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[1]PENG Yi,LI Yu-yuan,LI Zhong-wu,et al.Comparison Study on Soil Infiltration Characteristics in Red Soil Slope Ecosystems[J].Research of Soil and Water Conservation,2009,16(06):205-209.

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Comparison Study on Soil Infiltration Characteristics in Red Soil Slope Ecosystems

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 16 Number of periods: 2009 06 Page number: 205-209 Column: Public date: 2009-12-20

Title:: Comparison Study on Soil Infiltration Characteristics in Red Soil Slope Ecosystems

Author(s):: PENG Yi^1,2, LI Yu-yuan², LI Zhong-wu¹, YANG Xiao-cong^1,2, PAN Chun-xiang², XIE Xiao-li²; 1. College of Environmental Science and Engineering, Key Laboratory of Environmental Biology and Pollution Control, Hu’nan University, Ministry of Education, Changsha 410082, China;
2. Institute of Subtropical Agriculture, Chinese Academy of Science, Changsha 410125, China

Keywords:: soil infiltration; red soil; slope ecosystems; disc permeameter

CLC:: S152.7;S181

DOI:: -

Abstract:: Soil infiltration characteristics, process and their relationship with soil main physical and chemical properties were studied. Six typical slope ecosystems in subtropical red soil region were selected and disc permeameter method was used. The selected ecosystems comprised of cropland (including steep and gentle slope types), grassland, shrub, tea garden, mixed evergreen and deciduous broadleaf forest, oil-tea (Camellia oleifera), woodland. Results showed that the relationship between soil infiltration rate and time in each ecosystems could be fitted as Y=aX^-b (P<0.01). The stable infiltration rate (Is) in all ecosystems ranged from 0.024 to 0.080 mm/min, while Is was the highest in cropland and oil-tea woodland but the lowest in grassland and tea garden. Is was negatively correlated to soil bulk density, initial moisture, but positively correlated to soil porosity. Infiltration process was mainly affected by soil porosity and clay content. The range of soil mean available pore size (MAPS) and macro-capillary length (MCL) were 0.064~0.179 mm and 41.5~128.2 mm respectively. However, MAPS and MCL were non-significantly related to main soil physical and chemical properties.

References:: [1] 张永涛,杨吉华,夏江宝,等.石质山地不同条件的土壤入渗特性研究[J].水土保持学报,2002,16(4):123-126.
[2] 樊军,邵明安,王全九.田间测定土壤导水率的方法研究进展[J].中国水土保持科学,2006,4(2):114-119.
[3] Angulo-Jaramillo R,Vandervaere J P,Roulier S,et al. Field measurement of soil surface hydraulic properties by disc and ring infiltrometers:a review and recent developments[J]. Soil Tillage Research,2000,55:1-29.
[4] Cameira M R,Fernando R M,Pereira L S. Soil macropore dynamics affected by tilllage and irrigation for a silt loam alluvial soil in southern Portugal[J]. Soil Tillage Research,2003,70:131-140.
[5] 薛绪掌,张仁铎.用盘式入渗仪数据计算土壤导水参数[J].水利学报,2001,10:12-18.
[6] 高鹏,穆兴民.黄土丘陵区不同土地利用方式下土壤水分入渗的对比试验[J].中国水土保持科学,2005,3(4): 27-31.
[7] 许明祥,刘国彬,卜崇峰,等.圆盘入渗仪法测定不同利用方式土壤渗透性试验研究[J].农业工程学报,2002,18(4):54-58.
[8] 马晓刚,张兵,史东梅,等.丘陵区不同土地利用类型紫色土入渗特征研究[J].水土保持学报,2007,21(5):21-29.
[9] 杨光,丁国栋,常国梁,等.黄土高原不同退耕还林地森林植被改良土壤特性研究[J].水土保持研究,2006,13(3):204-210.
[10] 杨文治,邵明安.黄土高原土壤水分研究[M].北京:科学出版社,2000:31.

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