Results 71 to 80 of about 5,242 (162)
Effects of different land use types on soil structure and hydraulic characteristics of reclaimed coal mines in semi-arid areas [PDF]
In order to explore the water characteristics of soil in reclaimed coal mines in semi-arid areas and make better use of the land in reclaimed mining areas, the basic physical properties, water characteristic curves, unsaturated water conductivity and ...
Duomei LI +5 more
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Remote sensing estimation on regional continuous daily evapotranspiration based on Richards equation [PDF]
Evapotranspiration (ET) is an important part of water cycle in nature, and the estimation of evapotranspiration on spatio-temporal scale has always been a hot issue. Remote sensing can estimate evapotranspiration on regional scale, but it is difficult to
Jinling KONG +4 more
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Shuitu Baochi Xuebao, 2008 通过对西南喀斯特不同石漠化过程中典型土壤水力特征的分析,研究了土壤水分参数与土壤水分库容特征及其影响因素。结果表明:(1)喀斯特地区土壤水分特征曲线呈先陡后缓的趋势,当土壤水吸力S潜在石漠化的普定灌丛黑色石灰土、玉米地棕色石灰土>轻度石漠化的荔波玉米地黄红壤,石漠化的发展减弱了土壤抗侵蚀能力。土层厚度、土壤有机质含量、土壤颗粒组成及0.3~0.03 mm孔隙度是影响土壤水分库容的主要因素。
李孝良, 陈效民, 周炼川, 方堃
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The Terraced Walls Significantly Influence the Spatial Distribution of Soil Water in Terraced Areas on the Loess Plateau [PDF]
[Objective] Converting slopes into terraces is a crucial soil and water conservation and agricultural measure on the Loess Plateau. Understanding the impact of terraced walls on soil water is conducive to preserving soil water and enhancing terrace ...
BAI Chenyun +5 more
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Shuitu Baochi Xuebao, 1995 土壤水分循环水平是指一定时期内土壤水分波动变化的平均状态。它是判别土壤水分循环状况优劣的标志之一，土壤水分循环达到平衡状态，并不一定说明土壤水分循环处于最佳状态。只有同时对土壤水平稀状态水分循水平进行，杂技和有可能作出可靠的判断，在一定程度上，生态系统的循环水平可以通过人为措施来调节。
王孟本
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Strategies of high efficiency water usage promoted by microbial remediation in coal mining areas of western China [PDF]
The fragile ecological environment in the western coal mining areas of China, compounded by intensive mining activities, has led to water and soil erosion, soil degradation, and damaged root systems.
Chao WU +4 more
core +1 more source
Shuitu Baochi Xuebao, 2008 通过对宁夏盐池沙地不同立地类型土壤水分连续两年的定位观测,探讨了固定沙丘不同部位、不同立地的沙柳林地和柠条林地的土壤水分特征和时空动态变化。结果表明:柠条林地的土壤容重最小,而保水能力最好。各样地土壤水分垂直分布总体表现出明显的分层特征,可划分为3层:土壤水分低值层、土壤水分活跃层、土壤水分相对稳定层,每一层的厚度因不同的立地类型而不同。
WNAG +7 more
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Synergistic Effects of No-tillage Combined with Mulching on Improving Soil Moisture Use and Potato Yield [PDF]
[Objective] Considering the severity of both spring drought and spring cold, and shallow effective topsoil in the southern mountainous areas of Ningxia Province, synergistic effects of no tillage combined with mulching on improving soil moisture use and ...
DUAN Ruibing +5 more
core +1 more source
Response of Soil Respiration to Snowfall in a Kubuqi Salix Plantation Forest of During Freeze-thaw Period [PDF]
[Objective] To investigate the changes of soil respiration in desert ecosystems and its relationship with environmental factors during the spring freeze-thaw period in arid and semi-arid regions, and to provide data support for the carbon budget of sandy
LAN Xiaozhen +8 more
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Shuitu Baochi Xuebao, 2004 湘北红壤坡地土壤持水力强,有效水含量低(10％左右),含水量呈季节性变化(年变化可分为饱和、亏缺和补充3个时期);土壤结构性差,养分贫乏,原始生产力低,易产生降雨土壤侵蚀。湘北红壤坡地雨水自然资源化程度为降雨量的(46±2)％,农业利用中必须强化雨水资源化过程。坡地典型农业利用系统(旱季)地表/大气界面的水分传输表现为:植被构成是影响传输通量的第一要素;气温和界面水势是影响土/气界面水分传输的主导环境气象因子;辐射和空气饱和水气压差是影响叶/气界面水分传输的主导环境气象因子;在一定的土壤含水量范围内,土/
谢小立 王凯荣
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