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基于HYDRUS软件的植物混掺土壤水分特征曲线分析 被引量:1

Analysis of soil water characteristic curve by mixed plants based on HYDRUS software
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摘要 为探求植物混掺对土壤持水性产生的影响,以甘肃景泰地区土壤为试验材料,设置1%玉米芯、1%玉米叶、3%玉米芯、3%玉米叶等不同比例、不同秸秆混掺物4种处理,采用离心机法测定土壤水分特性曲线,同时利用HYDRUS软件进行模拟计算。结果表明,在相同吸力下,相同混掺物处理,混掺比为3%的土壤体积含水率高于混掺比为1%的土壤;相同混掺比处理,混掺玉米叶的土壤体积含水率高于混掺玉米芯的土壤,且混掺处理后土壤体积含水率均高于纯土;不同土壤水分特征曲线的模型拟合分析表明,不同处理的最优拟合模型均为Van Genuchten模型。研究结果可为探索该地区植物混掺条件下土壤水盐运移规律提供一定参考。 In order to explore the effect by mixed plants to soil water holding capacity,we have taken the soil from Jingtai,Gansu for the experimental material,set up four treatments with different plants mixed proportion (such as 1%corn cobs,1%corn leaves,3%corn cobs and 3%corn leaves),and use the centrifuge method to measure the soil wa-ter characteristic curve .At the same time,utilize the HYDRUS software to simulate and calculate .The results shown that:Under the treatment with same suction and mixed proportion,the soil volumetric water content with mixed propor-tion of 3% was higher than 1% soil;Under the same mixed proportion theatment,the soil volumetric water content mixed corn leaves was higher than mixed corn cobs soil,also the soil volumetric water content with all plants mixed treat-ments were total higher than the pure soil as without any mixed .Though the different model fitting analysis for the soil water characteristic curves,have indicated that the Van Genuchten model was the best fitting model for the four treat-ments .This research results can be provided a certain reference for exploring the rule of soil water and salt movement un-der plants mixed condition in this region .
出处 《干旱地区农业研究》 CSCD 北大核心 2014年第5期168-173,共6页 Agricultural Research in the Arid Areas
基金 国家自然科学基金项目(51369014) 旱区农业水土工程教育部重点实验室访问学者基金 兰州理工大学博士基金(0906ZXC121)
关键词 混掺物 土壤水分特征曲线 模型 HYDRUS Plants addictive soil water characteristic curve model HYDRUS
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参考文献21

  • 1刘洪波,张江辉,虎胆.吐马尔白,白云岗.土壤水分特征曲线VG模型参数求解对比分析[J].新疆农业大学学报,2011,34(5):437-441. 被引量:16
  • 2来剑斌,王全九.土壤水分特征曲线模型比较分析[J].水土保持学报,2003,17(1):137-140. 被引量:66
  • 3Turcotte D L. Fractals and fragmentation [ J ]. J Geophysical Res, 1986,91 (B2) : 1921-1926.
  • 4Bartoli F, Philippy R, Doirisse M, et al. Silty and sandy soil structure and self-similarity:The fractal approach[J]. J Soil Sci, 1991,42:167- 185.
  • 5Tyler S W, Wheateraft S W. Application of fraetal mathematics to soil water retention estimation[J]. Soil Sci SOe Am J, 1989,53:987-996.
  • 6Qadir M, Ghafoor A, Murtaza G. Amelioration Strategies for Saline Soils[ J]. land Degradation and Development, 2000,11 : 501-521.
  • 7Konukcu F, GowinJ W, Rose D A. Dry dminage:a sustainable solu- tion to water logging and salinity problems in irrigation areas? [J] .A- gricultural water nmrmgement,2006,83(12) : 1-12.
  • 8刘致远.不同外界条件对土壤入渗性能影响研究[J].山西林业,2008(5):23-25. 被引量:5
  • 9王全九,汪志荣,张建丰,高岩.层状土入渗机制与数学模型[J].水利学报,1998,29(S1):77-80. 被引量:17
  • 10Kasteel R, Gamier P, Vachier P, et al. Dye tracer infiltration in the plough layer after straw incorporation[ J ]. GcxMerma, 2007, 137 (3/ 4) : 360-369.

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