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沟壁侧面蒸发与黄土高原环境旱化关系初探 被引量:8
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作者 郑纪勇 李裕元 +1 位作者 邵明安 王全九 《中国水土保持科学》 CSCD 2006年第3期6-10,共5页
为定量研究沟壁侧面蒸发对加速黄土高原环境旱化的作用,在侵蚀强烈的水蚀风蚀交错带选择典型冲沟,分别在沟岸地(邻近沟缘的沟间地部分)距冲沟沟缘20、100、200、300、400、500、600cm处布设中子管,研究沟岸地土壤水分的垂直分布及... 为定量研究沟壁侧面蒸发对加速黄土高原环境旱化的作用,在侵蚀强烈的水蚀风蚀交错带选择典型冲沟,分别在沟岸地(邻近沟缘的沟间地部分)距冲沟沟缘20、100、200、300、400、500、600cm处布设中子管,研究沟岸地土壤水分的垂直分布及其动态变化。结果表明:土壤水分在距沟缘500cm范围内随距离增加而增加,证明了沟壁侧面蒸发作用的客观存在;对距沟缘不同距离0~300cm土层土壤储水量动态变化的研究表明:降雨发生时,不同距离各点的储水增量并无显著差异,但距沟缘20cm处土壤水分损失最快,而500cm土壤水分损失最慢,证明了沟壁侧面蒸发通过加速土壤水分蒸发加速黄土高原环境旱化的客观事实。沟岸地土壤储水量与距沟缘距离幂函数关系的确定为定量化研究沟壁侧面蒸发加速黄土高原环境旱化程度奠定了初步基础。 展开更多
关键词 黄土高原 土壤水分 环境旱化 沟壁 土壤蒸发
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河北省环境旱化的人为因素分析
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作者 梁彦庆 黄志英 伊立芬 《石家庄经济学院学报》 2003年第6期745-748,共4页
通过描述环境旱化在地表水、地下水、水质及旱灾等方面的影响 ,分析作物需水特性和环境旱化的关系 ,论述了人为因素在环境旱化过程中的作用 ,并从发展经济、保证水资源持续利用的角度提出了减少环境旱化影响的措施和对策。
关键词 河北 环境旱化 原因 人为因素 人口增加 经济发展 水质污染 水土流失 对策
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河北省环境旱化的气候分析
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作者 黄志英 梁彦庆 冯忠江 《干旱区研究》 CSCD 2003年第4期326-329,共4页
河北省历史上有“十年九旱”之称 ,干旱对农业生产影响很大。其气候原因一是降水少且时空分布不均 ;二是气温偏高 ,蒸发剧烈。利用承德围场站 195 1- 1999年降水量、平均气温和蒸发量的实测资料 ,对年降水量随时间变化进行分析 ,得到年... 河北省历史上有“十年九旱”之称 ,干旱对农业生产影响很大。其气候原因一是降水少且时空分布不均 ;二是气温偏高 ,蒸发剧烈。利用承德围场站 195 1- 1999年降水量、平均气温和蒸发量的实测资料 ,对年降水量随时间变化进行分析 ,得到年际演变规律。在此基础上进一步分析了降水、气温和蒸发量异常的时空变化特征与河北省环境旱化之间的关系。在初步分析全省环境旱化成因后 ,提出若干治理干旱的对策措施———建立健全干旱监测预警措施、加快水利建设、充分利用空间水资源、推广旱作节水农业技术、开展高效特色农业开发。 展开更多
关键词 河北 环境旱化 气候分析 时空变特征 降水 气温 蒸发量 治理 监测预警措施 水利建设 作农业
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Thermodynamic Effects on Particle Movement:Wind Tunnel Simulation Results 被引量:2
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作者 NIU Qinghe QU Jianjun +1 位作者 ZHANG Kecun LIU Xianwan 《Chinese Geographical Science》 SCIE CSCD 2012年第2期178-187,共10页
Sand/dust storms are some of the main hazards in arid and semi-arid zones. These storms also influence global environmental changes. By field observations, empirical statistics, and numerical simulations, pioneer rese... Sand/dust storms are some of the main hazards in arid and semi-arid zones. These storms also influence global environmental changes. By field observations, empirical statistics, and numerical simulations, pioneer researchers on these natural events have concluded the existence of a positive relationship between thermodynamic effects and sand/dust storms. Thermodynamic effects induce an unsteady stratified atmosphere to influence the process of these storms. However, studies on the relationship of thermodynamic effects with particles (i.e., sand and dust) are limited. In this article, wind tunnel with heating was used to simulate the quantitative relationship between thermodynamic effects and particle movement on different surfaces. Compared with the cold state, the threshold wind velocity of particles is found to be significantly decrease under the hot state. The largest decrease percentage exceedes 9% on fine and coarse sand surfaces. The wind velocity also has a three-power function in the sand transport rate under the hot state with increased sand transport. Thermodynamic effects are stronger on loose surfaces and fine particles, but weaker on compacted surfaces and coarse particles. 展开更多
关键词 thermodynamic effect threshold wind velocity nel simulation drifting sand flux structure sand transport rate wind tunnel simulation
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Structure of weathered clastic crust and its petroleum potential 被引量:7
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作者 ZOU CaiNeng HOU LianHua +4 位作者 YANG Fan YANG Chun TAO ShiZhen YUAN XuanJun ZHU RuKai 《Science China Earth Sciences》 SCIE EI CAS 2014年第12期3015-3026,共12页
Weathered clastic crust can be subdivided into weathered clay and leached zone in terms of variable weathering of different minerals and mobility of weathered products.On the basis of clastic outcrops and well cores i... Weathered clastic crust can be subdivided into weathered clay and leached zone in terms of variable weathering of different minerals and mobility of weathered products.On the basis of clastic outcrops and well cores in the Junggar Basin,the dark red Fe-rich weathered clay is formed in an arid environment,whereas the light blue Al-rich weathered clay under humid conditions.According to the geochemical analysis,a new weathering index for weathered clastic crust is built mainly on Fe and Al contents,accurately indicating the weathered clay,sandy leached zone,and muddy leached zone in the Junggar Basin.The breaking pressure of weathered clay is rather large,the same as that of normal muddy cap,effectively to seal oil or gas.The porosity of underlying leached zone is greatly enhanced by weathering and leaching,but its permeability is a function of clay mineral content,i.e.,the higher the clay content,the worse the permeability.Weathered crust provides effective sealing conditions for both top and bottom layers of a petroleum reservoir,and is important in the clastic hydrocarbon exploration. 展开更多
关键词 structure of weathered crust weathering index Junggar Basin reservoir properties hydrocarbon exploration
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Seasonal Variation of Cumulative CO_2 Emission from a Vertisol Under Apricot Orchard in Semi-Arid Southeast Turkey
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作者 G.YILMAZ 《Pedosphere》 SCIE CAS CSCD 2012年第3期322-332,共11页
Understanding the factors affecting the CO 2 emission from agricultural practices is crucial for global warming.A study was performed in an apricot orchard field in the experimental farm of the Harran University,South... Understanding the factors affecting the CO 2 emission from agricultural practices is crucial for global warming.A study was performed in an apricot orchard field in the experimental farm of the Harran University,Southeast Turkey,to i) quantify weekly and seasonal variations of the CO 2 emissions from a Vertisol under apricot orchard;ii) evaluate the difference in CO 2 emission between the area under trees and rows;and iii) assess the relationships between the amounts of CO 2 emissions and environmental parameters for better use and management of the soils from the view point of carbon balance and flux in a semi-arid environment under drip irrigation.Soil CO 2 emission measurements were performed during May 2008 and May 2010,from both under tree crowns (CO 2-UC) and between tree rows (CO 2-BR),on a weekly basis in southeast Turkey with a semi-arid climate.CO 2 emissions were statistically correlated with weather and soil parameters such as air temperature,relative humidity,rainfall,soil water content,and soil temperature at various depths from 5 to 100 cm.The weekly emissions ranged from 82 to 1 110 kg CO 2 ha 1 week 1 and from 96 to 782 kg CO 2 ha 1 week 1 in CO 2-UC and CO 2-BR,respectively.Increase in CO 2 emission in the second year was due to increases in mean air and soil temperatures.The weekly and monthly cumulative CO 2 emissions were positively correlated with the air and soil temperatures.Multiple linear regression analysis explained 35% and 83% variations in average weekly and monthly CO 2 emissions,by using meteorological data.Including the interaction effects of meteorological parameters in regression equations nearly doubled the variance explained by the regression models.According to stepwise regression analysis,soil and air temperatures were found to have the most significant impact on the temporal variability of the soil CO 2 emission. 展开更多
关键词 global warming meteorological data PLOWING soil temperature stepwise regression
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