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对广州市秀全、巴江、江村、石门、西村、刘屋洲、南洲和沙湾等主要生活饮用水地表水源地中钼、钴、铍、硼、锑、镍、钒、钛、锡、银和钡等微量元素含量水平进行了调查,并采用单因子污染指数法和内梅罗综合污染指数法对微量元素水质进行了评价。结果表明,硼和锡在所有地表水源地均未检出,铍在部分地表水源地有检出,其他检测项目在所有地表水源地均有检出。整体而言,微量元素含量水平不高,地表水源地由北往南微量元素内梅罗指数呈逐渐降低态势,南部水源地水质优于北部水源地。巴江和西部水源地镍含量相对较高,电镀企业排污监管力度有待进一步加强。 相似文献
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Effect of lime application on microbial community in acidic tea orchard soils
in comparison with those in wasteland and forest soils 总被引:1,自引:0,他引:1
Lime application is a conventional technology to control acidification in tea orchard soils. We investigated the e ect of lime
application on soil microbial community diversity in the soils of three tea orchards, wasteland and forest. The BIOLOG data showed
that both the average well color development of all carbon sources and the functional diversity index increased with the liming rate in
the tea orchards and the forest, but decreased in the wasteland. The phospholipid fatty acid (PLFA) analysis showed that the structural
diversity index of soil microbial community increased with the liming rate in all the tea orchards, the wasteland and the forest. Lime
application also increased the soil-bacterial PLFA content in all the soils. Soil fungal and actinomycete PLFAs in the tea orchards
showed an increasing trend from 0 to 3.2 g CaCO3/kg application and then a decreasing trend from 3.2 to 6.4 g CaCO3/kg application.
The principal component analysis of BIOLOG and PLFA data suggested that lime application had a significant e ect on soil microbial
community structure, and land use had a greater e ect on soil microbial community structure compared to lime application. 相似文献
609.
Zongming Wang Kaishan Song Bai Zhang Dianwei Liu Chunying Ren Ling Luo Ting Yang Ni Huang Liangjun Hu Haijun Yang Zhiming Liu 《Agriculture, ecosystems & environment》2009,129(1-3):315-324
In the past century, especially the past five decades, the grasslands of the West Songnen Plain, Northeast China, were rapidly converted into croplands and salinized wasteland, and experienced a fragmentation process that is still ongoing. Almost no information is available on the spatial-temporal changes of grasslands in this area. In this study, grassland cover change, agricultural reclamation and salinized wasteland expansion were investigated during the past five decades. Grassland fragmentation was studied based on four landscape metrics. The grassland cover change was detected from a time series of topographic maps from 1954, satellite images of Landsat TM in 1986, 1995, and 2000 using remote sensing and geographic information systems (GIS). In addition, the land use changes were analyzed using a transition matrix of land use types, while the driving forces were explored according to climatic changes and socioeconomic developments. The results indicated a significant decrease in grassland area. Of the 1 418 945 ha of native grassland in 1954, approximately 64% was removed by 2000, while the number of patches (NP) increased from 865 to 2035 and the mean patch size (MPS) decreased from 1640 ha to 252 ha. During the whole study period, the average annual decrease rate of grassland was 34 894 ha/year. Cropland and salinized wasteland were the two main land use types into which grassland converted. During the past decades, obvious climatic changes occurred, which supplied a favorable potential environment for agricultural development but damaged grassland productivity. On the other hand, population, GDP and livestock number increased significantly as grassland quality decreased. According to the results, the shrinkage and fragmentation of grasslands may well be explained by socioeconomic development and aided by changing climatic conditions. 相似文献
610.
Xinye Wang Yaji Huang Miaomiao Niu Yongxing Wang Changqi Liu 《Journal of Material Cycles and Waste Management》2016,18(2):287-295
The thermodynamic equilibrium of trace lead during the waste incineration was calculated on the basis of the minimization of the total Gibbs energy. The effect of incineration condition and MSW components on Pb distribution was investigated mainly in the view of the interaction of related elements. In the oxygen-rich condition, incineration temperature affects Pb distribution by the interaction of Cl, Ca and Na. In the fuel-rich condition, incineration temperature affects Pb distribution directly by the thermal transition of PbS(s) to PbCl(g) and the thermal transition of PbCl(g) to Pb(g). Air ratio has significant effect on Pb distribution by the interaction of H, O and Cl. The liberated Cl in oxidizing condition is far less than that in reducing condition. Na has the top priority to bond with Cl, than Ca only at low temperature and H only at high temperature, so the effect of Cl on Pb distribution depends on the content of Na and Ca. S promotes Pb volatilization by the interaction with Na in oxygen-rich and chlorine-poor condition and depresses Pb volatilization by the formation of PbS(s) directly without interaction with other elements in fuel-rich condition. 相似文献