微波高压硝酸消化原子荧光法测定微量砷

采用微波消化测定煤和土壤中微量元素砷。用硝酸高压消解，然后用原子荧光仪测定。方法的检出限0.011ng／L，线性范围0～40ng／L，其回收率为90．95～104．25％。该方法简便了煤和土壤中砷的消化和测定，精密度高，检出限低。     

某滑坡滑带非饱和土强度特性试验研究

借助专门的能够控制吸力的四联式非饱和土直剪仪,对清江水布垭坝区古树包滑坡滑带土的重塑样进行了一系列抗剪强度试验,验证了F red lud提出的非饱和土抗剪强度公式对滑带土的适用性,求出了该滑带非饱和土的强度参数;通过在一定基质吸力条件下量测含水率-固结压力之间的关系,指出土-水特征曲线与固结压力相关的特性。     

莠去津在填充土柱中的运移

用土柱实验模拟莠去津在土壤中的运移、实验结果表明相当浓度的莠去津被淋溶到土柱的底部，说明莠去津对地下水存在很大威胁、应用CXTFIT的平衡与非平衡模型模拟莠去津在土柱中的运移，模拟结果表明CXTFIT的非平衡模型能很好地模拟莠去津的穿透曲线．由CXTFIT率定得到的莠去津在土柱实验中的吸附和降解参数和从批次实验得到的吸附和降解参数有较好的一致性．     

横泉水库已筑坝体强夯试验研究

以横泉水库坝体强夯试验为背景,结合加固过程中测得的试验数据,通过对比分析夯前夯后试样物理力学指标的变化,对碾压填土强夯的加固效果进行了分析,其结果可对类似工程的施工提供参考。     

稀土农用研究进展

在系统收集已有资料及课题研究的基础上,论述了国内外稀土农用的研究进展与意义,并对海南岛砖红壤中稀土农用研究的意义进行了探讨.     

强夯—塑料板排水法在粉土和粉质粘土地基加固中的试验研究

针对黄河中下游粉土、粉质粘土成层地基,通过插设塑料排水板和不插排水板条件下强夯对比试验研究,证实了插设塑料排水板可以有效的降低强夯时超静孔隙水压力峰值,加快其消散,缩短强夯施工工期;提高强夯夯沉,减少振动对土体的扰动,缩短触变恢复时间,因而人工塑料排水板在强夯处理此类地基中是十分有效的。     

攀枝花地区昔格达土中钒的含量及分布

对母质为昔格达组粘土的攀枝花土壤样品数据进行了分析研究。结果表明，该区土壤中的钒普遍具有一定的地带性分布规律及剖面分布特征。一般来说，矿区土壤中的钒含量明显高于非矿区，表明该区土壤主要受采矿污染的影响；水田土壤中钒含量明显高于旱地，表明水是钒元素迁移的重要介质（载体）。钒含量在土壤剖面上的空间分布呈底层富集型，反映了成土因素的综合影响。     

基于GIS的土壤信息系统

分析了GIS的功能和技术特点，研制了基于GIS的土壤信息系统。系统采用了Client／Server、Browse/Server相结合的开发模式，采用MapInfo来管理空间数据，SQL Server管理属性数据。系统实现了土壤肥力数据、土壤分类信息等的查询、检索、属性数据统计分析、专题图制作、输出及更新功能。系统的研制为提高农业生产中的科技含量，合理利用各种土壤信息提供了支持。     

^210Pbex depth distribution in soil and calibration models for assessment of soil erosion rates from ^210Pbex measurements

Throughout the past decade, the potential for using nuclear weapon-produced 137Cs ( half-life 30.2 a) fallout to quantify soil erosion rates on both cultivated and uncul- tivated lands for medium-term timescales (≈ 40 a) has been successfully demonstrated in a wide range of envi- ronments in different regions of the world[1—6]. Because in difficulties of distinguishing Chernobyl-derived compo- nent from total 137Cs input in many parts of Europe, and in measuring low activity samples of…     

Loess-soil sequences in southern Anhui Province： Magnetostratigraphy and paleoclimatic significance

Two parallel loess-soil sequences from Xuancheng and Fanchang in southern Anhui Provinces are dated using geomagnetic and luminescence methods.The Brunhes/Matuyama(B/M) reversal boundary is recognized within the lower part of the so-calles Vermiculated Red Soil (VRS) in the Xuancheng section while the entire Fanchang sequence is of Brunhes age.This indicated that the most recent VRS in southern China,a stratigraphic marker and an indication of extremely warm-humid conditions,was formed during the middle Pleistocene,chronologically correlative with the S4 and S5 soil units in northern China.Microscopic and sedimentologic in vestigations reveal that eolian deposition started in this region at about 0.85 MaBp,roughly synchronous with the well-known Mid-Pleistocene climate change of global significance.The strengthening of both summer and winter monsoon circulations and the consequent river hydrological changes at that time would have provided favorable conditions for sustained eolian deposition in the middle-lower reaches of the Yangtze River since 0.85 MaBP.