supp

假设supply=S, demand=D, price=P, 先划一个数标轴,x轴就是quantity货物的数量,y轴就是P价格需求D和价格P成反比,所以是在图表里表示为一条从左上往右下倾斜的直线供给S和价格p成正比,所以是从左下往右上倾斜的直线所以D和S表现为一个叉 (x),他们相交的那个点刚好是供给者和消费者都能接受的市场均衡价格P1,那个点就是均衡价格equilibrium,具体价格为横对过来y轴的数值给你画个草图P | s | ＼ ／ | p1＼.／ | ／＼ | ／ ＼ |_________＼d__________Q

假设supply=S, demand=D, price=P, 先划一个数标轴,x轴就是quantity货物的数量,y轴就是P价格需求D和价格P成反比,所以是在图表里表示为一条从左上往右下倾斜的直线供给S和价格p成正比,所以是从左下往右上倾斜的直线所以D和S表现为一个叉 (x),他们相交的那个点刚好是供给者和消费者都能接受的市场均衡价格P1,那个点就是均衡价格equilibrium,具体价格为横对过来y轴的数值给你画个草图P | s | ＼ ／ | p1＼.／ | ／＼ | ／ ＼ |_________＼d__________Q

提供壁橱

供给、需求、价格、均衡参考一下高鸿业的《微观经济学》第二章：供求曲线。

表示情感类的动词基本上都有这两种形式的形容词。如：excited/exciting; amused/amusing; frightened/frightening; disappointed/disappointing;

补给,供给 v. 补给,供给

自己感觉吧

牛仔裤供应

grasp: 有掌握那种抓住的意思，即理解的意思 scratch：有刮、擦的意思，那种clutch：和grip差不多，也是紧紧抓住地意思 grab：强取豪夺的意思，和前几个

请参考

collagen supplements胶原蛋白的补充双语例句Consuming collagen orally is the most effective way, because most of the collagen supplements are hydrolyzed collagen and it ensures a better absorption. 而口服是最有效的方法，因辅助品中的胶原蛋白多属水解性胶原蛋白，助人体更加容易吸收。

http://support1.ap.dell.com/cn/zh/forum/forum.asp?fid=6去这里去找高人求教

你的内存插得位置不对，要放到第一个槽或者第三个。

convince sb sth 使某人相信某事 可以跟名词、代词必然能跟从句

浏览器不支持applet，你设置下你的浏览器

设成true会给 scripts 更大权限进行功能更强但有风险性的操作，比如说可以用某些脚本复制到剪贴板的操作，需要注意的是只是允许脚本进行有风险性的操作，而不是直接允许操作，还是需要使用脚本。

ture

现在浏览器的地址栏输入about:config 然后在搜索框中输入signed.applets.codebase_principal_support 双击它 就改为true

把分给我好不好，却分啊

地址栏输入about:config 然后搜索这个改了就行了 不过迅雷下载的话改了也没用 还是直接用IE吧

branded goods&supplies since 1982品牌商品与供应自1982采纳呀。

你好，很高兴为你解答:品牌商品供应词汇branded goods有商标货物，厂商定牌货物since自…以后; 从…以来; 何曾，什么时候; 从…以后; 自…以来; 因为; 由于; 既然; 此后; 后来

在表示支持的意思的时候，endorse经常表示为（公开地）赞同，支持，认可，而SUPPORT则是单纯地支持。

在表示支持的意思的时候,endorse经常表示为（公开地）赞同,支持,认可,而SUPPORT则是单纯地支持.

在表示支持的意思的时候,endorse经常表示为（公开地）赞同,支持,认可,而SUPPORT则是单纯地支持.

供养子女的费用呗！！

　　transaction　 n.交易；事务；办理；会报,学报 　　epidemic n.传染病；流行病；风尚等的流行 adj.流行的；传染性的 　　supplement n.补充,补遗；补充物；附录 vt.补充,增补 　　subsequent adj.后来的,随后的 　　contradict vt.反驳；否定；与…矛盾；与…抵触 vi.反驳；否认；发生矛盾 　　unaffected adj.不受影响的；自然的；真挚的；不矫揉造作的 　　1.The writer was very excited because his story would be published in the【subsequent】issues of the newspaper. 　　作者非常激动,因为他的故事将会发表在【后续】问题的报纸上. 　　2.It is not easy for a bank clerk to keep cool when there are millions of【transaction】to deal with every day. 　　对一个银行职员来说,当每天处理成千上万的交易时要保持冷静并不容易. 　　3.Everybody was worried about their health when the unexpected【epidemic】took lives of many people. 　　每个人都在担心他们的健康,当意想不到的流行病夺走很多人的生命. 　　4.Good food should be【supplemented】by regular exercise if you want to keep fit. 　　如果你想保持健康,好的食物应该根据定期锻炼来补充. 　　5.No matter what difficulty he ran into ,his dream of being a respectable doctor stayed 【unaffected】. 　　不管他遇到什么困难,他梦想成为一名受人尊敬的医生始终不受影响. 　　6.Many citizens were angry when the new housing policy 【contradicted 】the mayor" promise 　　当新的住房政策违背了市长的承诺时许多市民都很生气.

vel.arx：这是cad的激活命令，删除后CAD将无法正常使用。建议下载一些误杀率比较低的杀毒软件：例如腾讯电脑管家，卡巴斯基等。如果已经删除vel.arx导致cad不可用，可以通过隔离区进行恢复。更新杀毒软件，更新病毒库可以减少误报几率。

water supply and drainage project给水排水工程双语对照例句:1.Design code of water supply and drainage for substation. 变电所给水排水设计规程。2.Introduction of water supply and drainage design for qingpu branch of shanghaihome cosmetics united co. 上海家化联合公司青浦分厂给排水设计介绍。

给水与排水water supply是供水的意思drainage 是排水的意思，倾向于指排污水；给排水是工程中的一个重要专业方向

dietary supplement英[u02c8dau026au026au02ccteri: u02c8su028cpliment]美[u02c8dau026au026au02cctu025bri u02c8su028cplu0259mu0259nt]膳食补充品Innovative Beverage says that its Drank is a dietary supplement and that it is working closely with FDA to"clear up any confusion. "该公司说，Drank是一种膳食补充品，它正在与FDA密切合作，澄清任何疑惑。

是虚拟语气，不是没倒嘛

broadway photo supply limited 百老汇摄影器材有限公司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

suppose 普通用词，指对事物进行假设、设想，所假设的事可能是真实的，也可能是虚 构的（从句需用虚拟语气）。 1）Supposehe is absent, what shall we do? 假设缺席了，我们该怎么办？ 2）Let"s supposethat they had not helped us.What would have happened? 假定他们不曾帮助我们，会发生什么情况呢? 3）Sopposethat one day scientists pick up a transmission which they thinkis generated by aliens. 假设有一天科学家收到了他们认为是外星人发射的信号。 4）Myths are accounts of important events that aresupposed to have occurred some time during a culture"sformative years. 神话是描述那些据说是发生的时间在某一个文化的形成年的代重要事件。assume 指主观上毫无根据的武断推测或不合逻辑的推理。1）It is entirelywrong to assume that your wealth entitles you tospecial respect. 你认为财富能使你享特特殊礼遇，那就大错特错了。 2）I assumed that he wouldnot come to attend the funeral. 我猜想他不会来参加葬礼。 3）Some people assume that thereis life on the other planets when they see UFOs. 有些人看到了不明飞行物就想当然地推测其他的行星上有生命。presume 与assume一样，指对事物进行推测，不同的是侧重指以过去的经验或 根据现实的情况作出合乎逻揖的推测和设想。 1）We cannot presume theexistence of life on other planets. 我们不能推定其他行星上没有生物。 2）John didn"t say whenhe would return, but I presume that he"ll be backfor dinner. 约翰没有说他什么时候回来,但我推测他将回来吃晚饭的。 3）One is presumed to beinnocent before the judge makes the final decision that he isguilty of the crime. 在法官作出最终的判决一个人有罪之前，他是被假定无罪的希望采纳哦！

Your browser is not supported.您的浏览器不支持。browser英 [u02c8brau028azu0259(r)] 美 [u02c8brau028azu025a]n.浏览程序； 浏览器（用于在互联网上查阅信息）； 浏览图书报刊者； 逛商店的人浏览器；浏览者；网页浏览器；自带浏览器复数： browsers supported英 [su0259"pu0254:tu026ad] 美 [su0259"pu0254:tu026ad]v.支持( support的过去式和过去分词 )； 帮助； 支撑； 维持负载；支；支承的；负载型

使用druid报错not support oracle driver 1.0, 是因为有多个驱动包造成的。在jre的ext目录下发现了class12.jar

application.properties中 spring.datasource.druid.filters=stat,wall 去掉wall 原因：Druid目前支持mysql和oracle、sql server。

提供的证件都invalid.Please再次尝试或联系你的系统管理员寻求帮助。

就这个最好sustain

The geochemical or long-term carbon cycle primarily involves the exchange of carbon between the ‘surficial"and ‘geologic"reservoirs. The former comprise atmosphere，oceans，biosphere， soils，and exchangeable sediments in the marine environment ( Fig. 1) while the latter include crustal rocks and deeply buried sediments in addition to the underlying mantle. How carbon is partitioned between the various reservoirs of the surficial system and between surficial and geologic reservoirs is what sets the concentration of CO2in the atmosphere. Life，and the cycle of organic carbon，as well as its geological ( and subsequent fossil fuel exhumation ) is of particular importance in this regard. The cycle of carbon in its inorganic，calcium carbonate ( CaCO3) form also affects atmospheric CO2，but by more subtle means. It also plays a fundamental role in regulating ocean chemistry and pH—a major factor in the viability of calcareous marine organisms.Carbonate precipitation and burialToday，the surface of the ocean is everywhere more than saturated ( over-saturated) with respect to the solid carbonate phase，with a mean value for the saturation state ( Ω: saturation state of the solution，also known as the solubility ratio) of calcite of 4. 8. In other words，the minimum thermodynamical requirement for calcite to precipitate is exceeded by a factor of almost 5. Despite this，the spontaneous precipitation of CaCO3from the water column is not observed in the ocean. This is because the initial step of crystal nucleation is kinetically unfavorable，and experimentally，spontaneous ( homogeneous) nucleation does not occur in sea water solutions until Ωcalcite＞ ～ 20 – 25 ( Ω = ［Ca2+］×［CO2-3］ /Ksp) . Although CaCO3precipitation occurs as cements and coatings in the marine environment，it is primarily associated with the activities of living organisms， particularly corals， benthic shelly animals， plankton species such as coccolithophores and foraminifera，and pteropods，and where it takes place under direct metabolic control. In comparison，carbonate deposition in fresh-water systems is of only minor importance globally，and will not be discussed further here.While not in itself sufficient to drive substantial abiotic precipitation，the saturation state of the modern ocean surface is favorable to the preservation of carbonates deposited in shallow water ( neritic) environments. Long-term accumulation of this material can result in the formation of extensive marine topographical features such as barrier reefs and carbonate banks and platforms. A different fate awaits CaCO3precipitated in the open ocean by plankton such as coccolithophores and foraminifera，however. This is because oceanic waters become increasingly less saturated with depth. Below the depth of the saturation horizon，conditions become under-saturated ( Ω ＜ 1. 0) and carbonate will start to dissolve. In the modern ocean the calcite saturation horizon lies at about 4500 m in the Atlantic and ～ 3000 m in the Pacific Ocean. Within a further 1000 m sediments are often completely devoid of carbonate particles ( the carbonate compensation depth， or CCD) . Topographic highs on the ocean floor such as the mid-Atlantic ridge can thus be picked out by sediments rich in CaCO3while the adjacent deep basins are low in % CaCO3. The visual effect has been likened to snow-capped mountains. The pressure induced surface-to-deep vertical contrast in Ω is further enhanced by the respiration of organic matter and release of metabolic CO2 in the ocean interior which suppresses the ambient carbonate ion concentration and thus Ω. The greater accumulation of metabolic CO2in the older water masses of the deep Pacific explains why the sea-floor there is much poorer in % CaCO3compared to the Atlantic at a similar depth.Fig. 1 The global biogeochemical cycling of calcium carbonate. ( a) Modes of CaCO3transformation and recycling within the surficial system and loss to the geological reservoir ( labeled ‘1 " through ‘4 ") .① Precipitation of calcite by coccolithophores and foraminifera in the open ocean; Ca+2+ 2HCO－3→CaCO3+CO2( aq)+ H2O. ② Carbonate reaching deep-sea sediments will dissolve during early diagenesis if the bottom water is under-saturated and / or the organic matter flux to the sediments is sufficiently high. ③ Precipitation of CaCO3by corals and shelly animals，with a significant fraction as the aragonite polymorph. Because modern surface waters are over-saturated relatively little of this carbonate dissolves in situ，and instead contributes to the formation of reefal structures or is exported to the adjoining continental slopes. ④ Precipitation of CaCO3 results in higher pCO2at the surface，driving a net transfer of CO2from the ocean to the atmosphere.( b) Modes of CaCO3transformation and recycling within the geologic reservoirs and return to the surficial system ( labeled“5”through“8”) . ⑤ CaCO3laid down in shallow seas as platform and reef carbonates and chalks can be uplifted and exposed to erosion through rifting and mountain-building episodes. CaCO3can then be directly recycled; CO2+ H2O + CaCO3→Ca+2+ 2HCO－3. ⑥ Thermal breakdown of carbonates subducted into the mantle or deeply buried. The decarbonation reaction involved is essentially the reverse of silicate weathering，and results in the creation of calcium silicates and release of CO2; CaCO3+ SiO2→CO2+ CaSiO3.⑦ Weathering of silicate rocks; 2CO2+ H2O + CaSiO3→Ca+2+ 2HCO－3+ SiO2. ⑧ Emission to the atmosphere of CO2produced through decarbonation. This closes the carbon cycle on the very longest time-scales.Unfortunately，the carbonate cycle does not conform to this simple picture，and a significant fraction of CaCO3appears to dissolve in the water column even before it can reach the sediment surface. This has been something of an enigma because the reduction in carbonate flux measured by sediment traps occurs well above the depth at which calcite becomes thermodynamically unstable. Dissolution of carbonate particles in acidic digestive conditions of zooplankton guts has been one proposed mechanism. Acidic micro-environments within individual ‘marine snow " aggregates may also be important. Another possible explanation surrounds the aragonite polymorph because it becomes susceptible to dissolution at much shallower depths than calcite under the same ambient conditions. In support of this are recent estimates of the depth at which most CaCO3 dissolution occurs in the ocean which appears to correspond to the aragonite saturation horizon. However，calculations suggest that solute release from sinking pteropod shells，the main aragonite product in the open ocean，should mostly occur much deeper than this. Dissolution of aragonite also does not help explain how 65% of calcitic foraminiferal tests can be lost at shallow depths. This uncertainty is of concern because a full appreciation of the controls of atmospheric CO2and response to global change requires an understanding of the dissolution and the depth of recycling of CaCO3in the water column.Overall，more than 80 % of all carbonate precipitated in the open ocean dissolves either in the water column or within the uppermost layers of the underlying sediments. The remainder，some 1 Gt CaCO3yr－ 1accumulates in deep-sea sediments. This burial loss，to which can be added as much as another 1 Gt CaCO3yr－ 1of deposition in neritic environments ( although the uncertainty in this figure is substantial) ，must somehow be balanced if the ocean is not to run out of calcium ions! This is achieved through the weathering of carbonate and silicate rocks.Weathering and Carbonate RecyclingThe weathering of calcium carbonate and calcium silicate minerals in soils and at exposed rock surfaces helps balance the CaCO3sedimentation loss by unlocking Ca2 +from the geologic reservoir. Alteration of ocean crust by percolating fluids adds an additional but more minor contribution. The weathering reactions ( see Fig. 1b; ⑤ and ⑦) provide the other raw material necessary for carbonate precipitation— bicarbonate ions ( HCO－3) . However，because the transformation 2CO2→2HCO－3( Fig. 1b; ⑦) is internal to the surficial system and does not represent a source of new carbon，the component of CaCO3burial derived from silicate rock weathering represents a loss of carbon to the geologic reservoir. This must be replaced on the long-term，achieved through the release of CO2to the atmosphere from volcanic sources. ( In contrast，the weathering and burial of CaCO3results into net loss or gain of CO2to the surficial system) .A powerful regulatory mechanism of the Earth system arises because weathering rates respond to surface temperature and atmospheric CO2while simultaneously silicate weathering rates control the rate of transformation CO2→HCO－3and thus rate of loss of carbon through CaCO3burial. This is a negative feedback system and acts to regulate the concentration of CO2in the atmosphere over hundreds of thousands of years.Buried carbonate is eventually recycled back from the geologic reservoir. This can occur if carbonates laid down in shallow seas such as limestones or chalks are subsequently uplifted and exposed to weathering as a result of mountain building episodes. However，carbonates deposited in open ocean sediments are only infrequently exposed at the Earth"s surface，as ophiolite complexes—portions of the oceanic crust and overlying sediments that have been trapped between colliding cratonic blocks and uplifted. Instead，the primary recycling of deep-sea CaCO3occurs through subduction into the upper mantle and decarbonation ( Fig. 1b; ⑥) .At this point it is important to recognize that carbonate burial represents the principal geologic mechanism of CO2removal from the ocean and atmosphere. However，the act of precipitating CaCO3has the effect of re-partitioning dissolved carbon in the surface ocean into CO2 ( aq)，raising ambient pCO2and pH. Thus，precipitation and deposition of CaCO3have the short-term effect of increasing the concentration of CO2in the atmosphere at the expense of the ocean carbon inventory，but at the same time represents the ultimate long-term sink for CO2.Both texts are selected from: The role of the global carbonate cycle in the regulation and evolution of the Earth system，Earth and Planetary Science Letters 234，2005: 299 － 315By: Andy Ridgwell，Department of Earth and Ocean Sciences，The University of British Columbia，6339 Stores Road，Vancouver，British Columbia，Canada V6T 1Z4andRichard E. Zeebe，University of Hawaii at Manoa，SOEST，Honolulu，HI，United StatesNew words and expressionsPart A地球科学专业英语Part B地球科学专业英语

　中文名：珍妮·瓦德又名:珍妮·韦德/珍妮·维德　　英文名： Jenny Wade 　　生日： 1980年10月6日 　　出生地：美国奥里良州 　　星座： 天枰座 　　性别： 女 　　地区： 美国国 　　职业： 演员、模特　　imdb编码：nm1023127　　外貌可人，声音甜美，身材匀称的珍妮·维德1980年10月6日出生于美国奥里良州。儿时的珍妮就因为她那小天使般的容貌，光滑白皙的肌肤受到了比同龄人更多的关爱，而大荧幕上那一位位身着华服，光芒万丈四周总不乏绅士环伺的女明星，正是小珍妮心中向往的职业。自从珍妮·维德踏足好莱坞接到的角色大都是爱情轻喜剧电影里一些雷同的花瓶配角，珍妮的表演潜力迟迟无法得以展现。2005年是珍妮·维德大有建树一年，由当年的一部惊悚片《红眼航班》珍妮的戏路开始渐渐拓宽......接下来同一年的恐怖片(黑色喜剧？)《兽餐》以其极尽血腥暴力的镜头赢得了一杆恐怖片簇拥的追捧，也因为真实刻画了那个“鲜红”无助 甜美的女侍者“Honey pie”，使得饰演者珍妮·维德得以被影迷所认同。自此珍妮出演恐怖片中角色的机会得到成倍增长，并于同年在《绝命圣诞夜》中出色的扮演了“Cupcake”一角。从此珍妮的片约不断部部都有所突破，一步一个脚印的继续着她的荧幕甜心路线，就像她在剧集《Reaper》(狙魔人/ 恶灵猎人)中扮演的恶魔美人“Nina”，看起来就那么惹人喜爱看上去就很美好。愿珍妮·维德在她冉冉上升的演艺事业道路上能够有新的突破，能继续那样无邪中带点“邪恶”的美好下去。1 表演作品编辑本段 1.1 电影作品　　兄弟Brothers(2009) ------- Tina　求欢地带The Strip (2009)------- Melissa　　兽宴3：快乐结局/兽餐3/人肉盛宴3/ 盛宴3Feast 3: The Happy Finish(2008) ------- Honey Pie 　　兽宴2/兽餐2/盛宴2/食人宴2/人肉盛宴2 Feast 2: Sloppy Seconds (2008) ------- Honey Pie 　　美味情缘/不快餐客/毫无保留/美味关系/不速食客/ No Reservations (2007) ------- Leah　　爱情是毒药Love Is the Drug (2006) ------- Erin Sutherland　　怪兽婆婆/邪恶亲家母/新抱大站战哥斯奶 Monster-in-Law (2005) ------- Viola"s Young Replacement　　"Project Greenlight 3" ------- (2005) 　　绝命圣诞夜/老大冻未条/冰雪圣诞夜 The Ice Harvest (2005) ------- Cupcake　　盛宴/兽餐/人肉盛宴/兽宴 Feast ------- (2005) 　　红眼/夜航杀机/赤眼玄机/长途吓机/ 红眼航班Red Eye (2005) ------- Coffee Shop Girl　　流言蜚语 Rumor Has It(2005) ------- Nikki　　赤裸酒店 Naked Hotel ------- (2003) 　　急救爱情狂/护士贝蒂/真爱来找碴 (2000) Nurse Betty ------- Diner Waitress　　Tumble ------- (2000) 　　不穿 "Undressed" ------- (1999)

代码做测试：import curses myscreen = curses.initscr()myscreen.border(0)myscreen.addstr(12, 25, "Python curses in action!") myscreen.refresh()myscreen.getch()

你玩的是《暗黑魔法师：崛起》吗？　　不要直接进游戏　　　用文件夹内的options（游戏设置）进　　　就行了

eggs for opps and suppo对有机磷农药及支持鸡蛋

你安装protege的路径protegeUninstallProtege>"Uninstall Protege.exe" LAX_VM 你安装的32位的jdk路径jdk-7u72-windows-i586injava.exe"这个问题的原因是你安装的protege有可能是不自带jvm的版本, 然后就需要操作系统上安装的jvm，但是操作系统安装的jvm有可能是32位的有可能是64位的，但是protege是32位的话一样可以安装在操作系统上，但是这个时候如果操作系统的jvm是64位就不支持protege的需要的jvm环境啦，所以一定要满足protege启动或者卸载程序的JVM运行环境。一句话：如果protege不自带JVM，那么protege的位数要和操作系统用的JVM的位数一致！ 当然操作系统安装多个JVM ，在命令行运行时可以指定使用那个即可。不需要麻烦的修改注册表，修改环境变量乱七八糟的。上面那行命令会帮你解决的。下面是理论解释

你好，dazu是加上去，此外的意思Dazu muss man sagen, dass Leifeng ein guter Kamerad ist. 此外要说，雷锋是个好同志。sonst的意思是不然Du musst Wasser trinken, sonst bleibt du weiter krank. 你必须喝水，不然还得继续病。Brühe Suppe两个词都是汤的意思，但是Brühe更多是表达用汤料和开水直接冲泡出来的，有很多味精的汤，或是直接描述这种固体的冲泡汤料。而suppe就是浓一点有很多西红柿或是奶油的浓汤了。

含这个 orm 的jar包如3.springframework.0.1.1.RELEASE.0 版在org.orm-3

我有可以送你的，要的话留言给我