土壤中钼的形态分析方法研究

本文对土壤中有效钼的浸取条件进行最佳化，并利用提高灰化温度达到消除浸取剂对石墨炉原子吸收测定钼的影响，方法用于国标样品和武汉市区土壤样品中钼的形态分析，获得满意的分析结果。     

陆架浅海沉积物-海水界面溶质通量的计算方法及其应用

陆架浅海沉积物—海水界面上的溶解态生源物质通量的准确估算是海洋生态系统动力学研究中的关键性问题之一。由于底栖生物活动以及海流、海浪及潮波与海底地形地物相互作用的影响 ,使得该通量的准确估算十分困难。本文综合分析讨论了近年来提出的各种计算该类通量的物理模型及参数的确定方法 ,并结合在中国黄、东海等陆架浅海水层—底栖生态动力学耦合模型研究的需要 ,比较深入地讨论了应用过程中应该考虑的几个问题     

矿区复合生态系统中土壤演替和植被演替的相互影响

在讨论矿区复合生态系统涵义的基础上，以平朔安太堡露天煤矿为例，探讨了大型露天矿区复合生态系统演替与原生态系统演替的不同，即露天矿区复合生态系统演替极大地受着社会--经济--自然三方面的控制，在演替过程中土壤演替与植被演替相互影响、相互协调，共同作用了矿区复合生态系统。同时，还阐述了进行矿区生态重建的两大关键措施：生态环境建设和群落建设。     

Relation between some variations of soil and surface vegetatio and desertization in agriculture-pasture interlacing zone an example from Kangbao County,North Hebei,China

The studied agriculture-pasture interlacing zone has its specific natural conditions,at which the natural systems are unstable ,their self-regulation capability is low and the equilibrium is easily broken, and hence the habitat is fairly vulnerable.During last 20 years the increasing population and livestock ,over-reclamation,over-pasturing,over-deforesting, and other intensified negative human activities in the zone resulted in coarsening of surface soil,decrease of organic mater content in soil, reduction of vegetation coverage ,variation and degradation of flora structure, and hence in desertization of the land, although average of gales and sandstorms some decreased and the climate tended to be better in the region.However, the frequent sandstorms occurring in the springs of last and present years has attracted much attention.Investigations confirmed that the main cause for the phenomena is the unreasonable human activites rater than the natural factors.     

沈阳张士污灌区土壤重金属元素形态分析

选取沈阳张士污灌区土攘样品,采用欧共体标准局的三步提取法研究土壤中5种重金属元素的形态分布.研究结果表明,在该污灌区土壤中,Cd和zn主要以B1(水溶态、可交换态与碳酸盐结合态)和B2(铁-锰氧化物结合态)为主,分别占总量的49.4%、26.4%和43.9%、44.3%.Cu、Pb主要以B2(铁-锰氧化物结合态)和B3(有机物与硫化物结合态)为主分别占总量的43.4%、66.6%和29.1%、25.3%.Cr以B3(有机物与硫化物结合态)和残渣态为主,分别占总量的40.4%和42.5%.元素总量和形态分析的结果表明该地区土壤污染为单一的镉污染土壤,且镉的可迁移性强,易被植物吸收.     

雷州半岛胀缩土地裂缝及其成因机理

本文简述了雷州半岛胀缩土地裂缝的特征及分布发育规律；分析了胀缩土地裂缝的成因。认为雷州半岛胀缩土地裂缝的形成发育是胀缩土以及气候、植被、地形地貌、水文地质作用等因素综合作用的结果。其中胀缩土含大量的亲水矿物和失水产生向心收缩的特性从而成为地裂缝成生发展的内因。而特定的气候、植被、地形地貌、水文地质作用等外部环境条件则是导致胀缩土失水和发展形成地裂缝的重要外因。桉树是一种吸水-蒸腾能力极强的树种，树根的干燥作用是导致了林区土体干燥-收缩和形成收缩应力场及在林地边缘产生地下暗裂缝的关键因子，而极端的干旱气候环境和久旱后第一场大暴雨则是暗裂牵动式胀缩土地裂缝发育形成不可或缺的因素。胀缩土地裂缝灾害应重在预防，有关的策略包括防水保湿、科学植树、建筑设计和地基处理、科学选址。     

云南土壤钴元素背景值及其特征研究

对云南省土壤钴元素背景值进行了采样分析,结果显示:云南土壤钴元素含量呈对数正态分布,中位值16.0mg/kg,几何均值14.88mg/kg,95%置信区间0.92~41.17mg/kg,背景值高于全国,接近南方部分地区。并对其特征进行了研究。     

CrⅥ adsorption on four typical soil colloids: equilibrium and kinetics

It is observed that the adsorption of chromium are greater on kaolinite minerals, red soil (R) and laterite (L) colloids than that on montmorillonite, indicotic black (IB) and yellow brown (YB) soil colloids. The adsorption process of CrⅥ on these media can be further described by Langmuir or Freundlich equation quite well. The adsorption reaction of CrⅥ is fast, and the adsorption equilibrium can be reached within the first two hours in moderate temperature. The adsorption quantity of CrⅥ to kaolinite mineral increased with the increasing pH in the range of 2.0 to 7.0, then decreased at higher pH. But it showed some consistence among the four soil colloids. The lower the pH, the stronger the adsorption. The possible mechanisms are further discussed here. Meanwhile the influence of temperature on CrⅥ adsorption on different soil colloid and clay minerals are also investigated.     

滕南煤田煤矸石对土壤的影响分析

通过对山东滕南煤田地区的土壤、煤矸石及部分农作物的灰份进行化学分析，从理论上探讨了其促进植物增产的机理；并认为该煤田3煤层的矸石含有与该地区土壤类似的化学组成，但其所含植物生长需要的主要元素普遍高于土壤中的含量，即煤矸石中含有较丰富的植物生长所需的矿物肥料。     

复杂粘性土层深基坑挡土桩受力分析

针对目前桩锚式支护计算方法的局限性，对复杂土层中下端固定的锚定式挡土桩作了受力分析，并编写了计算机程序，适用于处理深基坑支护中的分层土(砂土、粘性土)、有超载、存在地下水等各种复杂土层。