黄土高原坡地退耕恢复草地的土壤水分动态

doi:10.11733/j.issn.1007-0435.2015.06.008

草地学报 ›› 2015, Vol. 23 ›› Issue (6): 1182-1189.DOI: 10.11733/j.issn.1007-0435.2015.06.008

黄土高原坡地退耕恢复草地的土壤水分动态

易彩琼¹, 王胜², 樊军^1,2

1. 西北农林科技大学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, 陕西杨凌 712100;
2. 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, 陕西杨凌 712100

收稿日期:2014-05-16 修回日期:2014-07-28 出版日期:2015-12-15 发布日期:2016-02-01
通讯作者: 樊军
作者简介:易彩琼(1989-),女,湖北监利人,硕士研究生,主要从事土壤侵蚀研究,E-mail:xiaocai1989123@163.com
基金资助:
国家自然科学基金(41271239);中国科学院西部行动计划项目(KZCX2-XB3-13)资助

Soil Water Dynamics of Degraded Grassland on the Slope of the Loess Plateau

YI Cai-qiong¹, WANG Sheng², FAN Jun^1,2

1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi Province 712100, China;
2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences, Yangling, Shaanxi Province 712100, China

Received:2014-05-16 Revised:2014-07-28 Online:2015-12-15 Published:2016-02-01

摘要/Abstract

摘要：

为了解黄土高原水蚀风蚀区坡地退耕还草后的土壤水分消耗与补充过程,利用2003年开始的野外坡面径流小区定位观测土壤剖面水分,分析坡地退耕还草多年后的土壤水分动态变化及丰水年的恢复状况。结果表明:坡地退耕还草后,土壤水分含量降低,多年以后,苜蓿地显著低于坡耕地,含水量已接近或者达到萎蔫含水量。撂荒草地土壤水分含量稍低于坡耕地,尽管坡耕地有较多的径流,但是土壤水分含量保持在较高水平。2010年初3个处理土壤剖面平均含水量分别为7.4%,12.6%,12.5%,丰水年降水可以不同程度的补充土壤剖面水分,补充深度较一般年份深110 cm左右,苜蓿地、撂荒地、坡耕地土壤水分分别恢复到10.0%,14.5%,15.5%,分别增加了35.1%,15.1%,24.0%。因此,坡耕地退耕种植紫花苜蓿(Medicago sativa)导致土壤水分含量显著降低,只有在丰水年土壤水分含量才有较明显的恢复。

关键词: 黄土高原, 土壤水分, 退耕还草, 丰水年

Abstract:

In order to understand the soil water depletion and replenishment after returning farmland to grassland on the sloping in the water-wind erosion region of the Loess Plateau, soil moisture dynamics were observed under different land use types. Results show that the soil water content of the grassland (alfalfa) decreased distinctly and water content was close to the wilting point after alfalfa was planted for many years. Despite of having more runoff, the soil water content was in a higher level in the farmland. The average water contents of grassland, abandoned land and farmland were 7.4%, 12.6% and 12.5% at the beginning of the growing season in 2010, respectively. Soil water was recharged to different levels under different land use types in the wetter year, and the recharging depth in the wetter year was deeper than normal year. The soil water contents of alfalfa land, abandoned land and farm land were restored to 10.0%, 14.5%, 15.5%, and the soil moisture increased by 35.1%, 15.1%, 24.0%, respectively. As a result, the soil water content decreased significantly by returning farmland to grassland, and the distinct recovery of soil water content was observed only in the wetter year.

Key words: The Loess Plateau, Soil moisture, Returning farmland to grassland, The wetter year

中图分类号:

易彩琼, 王胜, 樊军. 黄土高原坡地退耕恢复草地的土壤水分动态[J]. 草地学报, 2015, 23(6): 1182-1189.

YI Cai-qiong, WANG Sheng, FAN Jun. Soil Water Dynamics of Degraded Grassland on the Slope of the Loess Plateau[J]. Acta Agrestia Sinica, 2015, 23(6): 1182-1189.

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黄土高原坡地退耕恢复草地的土壤水分动态

Soil Water Dynamics of Degraded Grassland on the Slope of the Loess Plateau

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