Assessment of elemental distribution and trace element contamination in surficial wetland sediments, Southern Tibetan Plateau

In order to analyze and evaluate different trace metals on surface water of the Changjiang River, concentrations of dissolved trace metals (Cu, Ni, Fe, Co, Sc, Al, Zn, Pb, Cd, Se, As, Cr, and Hg), major elements(Ca and Mg), and nutrient(NO $_{3}^{-})$ were measured. Samples were taken at 76 positions along Changjiang River in flood and dry seasons during 2007?C2008. Spatial distributions identified two main large zones mainly influenced by mineral erosion (sites 1?C22) and anthropogenic action (sites 23?C76), respectively. Principal component analysis (PCA) and hierarchical cluster analysis were used to identify the variance distinguishing the origin of water. Four significant components were extracted by PCA, explaining 74.91% of total variable. Cu, Ni, Fe, Co, Sc, Al, Ca, and Mg were mainly associated with the weathering and erosion of various rocks and minerals, while an anthropogenic source was identified for Cd and As. Although erosion was one source of Pb and Zn, they were also input by atmospheric deposition and industrial pollutions. NO $_{3}^{-}$ and Se were mainly associated with agriculture activities. However, Hg and Cr showed different sources. CA confirmed and completed the results obtained by PCA, classifying the data into two large groups representing different areas. Group 1 referred to the upper reaches which represented samples mainly corresponding to natural background areas. Group 2 referred to the middle and lower reaches including samples under anthropogenic influence. Meanwhile, group 2 was subdivided into three new groups, representing agricultural, industrial, and various artificial pollution sources, respectively.     

Characteristics of CO2 release from forest soil in the mountains near Beijing

CO₂ release from forest soil is a key driver of carbon cycling between the soil and atmosphere ecosystem. The rate of CO₂ released from soil was measured in three forest stands (in the mountainous region near Beijing, China) by the alkaline absorption method from 2004 to 2006. The rate of CO₂ released did not differ among the three stands. The CO₂ release rate ranged from ??341 to 1,193 mg m^???2 h^???1, and the mean value over all three forests and sampling times was 286 mg m^???2 h^???1. CO₂ release was positively correlated with soil water content and the soil temperature. Diurnally, CO₂ release was higher in the day than at night. Seasonally, CO₂ release was highest in early autumn and lowest in winter; in winter, negative values of CO₂ release suggested that CO₂ was absorbed by soil.     

Changes in the area of inland lakes in arid regions of central Asia during the past 30 years

Inland lakes are major surface water resource in arid regions of Central Asia. The area changes in these lakes have been proved to be the results of regional climate changes and recent human activities. This study aimed at investigating the area variations of the nine major lakes in Central Asia over the last 30 years. Firstly, multi-temporal Landsat imagery in 1975, 1990, 1999, and 2007 were used to delineate lake extents automatically based on Normalized Difference Water Index (NDWI) threshold segmentation, then lake area variations were detailed in three decades and the mechanism of these changes was analyzed with meteorological data and hydrological data. The results indicated that the total surface areas of these nine lakes had decreased from 91,402.06 km² to 46,049.23 km² during 1975?C2007, accounting for 49.62% of their original area of 1975. Tail-end lakes in flat areas had shrunk dramatically as they were induced by both climate changes and human impacts, while alpine lakes remained relatively stable due to the small precipitation variations. With different water usage of river outlets, the variations of open lakes were more flexible than those of other two types. According to comprehensive analyses, different types of inland lakes presented different trends of area changes under the background of global warming effects in Central Asia, which showed that the increased human activities had broken the balance of water cycles in this region.     

乌鲁木齐市蔬菜基地土壤有效态镉的空间变异特征

以乌鲁木齐市北郊蔬菜基地为典型区,对干旱区绿洲城市郊区土壤有效态镉含量的结构特征进行分析,得出该区有效态镉的空间分布格局,并揭示了引起这种分布格局的成因和污染来源.结果表明,乌鲁木齐市北郊蔬菜基地有效态镉属中等变异.半方差函数模型拟合表明,有效态镉含量可以用指数函数拟合,且在一定范围内存在空间相关性.采用Kriging...     

参窝水库水体自净能力及水质变化规律研究

根据参窝水库近几年的水质监测资料，对参窝水库的水体自净能力及水质变化规律进行了较深入的研究、计算出主要污染物在参窝水库的自净率，分析了参窝水库水质变化规律，为参窝水库的水污染防治提供了科学的依据。     

WTO:中国环境立法挑战与整合

探讨了我国“入世”后环境立法所面对的挑战问题。分析了世贸组织法中的环保条款及中国环境立法不完善之处，指出这将对中国“入世”后对外贸易产生不利影响。对完善中国环境立法提出建议。     

Status of mercury pollution during resources development in Guizhou Province, China

1　ＩｎｔｒｏｄｕｃｔｉｏｎＧｕｉｚｈｏｕＰｒｏｖｉｎｃｅｉｓｌｏｃａｔｅｄｉｎｓｏｕｔｈｗｅｓｔＣｈｉｎａｗｉｔｈａｔｏｔａｌａｒｅａｏｆ 176.2 8ｔｈｏｕｓａｎｄｓｑｕａｒｅｋｉｌｏｍｅｔｅｒｓ,ｏｆｗｈｉｃｈ 87%ｉｓｍｏｕｎｔａｉｎ ,10 %ｉｓｈｉｌｌｓ,3%ｉｓｒｉｖｅｒ,ｂａｓｉｎａｎｄｐｌａｉｎ .Ｇｕｉｚｈｏｕｉｓａｍｏｕｎｔａｉｎｏｕｓｐｒｏｖｉｎｃｅｗｉｔｈｒｉｃｈｍｉｎｅｒａｌｒｅｓｏｕｒｃｅｓ,ａｍｏｎｇｗｈｉｃｈｍｅｒｃｕｒｙｒｅｓｅｒｖｅｒａｎｋｓｆｉｒｓｔｉｎＣｈｉｎａ,ｅｖｅｎｉ…     

柴达木盆地水资源承载力研究

提出了以期望人口为核心的水资源承载力指标体系,并应用于柴达木盆地水资源承载力的实际研究． 用柴达木盆地水资源承载力系统动力学仿真模型（ＳＤＳＭＷＲＳＣＣＢ）计算了人口等承载力指标的预测值,把期望值和预测值进行了深入分析比较,推断出柴达木盆地水资源承载力．     

热重法研究煤燃烧添加剂的催化效果

采用热量分析法研究了江西丰城劣质煤燃烧特性和稀土助燃添加剂对该煤的催化燃烧作用效果，比较了劣质煤在加入稀土助燃添加剂前后燃烧峰值温度、燃烧反应活化能、反应级数的变化。结果表明，在劣质煤中加入５％的稀土助燃添加剂后，能显著加快煤燃烧速率，降低燃烧反应活化能，从而产生助燃效果，进一步分析了稀土助燃添加剂的催化作用机理。     

泸沽湖特有水生生物的保护初探

泸沽湖有水生生物 133种。本文对其种群结构、数量作了调查 ,分析了特有种水生生物结构变化原因是不合理利用 ,应通过管理措施和工程措施保护特有水生生物