期刊论文

Wang, H.

中文

环境科学学报

0253-2468

2008

28

8

1571-1578

10.3321/j.issn:0253-2468.2008.08.012

中国科学院***项目（No2004109）； 国家自然科学基金资助项目（No50479065）； 中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室开放基金（No10501-168）~~；

本校为第一且通讯机构

采用室内人工降雨模拟试验的方法,研究了不同土壤前期含水量对塿土和砂黄土的坡面土壤硝态氮和磷素流失过程的影响.研究结果表明,淋失是土壤硝态氮流失的主要途径,仅在前期含水量高于20%时,才产生硝态氮大量径流流失;随着土壤前期含水量的提高,塿土溶解态磷(DP)流失量与泥沙浸提态磷(SEP)流失量的比值呈减少趋势,砂黄土中该比值却呈指数函数增大趋势;2种土壤坡面径流SEP流失量与产沙量呈线性关系;通过坡面物质流失量(NO_3~--N、SEP、DP和产沙量)与前期土壤含水量的二次多项式关系,获得了使黄土坡面物质流失量最小的最优前期含水量值,其中塿土为10.21%～11.37%,砂黄土为8.97%～13.39%.

Antecedent moisture content is one of the important factors affecting runoff, as well as sediment and nutrient losses from slope-land. In this work, the effects of the antecedent moisture contents of the soil on the loss of Nitrate-N and phosphorus from the slope-land were investigated through indoor artificial rainfall experiments. The results show that NO3^- -N leaching plays a key role in the NO3^- -N loss of the soil, and the NO3^- -N in the soil transports into surface runoff when the antecedent soil moisture exceeds 20%. The ratio of diss...