侧面蒸发条件下黄土高原北部沟岸地土壤水分及养分分布特征
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摘要
为确定单侧和双侧沟壁侧面蒸发条件下沟岸地土壤水分养分分布特征,选取典型沟岸地测定距沟壁不同距离处的土壤水分养分数据进行分析,结果表明:1)侧面蒸发条件下,沟岸地土壤水分含量随着距沟壁距离的增加有上升趋势,双侧面蒸发导致土壤水分含量在东西两侧分别低于单侧面蒸发9.9%和15%。2)侧面蒸发条件下土壤有机质含量平均低于对照组89.20%(0-20 cm)和16.71%(20-100 cm),双面蒸发条件下土壤有机质含量则呈西高东低的趋势。3)单侧面蒸发条件下土壤速效磷含量与对照组差异不大,在双侧面蒸发条件下土壤速效磷含量明显高于对照,且呈中间高,靠近沟壁处低的规律。4)侧面蒸发对土壤速效钾含量的影响不明显。该研究旨在为该区植被恢复和农业生产提供理论依据,为进一步研究黄土高原水分养分特征提供研究基础。
引文
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