欢迎访问林业科学,今天是

林业科学 ›› 2011, Vol. 47 ›› Issue (1): 29-35.doi: 10.11707/j.1001-7488. 20110105

• 论文 • 上一篇    下一篇

黄土丘陵区燕沟流域农林草地土壤水库充失水过程模拟

王力1,2, 卫三平1,3, 王全九1   

  1. 1. 西北农林科技大学黄土高原土壤侵蚀与旱地农业国家重点实验室 杨凌 712100;2. 中国科学院水利部水土保持研究所 杨凌 712100;3. 山西省吕梁市水利局 离石 033000
  • 收稿日期:2009-08-12 修回日期:2010-11-06 出版日期:2011-01-25 发布日期:2011-01-25

Simulation of Soil Moisture Dynamics under Farmland, Woodland and Grassland in Yangou Small Watershed of the Hill-Gully Region of the Loess Plateau

Wang Li1,2, Wei Sanping1,3, Wang Quanjiu1   

  1. 1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau,Northwest A & F University Yangling 712100;2. Institute of Soil and Water Conservation, CAS & MWR Yangling 712100;3. Bureau of Water Conservancy in Lüliang City, Shanxi Province Lishi 033000
  • Received:2009-08-12 Revised:2010-11-06 Online:2011-01-25 Published:2011-01-25

摘要:

基于野外实测资料,用土壤-植被-大气传输模型(SVAT-model)——CoupModel对陕北黄土丘陵区燕沟流域农地、刺槐林地、荒草地2006年6月—2007年5月间土壤水库充失水过程进行模拟。结果表明:农地、刺槐林地和荒草地0~600 cm土层平均蓄水量随土壤基质吸力增大而减小,土壤水库库容曲线均呈幂函数关系; 试验期间,农地、刺槐林地和荒草地的总充水量分别为437,361和429 mm,分别占同期降水量463 mm的94.3%,77.9%和92.6%; 农地土壤水库的充满程度达72.8%~79.3%,荒草地为41.4%~47.5%,刺槐林地仅为37.1%~41.2%; 农地、刺槐林地和荒草地的总失水量分别为421,393和468 mm; 研究期属于干旱年份,农地土壤水库的失水量比充水量少15 mm,土壤水库中的水分略有剩余; 刺槐林地和荒草地土壤水库的失水量分别比充水量多32 mm和39 mm,说明刺槐林和荒草会过多地消耗土壤水库中的水分,水分平衡出现负补偿现象。研究不同植被覆盖条件下土壤水库充失水特征,可为黄土丘陵区农田管理、退耕还林等生态环境建设提供科学依据。

关键词: CoupModel, 土壤水库, 土壤水分, 模拟, 黄土丘陵区

Abstract:

The CoupModel is a one-dimensional soil-vegetation-atmosphere transfer model (SVAT). It was applied to simulate and study the processes of soil moisture loss and gain in potato farmland, acacia woodland, and grassland occurring in the hill-gully region of the Loess Plateau of China. The objective of the study was to develop theoretical guidance for farmland management and restoration of sloping farmland to woodland using measured and simulated soil moisture dynamics in three different vegetation regimes. Simulations followed the expected pattern in which water storage within the soil reservoir decreased with increasing soil matric suction and soil-water reservoir capacities were all characterized by power functions. The farmland, acacia woodland, and grassland soils respectively received a water input of 437, 361 and 429 mm water accounting for 94.3%, 77.9% and 92.6% of total precipitation (463 mm) in the experimental period from June 2006 to May 2007. Water storage within the soil profile of 600 cm layers ranged between 72.8%-79.3%, 37.1%-41.2% and 41.4%-47.5% of the field capacity, respectively, in the farmland, acacia woodland and grassland. The total water loss from the soil reservoir over the simulation-year was 421, 393 and 468 mm, respectively. Overall, there was a net annual water gain of 15.3 mm in the farmland while there was a net annual water loss of 32 and 39 mm respectively from the acacia woodland and grassland. It was suggested that there was excess water for farmland to consume, while a water deficit occurred in the acacia woodland and grassland. Therefore, more attention should be paid on the assessment of sustainability of vegetation restoration with woodland and grassland species for improving soil water management and soil reservoir restoration.

Key words: CoupModel, soil reservoir, soil water, simulation, hill-gully region of the Loess Plateau of China

中图分类号: