Results 1 to 10 of about 312 (99)
Comparison of Infiltration Capacity Between Grassland of Different Time Lengths of Abandonment and Sea Buckthorn Land in Inner Mongolia [PDF]
[Objective] The effect of different vegetation covers on soil infiltration capacity in Inner Mongolia was analyzed in order to provide a theoretical basis for ecological restoration and vegetation allocation of the region.
Cheng Shuai +5 more
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Influence Mechanism of Ionic Interface Reaction on Soil Porosity [PDF]
[Objective] The changes in surface charge properties of soil particles and the net force between particles were analyzed, in order to elucidate the influence mechanism of particle interaction on pore conditions.
Ding Wuquan +3 more
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A Study on Pore Structure and Erosion Resistance of Soil Column Based on CT Scanning Technology [PDF]
[Objective] The relationship between soil column pore structure and soil erosion resistance for soil columns with Bahiagrass was analyzed in order to provide a scientific basis for the optimal arrangement of plants for soil and water conservation and to ...
Cao Longxi +4 more
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Effects of Different Plant Spacings on Preferential Flow Development Characteristics of Vetiver Plant Slopes [PDF]
[Objective] The development characteristics of preferential flow for a vetiver slope and the relationship between vetiver roots and preferential flow were analyzed in order to provide a theoretical basis for further study on the influence of plant roots ...
Jiang Xueliang +4 more
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采用X-ray computed tomography(CT)技术研究了果树行间不同油菜间作密度(CK:清耕;L:低密度间作;M:中密度间作;H:高密度间作)对土壤大孔隙特征参数的影响。结果表明:油菜间作改善了果树行间(0—60 cm)土壤大孔隙特征,各土层的土壤大孔隙数量、大孔隙面积、大孔隙度等参数分别较清耕显著提高(P 1 mm)在各土层间的数目多、差异小,并且在0—30 cm土壤剖面上的成圆率最高。中、高密度油菜间作的土壤大孔隙特征参数均优于清耕及低密度间作,而中密度间作的土壤大孔隙分布更均匀 ...
何娜娜 +4 more
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根据水分穿透曲线和Poiseuille方程,定量研究桂东南花岗岩区6种(次生林、柑橘园、玉米地、杉木林、撂荒地和桉树林)不同土地利用方式土壤大孔隙半径范围、数量及分布情况,分析不同土地利用方式对土壤大孔隙特征的影响。结果表明:(1)不同土地利用方式土壤水分穿透速率存在差异,土壤水分出流速率短时间内可达到稳定状态,柑橘园不同土层之间稳定出流速率变化较大;(2)不同土地利用方式的土壤大孔隙半径为0.4~2.4 mm,主要集中分布在0.4~1.2 mm,均值为0.85 mm,
黄娟 +5 more
doaj
以明确自然界中广泛存在的层状结构土壤孔隙分布特征为目的。选黄土高原典型坝地土壤剖面为研究对象,利用CT扫描技术分析耕作层、犁底层、心土层土壤三维结构,探讨层状土孔隙参数随土层结构变化及界面层孔隙特征。结果表明:(1)瘦长型孔隙(孔隙形状系数≤0.2)是各土层土壤孔隙的主要形态。各土层的孔隙参数具有明显差异。耕作层的总孔隙度最高,大孔隙(≥1 mm)分布较多;犁底层孔隙总数量最高,含有较多孤立的小孔隙(≥0.1~0.5 mm)和微小孔隙(≥0.06~0.1 mm),但连通性最差 ...
张佐源 +5 more
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为探究大气氮沉降增加导致的土壤团聚体结构变化规律及其对土壤水分入渗性能的影响,在贡嘎山针叶成熟林和中龄林内分别设计2种氮肥形态[(NH4)2SO4、KNO3]和4个浓度水平(0,10,20,40 kg/(hm2·a)N)的添加试验,研究不同形态大气氮沉降对亚高山森林土壤团聚体结构和土壤水分入渗特征的影响。结果表明:(1)随施氮量增加,中龄林土壤大团聚体含量逐渐增加,土壤持水量、孔隙度和水分稳定入渗率逐渐增大;成熟林土壤大团聚体含量、土壤持水量、孔隙度和水分稳定入渗率均表现出先增加后降低的趋势;(2 ...
郭海云, 王根绪, 孙守琴
doaj
在岩溶作用下,喀斯特土壤—表层岩溶带耦合发育,上覆土壤中大孔隙与下伏表层岩溶带中裂隙、管道存在密切的水力联系,然而土壤大孔隙影响土壤—表层岩溶带系统中水土漏失的过程机理尚不清楚。通过人工模拟降雨试验,采用试验微区模拟不同土壤大孔隙形态(出露型、浅埋型、深埋型),并以全土微区为对照,探讨了土壤大孔隙对喀斯特地区水土漏失过程的影响。结果表明:与全土微区相比,土壤大孔隙的存在明显加速了水分的垂直渗漏,其对水分渗漏量的影响表现在峰值不同(出露型 > 浅埋型 > 深埋型 > 全土 ...
周春衡 +4 more
doaj
采集了太湖地区3种主要水稻土(白土、黄泥土和乌栅土)的原状土柱为供试土样,利用CT扫描技术,在不破坏土体结构的前提下,准确地得出了不同深度土壤剖面上各种大孔隙的数量、面积以及分布状况。结果表明,3种水稻土均以表层的大孔隙度最大,在30~40cm处达到一个最低点,再往下又呈波浪形变化。土柱各截面上大孔隙面积的变异系数随着深度的变化与大孔隙度相似,大孔隙度大的层次其变异系数也较大。等效直径越大的孔隙(〉5mm)在土壤不同深度下数量的变化也越大。表层上大直径(〉5mm)的大孔隙较多,在土壤剖面30 ...
吴华山, 陈效民, 陈粲
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