四川盆地海相三叠系硫同位素组成及其地质意义

系统整理研究了四川盆地海相三叠系硬石膏和卤水的硫同位素组成、演化特点及其地质意义。这对促进四川和全球海相三叠系硫酸盐硫同位素的研究有重要参考价值。     

Diagenesis of Upper Carboniferous rocks in the Ouachita foreland shelf in mid-continent USA: an overview of widespread effects of a Variscan-equivalent orogeny

Diagenesis of Upper Carboniferous foreland shelf rocks in southeastern Kansas took place at temperatures as high as 100–150° C at a depth of less than 2 km. High temperatures are the result of the long distance (hundreds of kilometers) advection of groundwater related to collisional orogeny in the Ouachita tectonic belt to the south. Orogenic activity in the Ouachita area was broadly Late Carboniferous, equivalent to the Variscan activity of Europe. Mississippi Valley-type Pb-Zn deposits and oil and gas fields in the US midcontinent and elsewhere are commonly attributed to regional groundwater flow resulting from such collisional events. This paper describes the diagenesis and thermal effects in sandstone and limestone of Upper Carboniferous siliciclastic and limestone-shale cyclothems, the purported confining layer of a supposed regional aquifer. Diagenesis took place in early, intermediate, and late stages. Many intermediate and late stage events in the sandstones have equivalents in the limestones, suggesting that the causes were regional. The sandstone paragenesis includes siderite cement (early stage), quartz overgrowths (intermediate stage), dissolution of feldspar and carbonates, followed by minor Fe calcite, pore-filling kaolinite and sub-poikilotopic Ca ankerite (late stage). The limestone paragenesis includes calcite cement (early stage); megaquartz, chalcedony, and Fe calcite spar (intermediate stage); and dissolution, Ca-Fe dolomite and kaolinite (late stage). The R _m value of vitrinite shows a regional average of 0.6–0.7%; Rock-Eval T _maX suggests a comparable degree of organic maturity. The T _h of aqueous fluid inclusions in late stage Ca-Fe-Mg carbonates ranges from 90 to 160° and T _mice indicates very saline water (>200000 ppm NaCl equivalent); ¹⁸O suggests that the water is of basinal origin. Local warm spots have higher R _m, T _max, and T _h. The results constrain numerical models of regional fluid migration, which is widely viewed as an artesian flow from recharge areas in the Ouachita belt across the foreland basin onto the foreland shelf area. Such models must account for heating effects that extend at least 500 km from the orogenic front and affect both supposed aquifer beds and the overlying supposed confining layer. Warm spots indicate either more rapid or more prolonged flow locally. T _h and T _mice data show the highest temperatures coincided with high salinity fluids.     

威远震旦系天然气与油气生运聚

根据威远震旦系气藏天然气组成、同位素特征、储层包裹体的对比研究 ,我们认为该气藏的天然气主要来源于下寒武统筇竹寺组泥岩 ,其天然气主要是干酪根裂解气 ,次为油的裂解气。威远震旦系气藏是喜山期形成的 ,威远的天然气无论是干酪根裂解气还是油裂解气都由北面古构造聚集的干酪根裂解气和油裂解气转移而来 ,威远构造之所以能形成工业聚集的重要原因就是威远构造的形成与北面古构造的消失的良好匹配关系     

Analysis of chemical composition of precipitation in a typical background site

ＡｎａｌｙｓｉｓｏｆｃｈｅｍｉｃａｌｃｏｍｐｏｓｉｔｉｏｎｏｆｐｒｅｃｉｐｉｔａｔｉｏｎｉｎａｔｙｐｉｃａｌｂａｃｋｇｒｏｕｎｄｓｉｔｅＬｉｕＪｉａｑｉ，ＳｈｉＬｉｌｉＹｕｎｎａｎＰｒｏｖｉｎｃｉａｌＥｎｖｉｒｏｎｍｅｎｔａｌＭｏｎｉｔｏｒｉｎｇ...     

不同放牧强度对红三叶、黑麦草草地植被和土壤养分的影响

对不同放牧强度下草地植物和土壤的变化规律进行了研究，结果表明：３年强度放牧使土壤的全氮含量和草地的组成和结构发生了较大的变化，使牧草产量下降１７．１％，草地主要种红三叶的重要值降低了３３．８％，均质度系数增加５１．１％，土壤的氮磷比升高１．３。轻度放牧使草地全氮含量降低０．０９６％，红三叶的均质度系数增加２１．０％。中度放牧并未使草地牧草产量和红三叶的重要值降低，同时使草地红三叶均质度系数保持在远低于１．０水平以下，但使土壤全氮含量下降０．０８５％。根据以上结果，中度放牧是保持草地持续高产的最好的放牧管理选择。     

Effects of salinity on activities of H+-ATPase, H+-PPase and membrane lipid composition in plasma membrane and tonoplast vesicles isolated from soybean (Glycine max L.) seedlings

The effects of NaCI stress on the H^＋-ATPase, H^＋-PPase activity and lipid composition of plasma membrane(PM) and tonoplast(TP) vesicles isolated from roots and leaves of two soybean cultivars( Glycine max L. ) differing in salt tolerance(Wenfeng^7,salt-tolerant; Union, salt-sensitive) were investigated. When Wenfeng^7 was treated with 0.3% (W/V) NaCI for 3 d, the H^＋ -ATP aseactivities in PM and TP from roots and leaves exhibited a reduction and an enhancement, respectively. The H^＋ -PPase activity in TP from roots also increased. Similar effects were not observed in roots of Union. In addition, the increases of phospholipid content and ratios of phospholipid to galactolipid in PM and TP from roots and leaves of Wenfeng^7 may also change membrane permeability and hence affect salt tolerance.     

辽宁省外来入侵种组成及控制体系

在实地调查和收集相关文献资料的基础上，初步确定了辽宁省外来入侵种组成，并简要评价了辽宁省外来入侵种控制体系现状。     

珠江三角洲城市生活垃圾处理方法的探讨

对目前常用的城市生活垃圾处理方法的优缺点进行对比分析，并针对珠江三角洲地区城市生活垃圾的产生量和垃圾成分的变化以及其他影响因素，提出了适合该地区的城市生活垃圾处理方式。     

北京城区可吸入颗粒物(PM10)的矿物学研究

使用X射线衍射技术(XRD)和扫描电镜技术(SEM/EDX)对北京PM10中的矿物组分进行了分析.结果表明,北京PM10中的矿物组分存在明显的季节变化规律,春季PM10中的矿物组成种类最多;秋季PM10中的矿物种类最少;在夏季PM10中,矿物的种类有所减少,却有新的物种出现,如NH4Cl、K(NH4)Ca(SO4)2?H2O、As2O3?SO3等.粘土矿物是北京PM10中含量最高的矿物,石英的含量次之,其他依次为方解石、石膏、长石、白云石以及其他矿物颗粒;北京PM10中还存在一定数量的复合颗粒,颗粒表面常有S、Cl元素的存在.     

沙尘暴PM2.5水溶和有机成分对巨噬细胞的损伤

用超纯水或二氯甲烷从甘肃省武威市和内蒙古包头市采集的沙尘暴细颗粒物(PM2.5)中提取水溶成分和有机成分,于体外处理大鼠肺泡巨噬细胞4h,测定细胞谷胱甘肽(GSH)和丙二醛(MDA)含量、质膜ATP酶活性、膜表层和膜脂疏水区流动性、胞质内游离钙离子(Ca2+)浓度以及细胞培养液中乳酸脱氢酶(LDH)和酸性磷酸酶(ACP)活性.结果表明,沙尘暴PM2.5水溶成分可抑制质膜Ca2+-Mg2+-ATP酶、Na+-K+-ATP酶活性,降低质膜表层和膜脂疏水区流动性,增加胞质LDH外渗,并使细胞脂质过氧化作用增强、抗氧化能力减弱,但对ACP和Ca2+浓度影响不大;有机成分除引起胞质LDH渗漏、质膜Na+-K+-ATP酶活性下降外,对其它测定指标的影响无统计学意义.说明沙尘暴PM2.5水溶和有机成分均可对肺泡巨噬细胞产生毒性,其中水溶成分的毒性作用大于有机成分.