when they see ya with ya mobile phoneBut tell the cops they can"t touch thisI don"t trust this when they try to rush I bust thisThat"s the sound of my tool you say it ain"t coolmy mama didn"t raise no foolAnd as long as I stay blackI gotta stay strappedand I never get to lay back"Cause I always got to worry "bout the pay backssome buck that I roughed up way backcomin" back after all these yearsrat-a-tat-tat-tat-tat that"s the way it is uhhThat"s just the way it is""Things"ll never be the sameThat"s just the way it isaww yeahThat"s just the way it is"way it is"" way it is"Things"ll never be the sameThat"s just the way it isaww yeah..http://music.baidu.com/song/7548937

In the Late Proterozoic，profound changes occurred that included the break-up of the supercontinent Rodinia，geographically extensive glaciations，dramatic isotope excursions of，for example，strontium and carbon Jacobsen and Kaufman，this volume on a scale unprecedented in the Phanerozoic，intervals with high abundance of acritarchs suggesting alternating periods of low and high organic productivity，and the emergence of trace，body and skeletonized fossils. Close to the Precambrian-Cambrian boundary， other dramatic biotic events continue that have been described as the Cambrian Explosion. Extensive biomineralization of soft tissue in many major groups of organisms resulted in diverse skeletonized faunas being preserved in the fossil record. Some new biochemical evidence suggests that the initial radiation of major clades of metazoans began about 1200 Ma rather than about 600 Ma ago. If so，what processes or threshold conditions existed to suppress the abundance，size，and diversity radiation for about 600 Ma from 1200 to 600 Ma? Answers may lie in the chemical nature of these oceans. Martin has argued for superoligotrophic oceans for most of the Early Paleozoic. He considered that the oceans were predominantly stratified and only sluggishly circulating; as a consequence there was limited mixing and transfer of nutrients from the deep ocean to surface waters for utilization by organisms ( Fig. 1) . If the oxygen and CO2levels of about 0. 2，2 and 20 times the present atmospheric levels，respectively，for the Cambrian are correct，as interpreted by Berner，then a critical threshold factor for respiration and for ecological expansion would have been the O2levels in the surface and deeper part of the oceans. The interplay of anoxic waters with surface waters somewhat enriched in oxygen is likely to have been a critical factor in the waves of extinctions evident in Cambrian and early Ordovician rocks. Such encroachment of anoxic waters onto carbonate platforms was considered by Zhuravlev and Wood to cause the mid-Early Cambrian Botomian extinction and later the periods of eutrophication to be characterized by phytoplankton blooms. Using Sr and C isotopes data from the Upper Cambrian，Saltzman et al. argued that catastrophic ocean overturning produced similar periodic，widespread，anoxic conditions. Such pulses may well explain the pattern of trilobite extinctions that were used to define biomere boundaries by Palmer.Progressive ventilation of the deeper oceans appears to have occurred through the Ordovician and Silurian. Attempts to deduce the pattern of oceanic circulation for intervals throughout these two periods have been made by Wilde and Wilde et al. ，respectively，using the paleogeographic reconstructions of Scotese and McKerrow. The superoligotrophic conditions of these oceans and the warm greenhouse climate state throughout the Early Paleozoic were only interrupted in the Ashgill and early Llandovery ( Late Ordovician—Early Silurian) when a continental glaciation developed across North Africa that was then located near the southern pole. The onset of aggressive thermohaline circulation both chilled and ventilated the deep ocean with several glacial phases occurring over about a 10 Ma interval，but with the main Hirnantian phase perhaps lasting only for a few hundred thousand years. The cause of this short-lived icehouse state within such a long 200 Ma period of greenhouse conditions is still speculative and some authors have related it to the passage of part of Gondwana over the south polar region or to the brief drawdown of atmospheric CO2. Even as greenhouse states prevailed through much of the Silurian，detailed analysis on conodont microfossil distributions and related microfacies changes have suggested to Jeppsson and Aldridge et al. that the Silurian ocean state and associated climate was characterized by alternating primo and secundo states with periodic，but rapid turnover intervals. The principal differences being a warm humid phase vs. a drier cooler phase that resulted in significantly different lithologies and reef tracts across the low latitude carbonate platforms. Fig. 1 Indices of ancient nutrient fluxes and productivity through the last 650 MaAnother seemingly important factor in paleoceanography is the changing pattern of eustasy. Sensitive records are preserved on the carbonate platforms and examination of several cratons allows a global pattern to emerge for the Ordovician and Silurian. Major transgressions produced as epicontinental seas that generated important sites of warm，dense hypersaline waters and the periodic development and then closure of this system with transgressive and then regressive events has not yet been fully accommodated into paleoceanographic models. Such oscillations certainly produced major global bio-events. For the Late Ordovician，the Caradoc transgression was the largest of the Phanerozoic and may have been generated by much higher rates of sea-floor spreading and / or the occurrence of a mantle superplume.There is a marked contrast in the studies of paleoceanography of the Early Paleozoic with those of the Mesozoic and Cenozoic as noted initially. The application of a wide range of isotope proxy data with DSDP and ODP core samples and detailed analysis of abundant cores and outcrop studies in well preserved sedimentary basins，such as the Western Interior Seaway of North America，have allowed increasingly sophisticated interpretations of paleoceanography. Periods of anoxia，of less than 1 Ma duration have been recognized in all major oceans for the Late Barremian to Late Aptian of the Early Cretaceous. Peak oxygen deficiency corresponded to highly eutrophic conditions whereas less intense dysoxic / anoxic intervals were characteristic of oligotrophic conditions. The Albian and part of the Cenomanian were the warmest parts of the Cretaceous at a time when there appears to have been four times the present atmospheric level of CO2. Some authors have argued that ready transfer of heat from the equator to the polar regions reduced the latitudinal gradient and fostered a warm green-house state. Larson advocated the presence of a mid-Cretaceous mantle superplume in the western Pacific that produced the Ontong Java Plateau and this model was elaborated upon by Caldeira and Rampino to explain the widespread black shales，high organic productivity and oil accumulation ( Fig. 2) . Even within the Cretaceous there are considerable changes in oceanic temperature gradients. Huber et al. showed that during the Coniacian—Santonian the difference between low and high latitude surface- water paleotemperatures was in the range of 0—4℃ . As cooling increased towards the end of the period，the temperature difference increased to about 14℃ . Detailed investigations of the Cretaceous biotas have revealed complex patterns of marine biogeography that primarily mirror the changing major water masses and current systems along with the modifications to the Tethys Seaway and the Western Interior Seaway of North America. The open equatorial circulation around much of the globe via the Tethyan Seaway and the presence of wide shallow shelves on which warm saline waters were generated seem to be critical components to maintain the ultra warm greenhouse state at this time.Fig. 2 Inferred mid-Cretaceous mantle superplume showing increased ocean crust generation， sea level，black shales and related increases in ocean temperature and oil generation. These changes correspond to an interval free of magnetic reversals.In addition to the Cretaceous deep oceans，particularly Tethys，Pacific and opening Atlantic， large shelf seas developed as in Europe and the Western. Interior Sea of North America. The latter has received considerable attention because of the large stratigraphic database developed through oil exploration. In the Western Canada Sedimentary Basin，over 150，000 wells have been drilled in Alberta alone，with many aimed at the Cretaceous or passing to Devonian targets. The Cretaceous Seaway initially spread north from the Gulf of Mexico and south from the Beaufort Sea， meeting in Albian time. The sea was constrained on the west by emerging tectonic forelands tied to major Cordilleran orogenic phases and terrane accretion on the Pacific margin; on the east it lapped progressively eastwards on a largely peneplained Canadian Shield. Tectonic deformation generated an asymmetrically subsiding foreland basin and an eastward migrating peripheral bulge. From sedimentological and paleontological studies the seaway is estimated to have been up to 1000 m deep in the west-central corridor. The western margin was subjected to much clastic fill from the deforming foreland，transported by complex river systems. Volcanoes contributed extensive， eastwardly transported ash falls with over 200 bentonites in the Cretaceous sequence，which，with detailed biostratigraphy，have provided a remarkably detailed chemostratigraphy to unravel the changes to the seaway through time.Within this overall framework，there have been several recent attempts to understand and model the paleoceanography of this north-south seaway. Kaufmann initially tried to discriminate the inflowing north and south waters from surface freshwater caps derived from rivers mainly flowing from the emerging Cordilleran foreland. More recent attempts have modelled current flows within the sea-way. Jewell noted that salinity stratification in the seaway could have been established rapidly. Slingerland et al. proposed that river flux was important and likely controlled the strong counterclockwise gyre occupying the entire north-south extent of the seaway.In the Cenozoic，an early phase of global warming ( Paleocene—Eocene) was followed by a progressive but variable decline in mean annual temperature ( Oligocene—Recent) . The onset of glaciation occurred first in Antarctica close to the Eocene—Oligocene boundary ( ca. 34 Ma) . Major Arctic glaciation appears to have been initiated in the late Pliocene ( ca. 2. 8 Ma) . The Cenozoic provides an opportunity to investigate the processes of changeover from a greenhouse to icehouse state. Fundamental questions remain unresolved about the initiation and maintenance of these two states and of the complex feedback loops in the climate system. Of particular interest are the processes of heat transfer to the high latitudes during a greenhouse state and their collapse during the icehouse state. Two possible principal causes have been advanced， possibly interrelated. Firstly，decreased atmospheric CO2partly derived from the weathering of uplifted crustal rocks during the late phases of alpine orogeny ( e. g. ， Himalayan， Alps， Andes， Cordillera) . Secondly，there was substantially altered ocean circulation，particularly the onset of the deep ocean conveyor belt with thermohaline circulation derived from sinking of cold water in the North Atlantic. In this latter case，the pattern of ocean circulation is strongly affected by paleogeographic barriers such as the opening of the Drake Passage or closing of the Panama Isthmus.For the early Cenozoic greenhouse state，O"Connell et al. modelled atmospheric circulation conditions. In one experiment，they showed that under extreme zonal conditions evaporation may have substantially exceeded precipitation leading to the generation of very saline water. Zachos et al. discussed early Cenozoic temperatures from the oceanographic view，and Hovan and Rea used ODP data to examine the particular changes at the Paleocene / Eocene boundary. Here，they noted the dramatic changes that occur over a period of about 1. 2 Ma including: extinction of some benthic foraminifera and changes in calcareous plankton assemblages，oceanic warming，decrease in carbon isotope ratios，reduction in wind strength，an increase in hydrothermal activity. This same change is found in the continental record and is marked by the first appearance of several important modern mammalian orders. The Paleocene and early Eocene climates were controlled primarily by large scale meridional energy transport through the oceans rather than the atmosphere and in part influenced by tectonic events. Hovan and Rea showed that a strong reduction in Paleocene / Eocene wind stress occurs in both hemispheres at the boundary，related to decreased latitudinal thermal gradients produced by a more effective poleward heat transport via the deep ocean.There were dramatic changes to these greenhouse conditions at the Eocene / Oligocene boundary，including: fall in oceanic bottom water temperatures; 1 km drop in the calcium compensation depth in the Pacific; increase in deep sea unconformities; extinctions of planktonic foraminifera. These were apparently related to sudden high latitude cooling and enhanced oceanic thermohaline circulation. The onset of Antarctic glaciation occurred at about 34. 5 Ma seemingly closely related to the opening of the Drake Passage ( between South America and Antarctica) : surface and intermediate water circulation is documented by paleontology at this time，with other geologic evidence suggesting complete opening and deepwater circulation by about 30 Ma. These circulation changes induced a new position for the polar front and strongly influenced the pattern of upwelling and productivity.The late Neogene marks the onset of Arctic glaciation and enhanced global cooling. A significant oceanographic circulation event during this time was the full closure，evaporation and then reflooding of the Mediterranean Sea; the Messinian Event ( ca. 8—5 Ma ) in the late Miocene. The more recent work based on defined sequence stratigraphy and chronostratigraphy has shown that there were two distinct phases of evaporite accumulation，each associated with a sea-level drop that were in turn likely to be of glacio-eustatic origin. Salt a

假若轻易就可以改变，那么人们就不会特意“期待改变”了。人即使想要改变也无法改变。正因为如此，才会不断有人被宣扬可以改变人的新兴宗教或怪异的自我启发课程所蒙骗。 1) 欺骗 I can"t believe she was taken in by him. 我简直不敢相信她被他骗了。 2) 收留，收容，收养（某人） Several families took in foreign students. 有几个家庭接待外国留学生。/ˈduː.bi.əs/ 半信半疑的，可疑的；不确定的；不可信的 These claims are dubious and not scientifically proven. 这些说法未经科学证实，有些可疑。 He has been associated with some dubious characters. 他曾经与一些可疑人物有交往。（尤指牧师在教堂中）讲道，布道 Father Martin preached to the assembled mourners. 马丁神父向聚集的哀悼者们布道。 During the sermon, he preached about the need for forgiveness. 在布道中，他宣讲了宽恕的必要性。那么，我要反过来问问你。为什么你会如此固执地主张人无法改变呢？ 作为回应 Moon Jae-in conveyed his gratitude in response. 文在寅在回信中表示感谢。 In response, Panama recalled its Ambassador from Caracas. 作为回应，巴拿马召回了驻加拉加斯大使。/ˈæd.ə.mənt/ 固执的；坚决的，坚定不移的 [ + that ] I"ve told her she should stay at home and rest but she"s adamant that she"s coming. 我告诉过她应该在家休息，可她坚持要来。作为朋友我可以担保他是一位非常认真并且对社会有用的男人。向某人保证 Breaking your leg isn"t funny , I can assure you. 打断你的腿不好笑，我可以向你保证 "Don"t worry, your car will be ready tomorrow," the mechanic assured him. “别担心，你的车明天就可以修好，”修理工向他保证。很有用 For I"m sure my major would be of great use for the position.  因为我肯定我的所学专业对这一工作一定会很有用处。假若如你所言，如果所有人的“现在”都由“过去”所决定，那岂不是很奇怪吗？现在, 此时此刻 Most people can"t be bothered thinking about their retirement - they"re too busy concentrating on the here and now. 大多数人都顾不上去考虑退休的事情——他们都在忙着考虑现在。1) …地发生（或发展）；结果是（尤指出乎意料的结果） As events turned out, we were right to have decided to leave early. 结果证明，我们当初决定早点离开是正确的。 How did the recipe turn out? 按这个食谱做出来的菜如何？2) 最终成为；最终发现 [ + to infinitive ] The truth turned out to be stranger than we had expected. 结果，真相比我们预期的更离奇。 [ + that ] It turns out that she had known him when they were children. 结果发现，她和他从小就认识。对不起，那是绝对不可能的事情。或者 be no question of (doing) sth 不可能 A trip to New Zealand is out of the question this year. 今年去新西兰旅行是不可能的了。 There"s no question of agreeing to the demands. 同意这些要求是不可能的。

天气骤变

that引导的定语从句，后面的is more tremendous than ever都是修饰的前面的way

c,目睹

c目睹 D是忽略的意思 所以选C

我记得对客观事实的陈述，用一般形式，呵呵

D 动词的时态。句意：—中国发展如此迅速。—是呀。它已经发生了很大的变化。表示发生在过去对现在仍有影响的动作。所以，判定为现在完成时。故选D。

Cause some things just don"t change因为有些事终究不会改变It"�0�3 better when they stay the same其实保持原样更好Although the whole world knows your name尽管全世界都知道你的名号So on the biggest days they came to see you spit your game因此在最重大的这个日子，他们全都过来看你点燃这个游戏Ooooohhhhhhh噢....It shouldn"t be difficult to explain这解释起来应该不太困难Just why you came back again, you hate the fame你为何又再次回来了，因为你憎恨名誉Love the game, cold as ice you remain热爱这个游戏，像你一贯的那样冷酷f**k em" all, tell "em all eat s**t, here we go againCTMD，叫他们全去吃屎，现在我们又启程了So, god damn... is it that time again already所以，该死的...又再次是这个时候Haha, you don"t look too happy to see me哈哈，你看上去不大高兴见到我f**k man, don"t everybody welcome me back at onceCNM的，既然不是每个人都欢迎老子的回归All right, f**k ya"ll then好吧，CNMB！(Verse 1)You can get the d*ck, just call me the ballsac, I"m nuts你能得到JB,叫老子ballsac，我是个疯子Michael Vick in thi�0�3 b**ch, fall back you mutt�0�3Michael Vick 臭婊丄子，给我趴下，杂种f**k your worms, you never seen such a sick puppyCNM你们这群懦夫，你们从未见过这样的疯狗吧？f**k it a sick duck, I"m on my duck sick mummyCNM的，这是口丄活，我弄出来了，给我吹And my nuts, lick, gobble "em up trick, yummy我的蛋蛋，给老子舔！用你的口技好好品尝，很美味吧？b**ch you don"t f**king think that I know that you suck d*ck dummy?臭婊丄子，你TMD认为我不知道你吮过假人的JB?You"ll get your butt kicked, f**k all that love s**t honey你们会被踹得屁滚尿流的，CNM的所谓的狗屎情情爱爱，情爱的Yeah I laugh when I call you a slut, it"s funny!耶，当我叫你婊丄子时，我笑了，真有趣！Shawty dance while I diss you to the beat, f**k the words小妞，当我伴着这拍子骂你时，给我跳起来，CNM的少废话You don"t listen to "em anyway, yeah struck a nerve sucker再说你也不会理会它们，耶，逮着了个紧张的口丄活者Motherf**ker might aswell let my lips puckerCNM的，也舔舔我的嘴唇啊！Like Elton John, cause I"m just a mean cock sucker就像Elton John一样，因为我是个恶毒的吹箫者This s**t is on, cause you wen"t and pissed me off好戏正上演着，因为你不会离开，不会把我惹毛Now I"m sitting and pissing on everbody现在我坐下来，朝每个人身上撒尿give a f**k if it"s right or wrong谁TMD在乎这是对是错？So buck the bu最近出了个不错的日语学习网站：大满足日本语那里有个很好用的日语学习软件： http://www.damanzu.com

带有chang的词语长处、班长、连长、长度、长老、生长、长江、军长、家长、长短、

1. 长（chang）开头的四个字的词语 长安道上 长安居大不易 长安棋局 长安少年 长傲饰非 长才短驭 长才广度 长材茂学 长材小试 长春不老 长此以往 长恶不悛 长恶靡悛 长风破浪 长歌当哭 长话短说 长虺成蛇 长戟高门 长计远虑 长驾远驭 长江后浪推前浪 长江天堑 长街短巷 长颈鸟喙 长久之计 长乐未央 长林丰草 长虑顾后 长虑后顾 长虑却顾 长眠不起 长鸣都尉 长命百岁 长命富贵 长目飞耳 长年累月 长年三老 长念却虑 长辔远驭 长辔远御 长篇大论 长篇大套 长篇累牍 长驱深入 长驱直进 长驱直入 长舌之妇 长蛇封豕 长生不老 长生不死 长生久视 长绳系景 长绳系日 长算远略 长他人志气，灭自己威风 长谈阔论 长亭短亭 长途跋涉 长往远引 长袖善舞 长嘘短叹 长夜漫漫 长夜难明 长夜之饮 长揖不拜 长吁短气 长吁短叹 长斋礼佛 长斋绣佛 长枕大被 长枕大衾 长治久安 2. 长开头的四字成语 长开头的四字成语 ： 长年累月、 长途跋涉、 长驱直入、 长吁短叹、 长歌当哭、 长眠不起、 长久之计、 长生不老、 长命百岁、 长话短说、 长幼有序、 长幼尊卑、 长篇大论、 长才短驭、 长嘘短叹、 长念却虑、 长材短用、 长鸣都尉、 长才广度、 长城自坏、 长安道上、 长颈鸟喙、 长相思守、 长城万里、 长虑顾后、 长斋绣佛、 长年三老、 长夜漫漫、 长天老日、 长夜难明 长幼妍媸、 长明乃晦、 长街短巷、 长夜之饮、 长啜大嚼、 长七短八、 长乐未央、 长身玉立、 长命富贵、 长舌之妇、 长揖不拜、 长材茂学、 长往远引、 长春不老、 长此以往、 长袖善舞、 长算远略、 长亭短亭、 长枕大被、 长材小试、 长吁短气、 长安少年、 长戟高门、 长安棋局、 长傲饰非、 长绳系日、 长生久视、 长篇大章、 长辔远驭、 长江天堑 3. 开头是四的四字词语 四不拗六 四百四病 四冲八达 四冲六达 四大皆空 四方八面 四方辐辏 四分五裂 四分五落 四纷五落 四分五剖 四方之志 四海波静 四荒八极 四海承风 四海鼎沸 四海九州 四海皆兄弟 四海飘零 四海升平 四海升平 四海他人 四海为家 四海一家 四脚朝天 四郊多垒 四角俱全 四面八方 四面楚歌 四海之内皆兄弟 四面出击 四马攒蹄 四面受敌 四平八稳 四衢八街 四清六活 四时八节 四书五经 四山五岳 四时之气 四亭八当 四通八达 四停八当 四体不勤，五谷不分 四体百骸 四体不勤 四通五达 四姻九戚 四至八道 四肢百骸 四肢百体 四战之地 四战之国 4. niang字开头的四字成语 没有niang字开头的成语。 niang可为娘、酿、娘等。 一、娘字成语 1、丁娘十索 【拼音】： dīng niáng shí suǒ 【解释】： 丁娘：隋朝歌妓；索：索取。原指隋代乐妓丁六娘所作的乐府诗，每首末句有“从郎索花烛”等语，本十首。后用以指 *** 的需索。 【出处】： 清·孙枝蔚《无题次彭骏孙王贻上韵》。 2、爷羹娘饭 【拼音】： yé gēng niáng fàn 【解释】： 指在父母的庇荫下生活。同“爷饭娘羹”。 【出处】： 元·宫天挺《范张鸡黍》第一折：“生下来便落在那爷羹娘饭长生运。” 3、儿大不由娘 【拼音】： ér dà bù yóu niáng 【解释】： 儿子长大了，由不得母亲作主。 【出处】： 清·西周生《醒世姻缘传》第89回：“别说我是他妗子，我就是他娘，他‘儿大不由娘"，我也管不的他。” 【举例造句】： 儿大不由娘，我也没办法了。 二、酿组词 1、酝酿[yùn niàng] 造酒的发酵过程，比喻做准备工作。 2、酿造[niàng zào] 原专指酿酒。后也指利用发酵作用制造醋、酱油等。 3、酒酿[jiǔ niàng] 带糟的甜米酒。 4、酿糯[niàng nuò] 以糯米酿酒。 5、酿饭[niàng fàn] 使饭发酵。 6、私酿[sī niàng] 私自酿酒。 5. yang音开头的四字成语大全 yang音开头的四字成语： 阳春白雪： 原指战国时代楚国的一种较高级的歌曲。比喻高深的不通俗的文学艺术。 阳春有脚： 用以称誉贤明的官员。 阳奉阴违： 阳：表面上；奉：遵守，听从；阴：暗地里。指玩弄两面派手法，表面上遵从，暗地里违背。 阳关大道 ： 原指古代经过阳关通向西域的大道，后泛指宽阔的长路，也比喻光明的前途。 阳关三迭 ： 阳关：古关名，在今甘肃敦煌县西南；三迭：反复歌唱某一句。原指古代送别的曲调。后也比喻离别。 阳煦山立： 象太阳那样暖和，象山岳那样屹立。比喻人性格温和，品行端正。 6. 开头是天的四字词语 天宝当年、天保九如、天崩地坼、天崩地解、天崩地裂 天崩地塌、天崩地坍、天崩地陷、天兵天将、天不假年 天不绝人、天不怕，地不怕、天不作美、天差地远、天长地久 天长地老、天长日久、天成地平、天愁地惨、天从人原 天从人愿、天摧地塌、天打雷劈、天大地大、天道好还 天道宁论、天道人事、天道无亲、天低吴楚，眼空无物、天地不容 天地长久、天地经纬、天地剖判、天地诛戮、天地诛灭 天夺其魄、天夺之年、天夺之魄、天翻地覆、天方夜谭 天府之国、天付良缘、天覆地载、天高地厚、天高地迥 天高地下、天高皇帝远、天高日远、天高听卑、天高听下 天各一方、天工人代、天公地道、天冠地屦、天寒地冻 天花乱坠、天华乱坠、天荒地老、天潢贵胄、天昏地暗 天昏地黑、天机不可泄漏、天机不可泄露、天机云锦、天假良缘 天假其年、天假因缘、天假之年、天经地纬、天经地义 天荆地棘、天惊石破、天开地辟、天空海阔、天朗气清 天老地荒、天理不容、天理良心、天理难容、天理人情 天理昭彰、天理昭昭、天伦之乐、天罗地网、天马行空 天命攸归、天命有归、天末凉风、天南地北、天南海北 天年不测、天年不齐、天年不遂、天凝地闭、天怒人怨 天女散花、天平地成、天清气朗、天清日白、天壤王郎 天壤悬隔、天壤之别、天壤之隔、天人共鉴、天人之际 天若有情天亦老、天上麒麟、天上人间、天上石麟、天生地设 天生丽质、天生天化、天生天杀、天生尤物、天时地利人和 天授地设、天粟马角、天随人原、天随人愿、天塌地陷 天台路迷、天堂地狱、天外飞来、天外有天、天王老子 天网恢恢、天网恢恢，疏而不漏、天无二日、天无绝人之路、天下本无事，庸人自扰之 天下大乱、天下第一、天下独步、天下归心、天下莫敌 天下太平、天下为公、天下为家、天下为笼、天下乌鸦一般黑 天下无敌、天下无难事，只怕有心人、天下无双、天下兴亡，匹夫有责、天下汹汹 天下一家、天香国色、天行时气、天悬地隔、天旋地转 天涯比邻、天涯地角、天涯海角、天涯咫尺、天摇地动 天衣无缝、天有不测风云、天有不测风云，人有旦夕祸福、天诱其衷、天与人归 天渊之别、天渊之隔、天缘凑合、天灾地变、天灾地妖 天灾人祸、天造草昧、天造地设、天真烂漫、天真烂熳 天震地骇、天之骄子、天之僇民、天之戮民、天知地知 天诛地灭、天姿国色、天字第一号、天作之合

长此以往，长短结合，长治久安，。。太多啦