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METHOD FOR DETERMINING LITHOLOGIC COMPOSITION OF FROZEN ROCKS

机译:冻岩岩性成分测定方法

摘要

FIELD: mining.;SUBSTANCE: at the profile points the current is supplied through a pair of feeding electrodes to the earth. Current value and potential difference between pair of receiving electrodes is measured. Feeding electrodes are moved with pitch equal to 1 m symmetrically relative to the centre to limit distance between feeding electrodes, which is determined by the specified investigation depth. As per measurement results the apparent specific resistance is calculated. As per data of apparent specific resistance the graph of its behaviour is built depending on half-spacings of feeding electrodes. Specific resistances of frozen beds are calculated as per apparent specific resistance graph. Percentage of clay in unit volume of rock is calculated as per data of specific resistances of frozen beds by the following formula: where ρclay - specific clay resistance, which in permafrost zone section is characterised as constant value which on average is equal to 100 ohm m, ρfb -specific resistance of frozen bed. Lithologic composition of sand-clay complex of frozen rocks is determined as per clay content.;EFFECT: reducing the cost of operations and improving informativity owing to determining lithologic composition of frozen rocks without any drilling data and using common data on geologic structure of investigation region.;1 tbl, 2 dwg
机译:领域:采矿;实体:在轮廓点处,电流通过一对馈电电极供应到地面。测量一对接收电极之间的电流值和电位差。进给电极相对于中心对称地以等于1 m的间距移动,以限制进给电极之间的距离,该距离由指定的检查深度确定。根据测量结果,计算表观电阻率。根据表观电阻率的数据,其行为图取决于馈电电极的半间距。根据表观电阻率曲线计算冷冻床的电阻率。根据以下公式,根据冷冻床的比电阻数据计算粘土在岩石单位体积中的百分比:其中ρ clay -特定粘土电阻,在多年冻土区段中被表征为恒定值,平均等于100 ohm m,ρ fb -冷冻床的比电阻。冻结岩砂粘土复合物的岩性成分是根据粘土含量确定的;效果:由于无需任何钻探数据即可确定冻岩的岩性成分,并使用调查区域地质结构的通用数据,从而降低了运营成本并提高了信息化。; 1 tbl,2 dwg

著录项

  • 公开/公告号RU2420765C1

    专利类型

  • 公开/公告日2011-06-10

    原文格式PDF

  • 申请/专利权人 TEN KONSTANTIN MAKAROVICH;

    申请/专利号RU20090135146

  • 发明设计人 TEN KONSTANTIN MAKAROVICH;

    申请日2009-09-22

  • 分类号G01V3/02;

  • 国家 RU

  • 入库时间 2022-08-21 17:48:23

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