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洛惠渠灌区水土化学特性分析
引用本文:于国强,李占斌,张霞,李鹏,王双平.洛惠渠灌区水土化学特性分析[J].水土保持通报,2009,29(1):103-107.
作者姓名:于国强  李占斌  张霞  李鹏  王双平
作者单位:于国强,李占斌,李鹏,YU Guo-qiang,LI Zhan-bin,LI Peng(西安理工大学西北水资源与环境生态教育部重点实验室,陕西西安,710048);张霞,ZHANG Xia(陕西省环境科学研究设计院,陕西西安,710061);王双平,WANG Shuang-ping(黄委会天水水土保持科学试验站,甘肃,天水741000)  
基金项目:国家科技支撑项目,国家自然科学基金,中日合作项目 
摘    要:为了深入了解洛惠渠灌区土壤盐碱化程度,分别测试了2004年实地采集的63个土壤样品和71个地下水样品,测定项目分别为土壤含盐量、碱化度、阴阳离子含量和地下水化学成分,并分析了该灌区土壤盐碱化现状以及地下水水质状况.结果表明,洛惠渠灌区土壤盐碱化较明显,盐渍化土壤分成盐土和碱土两类,主体成分为钠(钾)、钙的硫酸盐和碳酸盐;而地下水化学类型基本属于氯化钠-硫化钠型.通过计算其钠吸附比和镁系数可以推知该灌区地下水大部分对灌溉作物有不利影响,并且对土壤有进一步碱化的威胁.因此,有效控制该灌区地下水位是治理土壤盐碱化的重要措施,还要考虑不同区域土壤易溶盐含量,作物耐盐碱性等因素.应当综合工程、生物、化学等方法来改良利用盐碱土地,方能起到事半功倍的治理效果.

关 键 词:土壤  盐化  碱化  地下水  化学类型
收稿时间:2008/3/27 0:00:00
修稿时间:2008/9/11 0:00:00

Water and Soil Chemical Characteristics in the Luohui Trench Irrigation District
YU Guo-qiang,LI Zhan-bin,ZHANG Xi,LI Peng and WANG Shuang-ping.Water and Soil Chemical Characteristics in the Luohui Trench Irrigation District[J].Bulletin of Soil and Water Conservation,2009,29(1):103-107.
Authors:YU Guo-qiang  LI Zhan-bin  ZHANG Xi  LI Peng and WANG Shuang-ping
Institution:Key Laboratory of Northwest Water Resources and Environmental Ecology of the MOE, University of Technology, Xi'an, Shaanxi 710048, China;Key Laboratory of Northwest Water Resources and Environmental Ecology of the MOE, University of Technology, Xi'an, Shaanxi 710048, China;Research and Design Institute of Environmental Science of Shaanxi Province, Xi'an, Shaanxi 710061, China;Key Laboratory of Northwest Water Resources and Environmental Ecology of the MOE, University of Technology, Xi'an, Shaanxi 710048, China;Tianshui Experimental Station of Soil and Water Conservation, the Water Conservancy Committee of the Yellow River, Tianshui, Gansu 741000, China
Abstract:In order to understand the extent of soil salinization in the Luohui Trench Irrigation District,63 soil samples and 71 groundwater samples were collected in situ in 2004.Soil salt content,degree of alkalization,anion and cation content,and chemical composition of groundwater were measured respectively.The present situation of soil salinization and the status of groundwater quality were analyzed.Results show that soil salinization in the irrigation district is considerably serious.Saline soils may be classified as the two categories of saline soil and alkali soil.The main salinity composition is consisted of sulfate of sodium(potassium),calcium,and carbonate.The chemical characteristic of groundwater is in the category of sodium chloride-sodium sulfide,basically.It can be inferred that most of groundwater in the irrigation district has an adverse effect on irrigated crops according to its sodium adsorption ratio and magnesium coefficient calculated and has a threat of further alkalization to soil.Hence,an effective control of soil salinization is an important measure to control groundwater table in the irrigation district.Such factors as the concentrations of soluble salts of different districts and the salt-alkali tolerance of crops should be taken into account as well.It is suggested that the measures of engineering,biology,and chemistry should be combined to get twice the achievement with half the effort.
Keywords:soil  salinization  alkalization  groundwater  chemical type
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