Atmospheric carbon dioxide concentrations before 2.2 billion years ago

The composition of the Earth's early atmosphere is a subject of continuing debate. In particular, it has been suggested that elevated concentrations of atmospheric carbon dioxide would have been necessary to maintain normal surface temperatures in the face of lower solar luminosity in early Earth history. Fossil weathering profiles, known as palaeosols, have provided semi-quantitative constraints on atmospheric oxygen partial pressure (pO2) before 2.2 Gyr ago. Here we use the same well studied palaeosols to constrain atmospheric pCO2 between 2.75 and 2.2 Gyr ago. The observation that iron lost from the tops of these profiles was reprecipitated lower down as iron silicate minerals, rather than as iron carbonate, indicates that atmospheric pCO2 must have been less than 10(-1.4) atm--about 100 times today's level of 360 p.p.m., and at least five times lower than that required in one-dimensional climate models to compensate for lower solar luminosity at 2.75 Gyr. Our results suggest that either the Earth's early climate was much more sensitive to increases in pCO2 than has been thought, or that one or more greenhouse gases other than CO2 contributed significantly to the atmosphere's radiative balance during the late Archaean and early Proterozoic eons.     

高浓度酿造啤酒工艺控制

本文叙述了高浓度酿造啤酒的过程中麦芽制备、啤酒发酵、稀释水处理、酒水混合和啤酒风味等问题。     

Kinetic model for the smectite to illite transformation in active geothermal systems

The smectite to illite transformation in active geothermal systems of New Zealand can be simulated by a first-order reaction kinetic model, which provides direct estimates about the minumum ages of active geothermal systems themselves. The derived kinetic values show that the smectite to illite transformation is sensitive to both temperature and time.     

Determination of tectonic background for sedimentary basin from sandstone geochemistry

The chemical composition of sedimentary rocks is mainly controlled by source rocks. Through examining chemical composition of terrigenous rocks, the tectonic evolution of a sedimentary basin can be modeled. The Turpan Basin belongs to a continental sedimentary basin and its source rocks are derived from the upper continental crust.     

CAD系统中面向对象用户界面的设计与研究

介绍铁路站场ＣＡＤ系统中面向对象用户界面的设计与研究,该系统用户界面的设计充分分考虑了铁路站场ＣＡＤ系统的特点和工程应用,采用面向对象的方法与技术,实现了一个高度图形化和交互式,适用于铁路站场设计工作需要的图用户界面。     

Fe3Al合金的高温变形行为

用载荷松弛法对Ｆｅ－２８Ａｌ－２Ｔｉ合金在较高温度下的变形行为进行了研究．测定了Ｆｅ－２８Ａｌ－２Ｔｉ合金在高温变形时的载荷松弛曲线、应力减小因子Ｙ及激活能值,并对试样进行了显微结构观察．结果表明,Ｆｅ－２８Ａｌ－２Ｔｉ合金的高温变形是一个亚晶界吸收位错,而且不断向大角晶界转变的过程．     

新疆植物物种多样性的特点分析

新疆土地面积占全国１／６,约１６４．６８万ｋｍ２,位于欧亚大陆腹地,景观与地形复杂,气候变化明显,植物种质资源特殊。新疆高等植物４０８１种（包括２２９亚种、变种与变型）,隶属于１６１科８７７属,新疆植物多样性的特点如下：１）单种科、单种属及寡种属丰富,分别为８０科、３７４属及３１５属。２）短命及类短命植物丰富,已知的有２３２种,隶属于２７科１１４属,主要分布于准噶尔盆地边缘。３）新疆特有种稀少,但中国、塔什库尔干、天山、阿尔泰山、昆仑山及帕米尔高原的特有种特别丰富。４）近５０年以来,发表的新疆新分类群较多,有３６０余种。５）中国仅分布于新疆的植物有１７７３种,其中１００种以上的科有４科（豆科,伞形科,菊科,禾本科）,总数为６２２种;８０种以上的科也有４科,总数为３３１种。最后,对新疆极端环境下的植物种质资源及栽培植物的野生近缘种的保护问题提出了几点建议。     

美东地区罗德河流域地下水中铝形态分布的化学平衡模式计算

美东地区的罗德河流域遭受着严重的酸沉降侵蚀．在酸性条件下,铝从土壤中大量溶解并迁移到水环境中．地表水中升高的铝浓度对鱼类产生毒害,监测地表水和土壤水中的铝形态及浓度变化已成为问题的关键．本文报导了用化学平衡模式计算法分析美东地区罗德河流域地下水中的铝形态分布,获得了有价值的结论     

超滤法分级和纯化蛋白质的现状和前景(英文)

超滤法具有高产率、低成本、容易放大等显著优点,但其低选择性一直限制其在生物蛋白制品的分级和纯化中的应用。本文总结和分析了超滤法用于蛋白质分级和纯化的近期研究成果,对其低选择性的原因进行了分析,提出并论证了提高超滤选择性的技术途径。