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药物分析前沿是啥呢? 药物分析前沿是啥呢查看更多 3个回答 . 4人已关注
Lewis酸碱性比较 IR测试求助? K+与Zn2+相比,哪个的Lewi S酸 性较强啊?K-O键的IR 测试 特征峰在哪个位置?查看更多 3个回答 . 20人已关注
求助,热力学途径求功问题? 第23题的(3)问,那个条件途径看不懂是什么意思?答案解析中划线部分不明白,它是如何求出b值的?查看更多 1个回答 . 20人已关注
接触三氟化硼乙醚,手指痒且蜕皮,还肿起来,群里朋友有办法吗? 各位朋友,本人目前接触三 氟化硼 乙醚 ,手指痒且蜕皮,还肿起来,如何操作可以避免,群里朋友有办法吗?查看更多 7个回答 . 30人已关注
质子交换膜只能通过质子其它离子都不行吗? 质子膜是只能通过质子吗?溶液中有其它阳离子离子Na,K这些,还有 阴离子 Cl-,NO3-可以通过吗查看更多 6个回答 . 18人已关注
怎么计算比厌氧氨氧化活性(SAA)? (求助)比厌氧氨氧化活性怎么计算呀?~~~~~~~~~~~~~~~~~~~~~~~~~~·谢谢~~~~~~查看更多 3个回答 . 6人已关注
关于扣式锂电电极片大小的问题? 求高手解答:? ? 装扣式锂电时,电极片大小多大比较合适。太大或太小了有什么影响,在装扣式锂电时,电极片一定要是圆形的吗,方形的行不行?查看更多 7个回答 . 28人已关注
求助 硅溶胶的制备工艺? 求助 硅溶胶 的制备工艺用 水玻璃 离子交换如何制取硅溶胶??具体的工艺条件是什么就是用工业水玻璃 如何控制条件制备 硅溶胶水玻璃稀释到具体什么浓度??,每一步的具体步骤是什么具体步骤和具体条件查看更多 5个回答 . 5人已关注
检测重金属Pb电化学方法,用方波伏安法如何测? 在文献里查到大多数人用SWASV测,我们用的是电化学CHI660E,里面没有这个方法。我看到有人说可以先用I-T富集,然后用方波伏安法剥离。我用的是这种方法,但是得到的图形很怪异,如下图,请问是什么原因?大家用SWASV检测时都怎么设置的? ? ? 缓冲液 是自配的pH4.5醋酸 醋酸钠溶液 0.1M,配方是2.93g 醋酸钠 ,3.86g醋酸,加水至1L,这样配缓冲液有问题吗? ? ? 富集时电压选择-1V,200s。如何判断Pb2+富集到了电极上? QQ截图20160120172752.png QQ截图20160118193544.png QQ截图20160118193640.png查看更多 5个回答 . 27人已关注
一篇关于海水电池较好的专利(美国)? 关于海水电池较好的专利,与各位共享!海水电池采用活泼金属,如镁、铝合金,作为阳极;采用AgCl,Cu2Cl2等惰性物质作为阴极;利用海水作为 电解液 。在放电过程中,阳极材料失去电子而溶解,这些电子通过外接电路对外做功,然后在惰性的阴极上与溶解在海水里的 氧气 结合形成氢氧根离子。由于采用海水作为电解液,电池本身无需携带电解液从而减小了电池的重量,使电池具有较高的能量密度。查看更多 0个回答 . 11人已关注
做聚氨酯的,求帮助。? 三乙基二胺 作为 聚氨酯 的 催化剂 ,固体怎么加?需要溶剂溶解,还是加热溶解?查看更多 6个回答 . 8人已关注
用EO数为5,7,9来合成脂肪醇聚氧乙烯醚磺酸钠做驱油剂可行吗? 我想做脂肪醇 聚氧乙烯醚 磺酸钠,我看文献上是用C12,14醇,EO数是3 合成脂肪 醇聚氧乙烯醚磺酸钠,课题要有所创新,我就想改用其他醇,或者用别的EO数来合成,就可以做课题了,大家觉得我的想法可行吗,谢谢查看更多 6个回答 . 15人已关注
大气化学名师之-保罗克鲁琴? (本文转自Encyclopedia of World Biography) Paul J. Crutzen (born 1933) has led fellow scientists in the attempt to map out the chemicals that affect the ozone layer. He has been instrumental in learning how the ozone layer is formed and destroyed, and in uncovering the role industries play in its destruction. He was awarded the Nobel Prize in Chemistry in 1995 for discovering certain chemical compounds that reduce the ozone layer, and that certain bacteria in the soil can determine its thickness. Crutzen was born on December 3, 1933, in Holland to Anna Gurk and Jozef Crutzen. He had one sister. Crutzen was raised in a rather cosmopolitan atmosphere filled with international ideas and attitudes. He grew up in a poor family in Nazi-occupied Holland. During his elementary school days World War II was going on, and he and his classmates had to move to a new building after their school was taken over by Nazi troops. Crutzen especially remembered the last winter of the war in 1944–45. He wrote in his autobiography on the Nobel Prize website, "During the cold 'hongerwinter' (winter of famine) of 1944–45, there was a severe lack of food and heating fuels. Also water for drinking, cooking and washing was available only in limited quantities for a few hours per day, causing poor hygienic conditions. Many died of hunger and disease, including several of my schoolmates." Intention to Build Houses Crutzen was one of the few children who was able to graduate from elementary school on time; the rest were kept back a year. At the time not all children were allowed to attend high school, but Crutzen was selected to do just that after he did very well on the entrance exam. He went to the Hogere Burgerschool, where he focused on natural sciences and learned to speak French, English, and German. He enjoyed playing soccer and bicycling and loved distance ice skating. He was also interested in chess, and at school he was interested in physics and math, not really liking chemistry at all. After graduation he went on to a two-year college, the Middelbare Technische School, because he could not afford to go to a university. He graduated with a degree in civil engineering in 1954. With this degree under his belt he set out to design bridges and houses. Soon after graduation, while he was vacationing in Switzerland, Crutzen met Tertu Soininen. The couple married two years later and moved to Gavle, Sweden, in 1958, where Crutzen had obtained a job at a building construction bureau. The Crutzens had a daughter, Ilona, that December. Another girl, Sylvia, was born in March of 1964. Switched to Atmospheric Chemistry What Crutzen really wanted professionally, however, was to work for an academic department, not a building bureau, so when the opportunity presented itself he applied for a job as a computer programmer at the Institute of Meteorology at the University of Stockholm. He had no experience in computers, but at the time there were few who did, and he was accepted from a large candidate pool to take on the position. The family moved to Stockholm. He was originally interested in mathematics, but soon lost his passion for it in favor of atmospheric chemistry. While working, Crutzen also earned a doctorate in meteorology at the university. In 1965 Crutzen went to help a U.S. scientist develop a model of the stratosphere. It was this project that awakened Crutzen's interest in the chemical makeup of the ozone layer. He started reading everything he could on the subject, his interest growing with each new piece of information. It also gave him an idea of the state of research on the ozone layer at that time. He went back to Sweden with a new purpose for his degree research. Crutzen stated in his autobiography on the Nobel Prize website, "Instead of the initially proposed research project, I preferred research on stratospheric chemistry, which was generously accepted." Researched Ozone Layer At the time the current research areas at the University of Stockholm were dynamics, the physics of clouds, the carbon cycle, studies of the chemical composition of rainwater, and especially acid rain, which was one of the hottest research topics at that time. However, Crutzen maintained an interest in studying the ozone layer. Ozone itself is a bluish gas that has a strong scent and is irritating to living organisms. It has three oxygen atoms and forms naturally in the atmosphere through a process called photochemical reaction, having to do with the chemical reaction of light. The ozone layer is located ten miles above the surface of the Earth and is approximately 20 to 30 miles thick. Its purpose is to absorb the ultraviolet radiation that the sun emits. Atmospheric warming occurs when that layer begins to deplete. In 1970 Crutzen discovered that certain bacteria in the soil gave off a nitrous oxide gas which rose all the way to the stratosphere, where it was changed by a photochemical process into two chemicals, nitric oxide and nitrogen dioxide. He learned that these two gases were part of what caused the ozone to shrink in size. This one realization led scientists across the globe to examine chemicals found on earth to see how they affected the ozone layer's size. Studied Effects of Smoke and Nuclear War Crutzen went on from this research to become in 1977 the director of the National Center for Atmospheric Research (NCAR) in Boulder, Colorado. From there he worked on how burning trees and brush in Brazil effected the atmosphere. In Brazil farmers would clear the forests every year by burning them down. It was thought that this burning was releasing carbon monoxide and other carbon compounds into the air that were causing the greenhouse effect, the warming of the atmosphere. When Crutzen collected samples and did his research, however, he found out that the exact opposite was happening. The yearly smoke was actually decreasing the amount of carbon dioxide in the atmosphere. This discovery intrigued Crutzen, and he went on to study the effects of other kinds of smoke on the atmosphere, especially the smoke that would come from a global disaster such as a nuclear war. Once he made his interest in researching such a topic known, several sponsors came forward. The journal Ambio paid Crutzen and his University of Colorado colleague John Birks to study how a nuclear war would effect the planet. The pair put together a model of a worldwide nuclear war. According to the scientists nuclear war would have a fallout of black carbon soot that would result from fires raging across the planet. This soot would absorb up to 99 percent of the sunlight that the Earth needs to survive. This would cause the entire planet to be thrown into a state of perpetual winter so vast that it would destroy every living thing. For proposing this theory Crutzen was named "Scientist of the Year" by Discover magazine in 1984 and was awarded the esteemed Tyler Award in 1988. When these theories and others about the destructive nature of certain chemicals on the ozone layer came to the attention of the general public and to governments around the world, an international treaty was drawn up in 1987. Called the Montreal Protocol, it was negotiated by the United Nations and was eventually signed by 70 countries. The protocol stated that these countries would phase out, no matter how slowly, the production of chlorofluorocarbons and other ozone-depleting chemicals by the year 2000. The United States managed to stop producing things with the harmful chemicals in them by the year 1995, although it still remained the leading producer of carbon emissions in the world. The hole in the ozone layer over the South Pole was still increasing in 2000, but it was thought that it was because of existing products with the harmful chemicals in them that would take a while to deplete. A full reversal of the problem was not expected to take place for hundreds of years. Crutzen stayed at the NCAR until 1980. At the same time he taught classes at Colorado State University in the department of Atmospheric Sciences. He became director of the Atmospheric Chemistry Department at Germany's Max Planck Institute for Chemistry in 1980 and remained as such until 2000. From 1992 on he taught part-time at Scripps Institution of Oceanography at the University of California and also at Utrecht University's Institute for Marine and Atmospheric Sciences in the Netherlands. Suggested Interim Solution to Ozone Problems In 2006 Crutzen was acknowledged to have come up with a solution for helping to stave off the effects of global warming. He suggested that the chemical composition of the Earth's upper atmosphere be altered. Attempts to stave off man-made alterations to the atmosphere had been so meager that according to Crutzen a more drastic approach was necessary. His suggestion was to release some sulphur into the upper atmosphere. The sulphur should reflect sunlight and the heat from it back into space. It was a very controversial solution, but has been receiving some serious consideration because of Crutzen's known track record of excellence in the past. The sulphur could either be scattered by balloons designed for high altitude flight or could be shot into the air by heavy artillery shells. According to the London Independent , "Such 'geo-engineering' of the climate has been suggested before, but Professor Crutzen goes much further by drawing up a detailed model of how it can be done, the timescales involved, and the costs." The idea has raised objections around the globe, most often because such an operation, scientists fear, would be seen as a quick fix and then governments would cease to search for more permanent solutions to the problem. Crutzen has argued that this would be a stopgap measure and that pressures on governments to improve their emissions would remain. In his opinion this would be a way to temporarily reduce global warming issues while countries worked more fervently to change their practices. His plan was modeled in part on the eruption of the Mount Pinatubo volcano in 1991. Thousands of tons of sulphur were thrown into the air when the volcano erupted causing temperatures around the globe to decrease. Putting the sulphur into the stratosphere rather than lower down, as in the case of the volcano, would create a year or two of lower temperatures rather than just a few weeks. The project would cost about $25 to $50 billion, but it is Crutzen's belief that that cost is nothing to what global warming is doing to all life on Earth. Because of his contributions to modern science, Crutzen was elected in 2006 to become a foreign member of the Royal Society, the United Kingdom's national academy of science and the world's oldest scientific academy in uninterrupted existence. As of 2007 he continued his studies into improving the atmosphere. Books Notable Scientists: From 1900 to the Present , Gale Group, 2001. World of Chemistry , 2 volumes, Gale Group, 1999. World of Earth Science , Gale, 2003. World of Scientific Discovery , 2nd edition, Gale Group, 1999. Periodicals Environment , April 2004; October 2005. Independent (London, England), July 31, 2006. Times (London, England), October 12, 1995. Times of India , August 1, 2006. Online "Paul J. Crutzen, Noble Prize Website , http://www.nobel.se/chemistry/laureates/1995/crutzen-autobio.html (January 2, 2007). Read more: http://www.notablebiographies.co ... Crutzen-Paul-J.html查看更多 3个回答 . 24人已关注
请问最新的高分子材料有哪些,导师要求写三个,急求。? 请问最新的高分子材料有哪些,导师要求写三个,急求。明天就跟导师上报,然后写PPT,我自己没百度出来,求前辈指导指导我。真心感谢!查看更多 2个回答 . 2人已关注
高分子溶解问题,? 高分子化合物溶解在溶剂中,本来全溶,后来出了一层 牛奶 膜那种膜,不溶,如何能把他溶了,加热,换溶剂行么查看更多 5个回答 . 20人已关注
询问Nafion膜的使用前处理和使用后保存? 本人第一次使用Nafion膜,请问使用前应当如何处理,使用后如何保存?有没有使用寿命?谢谢查看更多 4个回答 . 2人已关注
反应釜中气体产物的定量? 我现在做的是高温高压加氢反应,我的主要产物都是气体。不知道大家做的 反应釜 中的气体都是怎么定量的?查看更多 7个回答 . 16人已关注
乙酰丙酸和5-羟甲基糠醛? 乙酰丙酸 和 5-羟甲基 糠醛在HPLC上怎么分开呢?调过流速和梯度洗脱,没有分开,用的是 甲醇 /水。希望大家指点,讨论一下,万分感谢!查看更多 3个回答 . 4人已关注
有关物质进样顺序问题? 有关物质 流动相 是等度的, 色谱柱 已经平衡了两个多小时,第一针没有进空白,走的供试品溶液。然后出了一个平时没有的 杂质 峰,我们领导就说这个问题的原因是第一针没有走空白。我想请教一下进空白对这个有什么影响?查看更多 2个回答 . 25人已关注
考研物化,问个题,没有思路? 第5题老师来吧,,,,]CAWQ{5TTX}T~1)F1I3TW`C.jpg查看更多 6个回答 . 12人已关注
简介
职业:宏正(福建)化学品有限公司 - 仪表工
学校:西华师范大学 - 历史文化学院
地区:河南省
个人简介:人的活动如果没有理想的鼓舞,就会变得空虚而渺小。查看更多
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