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OALib Journal期刊
ISSN: 2333-9721
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新疆铁干里克绿洲水文过程对土壤盐渍化的影响
DOI: 10.11821/xb200807005, PP. 714-724
Keywords: 绿洲,地下水埋深,土壤盐渍化,塔里木河
Abstract:
在对塔里木河下游绿洲地表灌溉水和地下水水质特征及土壤盐分实测分析的基础上,探讨了地表水、地下水过程及其对土壤盐渍化的影响。结果显示塔里木河下游绿洲灌区地表水矿化度与土壤表层0~50cm盐分含量呈显著正相关,与50~100cm土层含盐量相关性不显著;地下水埋深与土壤盐分含量密切相关,0~50cm表层土壤盐分含量随地下水埋深的增加而下降,其中0~20cm下降幅度最大。当地下水埋深较浅时,绿洲内土壤含盐量高,呈T型分布,盐分表聚性强,土壤盐分含量随土壤深度的增加呈下降趋势;当地下水埋深较深时,绿洲内土壤盐份呈菱形分布,中层土壤盐分高,且地下水矿化度和土壤盐分分布转折点均为6.0m。据此推断,6m是地下水盐分积聚和表层土壤盐分积累停止的临界地下水埋深。
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