资源研究方法

模拟降雨条件下料浆石对土壤水分入渗的影响

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  • 1. 西北农林科技大学 资源环境学院,陕西,杨凌 712100;
    2. 黄土高原土壤侵蚀与旱地农业国家重点试验室, 西北农林科技大学 水土保持研究所, 陕西 杨凌 712100;
    3. 生态系统网络观测与模拟重点实验室, 中国科学院 地理科学与资源研究所, 北京 100101
周蓓蓓(1982- ),女,江苏徐州人,博士后,主要研究方向为土壤物理学。E-mail: happyangle222@yahoo.com.cn

收稿日期: 2009-10-16

  修回日期: 2011-01-15

  网络出版日期: 2011-06-20

基金资助

教育部创新团队(IRT0749); 黄土高原土壤侵蚀与旱地农业国家重点试验室(10501-259)。

Study on the Effect of Calcium Nodule on Soil Water Infiltration by Artificial Rainfall

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  • 1. College of Resources and Envirnmental Sciences, Northwest Sci-Tech University of Agriculture and Forestry, Yangling 712100, China;
    2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest Sci-Tech University of Agriculture and Forestry, Yangling 712100, China;
    3. Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China

Received date: 2009-10-16

  Revised date: 2011-01-15

  Online published: 2011-06-20

摘要

论文基于田间坡地人工模拟降雨实验,分析了料浆石覆盖及嵌入对入渗过程的影响,对比了其入渗速率及拟合参数的变化趋势。其结果表明,随料浆石覆盖度及料浆石嵌入含量的增加,入渗补给系数逐渐减小,且后者对其影响显著;料浆石嵌入小区的平均入渗速率及稳定入渗速率随料浆石含量的增加而缓慢减小。Kostiakov入渗经验公式和Philip方程均可以对降雨入渗过程进行描述。

本文引用格式

周蓓蓓, 姜艳丽, 邵明安, 温明霞 . 模拟降雨条件下料浆石对土壤水分入渗的影响[J]. 自然资源学报, 2011 , 26(6) : 1075 -1082 . DOI: 10.11849/zrzyxb.2011.06.018

Abstract

Based on the artificial rainfall experiment on the slope land, the effects of calcium nodule content (embedded in soil) and coverage on infiltration process were studied, as well as the infiltration rate and fitting parameters. The results showed that both of the calcium nodule content and coverage had obvious effects on recharge coefficient, while the effect of the former was much more obvious. The average infiltration rate and the stable infiltration rate decreased with the increase of calcium nodule content. Both of Kostiakov infiltration model and Philip equation could describe the rainfall infiltration process well.

参考文献

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