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煤岩瓦斯动力灾害主控地质体理论及地质作用机理 被引量:3
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作者 董国伟 胡千庭 《西安科技大学学报》 CAS 北大核心 2017年第1期7-14,共8页
为研究煤岩瓦斯动力灾害地质作用机理,初次提出了控制煤岩瓦斯动力灾害的"主控地质体"的概念,并进行了定义及分类,采用理论分析、实验室实验、现场实测及现场考察等手段进行了相关研究。研究认为:煤系地层区域沉积体系、地层... 为研究煤岩瓦斯动力灾害地质作用机理,初次提出了控制煤岩瓦斯动力灾害的"主控地质体"的概念,并进行了定义及分类,采用理论分析、实验室实验、现场实测及现场考察等手段进行了相关研究。研究认为:煤系地层区域沉积体系、地层层序位置决定着煤层厚度、顶底板岩性及粒度、煤层赋存状况等,越靠近海(湖)侵体系域最大海(湖)泛面位置,煤层瓦斯赋存量越大(顶底板石灰岩煤层除外)、煤层煤岩瓦斯动力灾害危险性越大,解释了煤层群中不同煤层煤岩瓦斯动力灾害程度差异;煤岩瓦斯动力灾害地质作用机理为地层沉积埋藏作用、地质构造作用、热作用、生烃作用等时空配置控制着煤层的改造程度、瓦斯的生成、保存及逸散程度,以及自重应力、构造应力的分布情况,进而控制煤岩瓦斯动力灾害区域分布及灾害程度;初步建立了主控地质体理论、分析方法及判识依据。研究成果在水城矿区进行了应用,验证了该方法的合理性和适用性。 展开更多
关键词 煤岩瓦斯动力灾害 发生机理 主控地质 地质作用机理 层序地层
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黔西地层热流体差异作用及其煤层气成藏效应
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作者 唐淑玲 汤达祯 +2 位作者 许浩 陶树 李松 《煤炭科学技术》 CAS 北大核心 2016年第2期8-16,共9页
为了研究煤层气系统热流体偶合地质作用机制,对织金、盘县煤系热流体地质特征进行了对比,并从地层热流体活动新的视角分析了黔西煤层气富集成藏地质选择过程。研究表明:织金、盘县均存在两期区域性热流体活动,早期以钙质流体为载体,晚... 为了研究煤层气系统热流体偶合地质作用机制,对织金、盘县煤系热流体地质特征进行了对比,并从地层热流体活动新的视角分析了黔西煤层气富集成藏地质选择过程。研究表明:织金、盘县均存在两期区域性热流体活动,早期以钙质流体为载体,晚期以硅质流体和少量钙质流体为载体,分别属于地层流体热循环作用和深源高温热流体的差异注入。热流体作用促使煤层气集中高强度生成和运移,产生密集成群管状气孔,与构造应力协同,导致煤体开裂破碎,明显影响煤的孔渗性。煤系地层中相对封闭滞留的热流体环境,是导致煤层气系统高压形成的重要因素之一。黔西北部台隆处于相对封闭滞留区,高温热流体配置条件更有利于煤层气富集成藏。 展开更多
关键词 热流体 地质作用机理 煤层气 富集成藏作用
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Analysis of soft rock mineral components and roadway failure mechanism 被引量:1
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作者 陈杰 《Journal of Coal Science & Engineering(China)》 2001年第2期87-90,共4页
The mineral components and microstructure of soft rock sampled from roadway floor in Xiagou pit are determined by X ray diffraction and scanning electron microscope. Combined with the test of expansion and water softe... The mineral components and microstructure of soft rock sampled from roadway floor in Xiagou pit are determined by X ray diffraction and scanning electron microscope. Combined with the test of expansion and water softening property of the soft rock, the roadway failure mechanism is analyzed, and the reasonable repair supporting principle of roadway is put forward. 展开更多
关键词 soft rock mineral components MICROSTRUCTURE failure mechanism
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Distribution,Properties,Land Use and Management of Mollisols in South America 被引量:4
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作者 Artigas Duran Hector Morris +1 位作者 Guillermo Studdert LIU Xiaobing 《Chinese Geographical Science》 SCIE CSCD 2011年第5期511-530,共20页
Mollisols are common in South America. They cover about 8.87 × 107ha, 1.3 × 107ha and 4.3 × 106ha in Argentina, Uruguay and Southern Brazil respectively, which is 11.5% of the world total. Most of South... Mollisols are common in South America. They cover about 8.87 × 107ha, 1.3 × 107ha and 4.3 × 106ha in Argentina, Uruguay and Southern Brazil respectively, which is 11.5% of the world total. Most of South American Mollisols were developed on Pleistocene and Holocene sediments and lie within the limits of the temperate zone, though the extreme north is bordering subtropical and the extreme south is within a cold-temperate zone. All suborders of Mollisols occur in Argentina, the most extensive being Udolls followed by Ustolls, whereas only Udolls, Aquolls and Albolls occur in Uruguay. Vertisols in Uruguay have many properties similar to Mollisols, and the occurrence of Vertisols is strongly associated with Mollisols. The Pampean Mollisols are a significant component of the global breadbasket of modem times. The main Argentine crops are wheat, corn, sorghum, barmy, soybeans and sunflower, while Mollisols in Uruguay remain mostly dedicated to cattle and sheep grazing though crop production has been increasing very rapidly in the last decade. Throughout South America, research has shown that Mollisols are experiencing losses of soil organic matter and nutrients, and degradation of physical properties after long cropping periods, resulting in soil scientists calling for increased conservation practices to reduce future losses and a deterioration of soil quality, and thus a more sustainable agriculture in the region. 展开更多
关键词 MOLLISOLS CLASSIFICATION SUSTAINABILITY soil fertility no tillage South America
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