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生物炭不同粒径及不同添加量对土壤收缩特征的影响 被引量:44
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作者 文曼 郑纪勇 《水土保持研究》 CSCD 北大核心 2012年第1期46-50,55,共6页
土壤收缩特征在准确定量评价土壤结构和水力学特性中发挥重要作用。生物炭孔隙结构发达、比表面积巨大,施加生物炭不仅可以改变土壤的生物、化学性质,而且还影响到土壤的收缩特性。利用离心机法测定了添加不同粒径(2~1mm,1~0.25mm,<... 土壤收缩特征在准确定量评价土壤结构和水力学特性中发挥重要作用。生物炭孔隙结构发达、比表面积巨大,施加生物炭不仅可以改变土壤的生物、化学性质,而且还影响到土壤的收缩特性。利用离心机法测定了添加不同粒径(2~1mm,1~0.25mm,<0.25mm)、不同比例(0,10,50,100,150g/kg)生物炭的土壤收缩特征,并采用三直线模型进行了模拟,得出如下结果:相同压力下,土壤比容积随着生物炭含量增加而增大,生物炭有效地限制了土壤收缩。土壤收缩变化过程适用三直线模型描述,伪饱和段和结构段的收缩特征值随生物炭含量增加而减小,超正常段的土壤特征值随生物炭含量增加而增大;生物炭粒径对土壤收缩特征值变化的影响不显著。研究表明,向土壤中添加生物炭能有效降低土壤干燥过程中的收缩程度,改善土壤结构,提高土壤持水性能。 展开更多
关键词 生物炭 土壤收缩特征 三直线模型
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关于土壤收缩特征曲线的探讨 被引量:10
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作者 杨绍锷 黄元仿 《土壤通报》 CAS CSCD 北大核心 2007年第4期749-752,共4页
简单介绍了土壤收缩特征曲线的基本理论,着重阐述了Groenevelt和Grant提出的收缩特征曲线模型,并对该模型提出改进的思想,以便为土壤胀缩特性的研究提供参考。
关键词 土壤收缩特征曲线 Groenevelt-Grant模型
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土壤胀缩特征研究进展
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作者 郑旭超 周明涛 +3 位作者 李鸿铭 邵艳艳 李天齐 洪志鹏 《价值工程》 2018年第30期174-175,共2页
土壤胀缩现象是指土壤在干燥、湿润交替变化过程中所表现出的土壤容积随含水量改变的一种现象。本文就土壤容重测定方法、土壤容积变化表示方法和常用土壤收缩特征曲线模型等方面进行了总结和归纳,为干湿循环条件下土壤的胀缩特征研究... 土壤胀缩现象是指土壤在干燥、湿润交替变化过程中所表现出的土壤容积随含水量改变的一种现象。本文就土壤容重测定方法、土壤容积变化表示方法和常用土壤收缩特征曲线模型等方面进行了总结和归纳,为干湿循环条件下土壤的胀缩特征研究提供参考。 展开更多
关键词 土壤收缩特征 土壤容重 土壤容积
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土壤干湿收缩特征研究进展 被引量:24
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作者 吕殿青 邵明安 《土壤通报》 CAS CSCD 北大核心 2003年第3期225-228,共4页
土壤收缩特征是土壤在干燥、湿润交替变化过程中所表现出的土壤容积随含水量改变的关系。本文就土壤容积变化表示方法、土壤收缩特征曲线模型、膨胀土水分运动等方面进行总结和归纳,以便为优先流运动和土壤胀缩运动提供重要的参考价值。
关键词 土壤收缩特征 土壤容积 比容积 含水量
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Shrinkage Characteristics of Lime Concretion Black Soil as Affected by Biochar Amendment 被引量:4
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作者 WEI Cuilan GAO Weida +1 位作者 William Richard WHALLEY LI Baoguo 《Pedosphere》 SCIE CAS CSCD 2018年第5期713-725,共13页
Studies have reported that biochar is a sustainable amendment that improves the chemical and physical properties of soil.In this study,an incubation experiment was conducted to investigate the effects of different app... Studies have reported that biochar is a sustainable amendment that improves the chemical and physical properties of soil.In this study,an incubation experiment was conducted to investigate the effects of different application rates of biochar on the cracking pattern and shrinkage characteristics of lime concretion black soil after three wetting and drying cycles.Biochar derived from the corn straw and peanut shell mixture was applied to the soil at rates of 0,50,100,and 150 g kg^(-1)dry weight,representing the treatments T_(0),T_(50),T_(100),and T_(150),respectively.During the wetting and drying cycles,the cracking pattern and shrinkage characteristics of the unamended and amended soil samples were recorded.Application of biochar significantly increased soil organic carbon content in the samples.During soil desiccation,biochar significantly reduced the rate of water loss.Cracks propagated slowly and stopped due to the relatively higher water content in the soil applied with biochar.The cracking area density(ρ_c),equivalent width,fractal dimension,and cracking connectivity index decreased during the drying process with increasing application rate of biochar.Theρ_(c )value of the T_(50),T_(100),and T_(150) treatments decreased by 33.6%,52.1%,and 56.9%,respectively,after three wetting and drying cycles,whereas the T_(0) treatment exhibited a marginal change.The coefficient of linear extensibility,an index used to describe onedimentional shrinkage,of the unamended soil sample(T_(0))was approximately 0.23.Application of 100 and 150 g kg^(-1)biochar to the soil significantly reduced the shrinkage capacity by 41.45%and 45.54%,respectively.The slope of the shrinkage characteristics curve,which indicates the ralationship between soil void ratio and moisture ratio,decreased with increase in the application rate of biochar.Furthermore,compared with the T_(0) treatment,the proportional shrinkage zone of the shrinkage characteristic curve of the T_(50),T_(100),and T_(150) treatments decreased by 5.8%,13.1%,and 12.1%,respectively.Differences were not observed in the moisture ratio at the maximum curvature of the shrinkage characteristic curve among the treatments.The results indicate that biochar can alter the cracking pattern and shrinkage characteristics of lime concretion black soil.However,the effects of biochar on the shrinkage of lime concretion black soil are dependent on the number of wetting and drying cycles. 展开更多
关键词 coefficient of linear extensibility soil cracking pattern soil moisture ratio soil shrinkage characteristic curve SOILSTRUCTURE soil void ratio wetting and drying cycles
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