east <mrow><msubsup><mi>U</mi><mi>i</mi><mi>e</mi></msubsup></mrow> and vertically <mrow><msubsup><mi>U</mi><mi>i</mi><mi>v</mi></msubsup></mrow> (i=1, 2,…, Ngeod) are determined. For the same time interval the displacements Nsat of steadily reflecting grounds in direction of a satellite <mrow><msubsup><mi>U</mi><mi>j</mi><mrow><mi>L</mi><mi>O</mi><mi>S</mi></mrow></msubsup></mrow> (j=1, 2,…, Nsat) are determined with the help of radar satellite interferometry. Afterwards the explored field is divided into K elementary volumes. The following is calculated: the displacements in the point of the j steadily reflecting ground in the direction of a satellite <mrow><msubsup><mi>V</mi><mrow><mi>j</mi><mo>,</mo><mi>k</mi></mrow><mrow><mi>L</mi><mi>O</mi><mi>S</mi></mrow></msubsup></mrow> which are resulting from the increase of pressure on a unit in the k elementary volume, and displacements in the point of i geodetic benchmark respectively to the north, east and vertically <mrow><msubsup><mi>V</mi><mrow><mi>i</mi><mo>,</mo><mi>k</mi></mrow><mi>n</mi></msubsup><mo>,</mo></mrow> <mrow><msubsup><mi>V</mi><mrow><mi>i</mi><mo>,</mo><mi>k</mi></mrow><mi>e</mi></msubsup><mo>,</mo></mrow> <mrow><msubsup><mi>V</mi><mrow><mi>i</mi><mo>,</mo><mi>k</mi></mrow><mi>v</mi></msubsup><mo>,</mo></mrow> which are resulting from the increase of pressure on a unit in the k elementary volume. Pressure difference ΔPk is defined in each volume. Afterwards three components of earth surface displacement vector are determined.;EFFECT: higher accuracy of determination of earth surface displacement.;4 dwg"/> METHOD TO DEFINE THREE COMPONENTS OF EARTH SURFACE DISPLACEMENT VECTOR AT OIL AND GAS FIELD EXPLORATION
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METHOD TO DEFINE THREE COMPONENTS OF EARTH SURFACE DISPLACEMENT VECTOR AT OIL AND GAS FIELD EXPLORATION

机译:确定油气田勘探中地表位移矢量的三种成分的方法

摘要

FIELD: instrumentation.;SUBSTANCE: invention relates to surveying and geodetic monitoring and can be used to ensure safety of oil and gas field exploration. As per the proposed method the geodetic measurements are carried out in the examined area and displacements Ngeod of geodetic becnhmarks to the north <mrow><msubsup><mi>U</mi><mi>i</mi><mi>n</mi></msubsup><mo>,</mo></mrow> east <mrow><msubsup><mi>U</mi><mi>i</mi><mi>e</mi></msubsup></mrow> and vertically <mrow><msubsup><mi>U</mi><mi>i</mi><mi>v</mi></msubsup></mrow> (i=1, 2,…, Ngeod) are determined. For the same time interval the displacements Nsat of steadily reflecting grounds in direction of a satellite <mrow><msubsup><mi>U</mi><mi>j</mi><mrow><mi>L</mi><mi>O</mi><mi>S</mi></mrow></msubsup></mrow> (j=1, 2,…, Nsat) are determined with the help of radar satellite interferometry. Afterwards the explored field is divided into K elementary volumes. The following is calculated: the displacements in the point of the j steadily reflecting ground in the direction of a satellite <mrow><msubsup><mi>V</mi><mrow><mi>j</mi><mo>,</mo><mi>k</mi></mrow><mrow><mi>L</mi><mi>O</mi><mi>S</mi></mrow></msubsup></mrow> which are resulting from the increase of pressure on a unit in the k elementary volume, and displacements in the point of i geodetic benchmark respectively to the north, east and vertically <mrow><msubsup><mi>V</mi><mrow><mi>i</mi><mo>,</mo><mi>k</mi></mrow><mi>n</mi></msubsup><mo>,</mo></mrow> <mrow><msubsup><mi>V</mi><mrow><mi>i</mi><mo>,</mo><mi>k</mi></mrow><mi>e</mi></msubsup><mo>,</mo></mrow> <mrow><msubsup><mi>V</mi><mrow><mi>i</mi><mo>,</mo><mi>k</mi></mrow><mi>v</mi></msubsup><mo>,</mo></mrow> which are resulting from the increase of pressure on a unit in the k elementary volume. Pressure difference ΔPk is defined in each volume. Afterwards three components of earth surface displacement vector are determined.;EFFECT: higher accuracy of determination of earth surface displacement.;4 dwg
机译:技术领域本发明涉及测量和大地监测,并且可以用于确保油气田勘探的安全性。根据所提出的方法,在检查区域进行大地测量,并向北 <![CDATA [ < mi> U i n ]]> <图像文件= “ 00000024.GIF” he =“ 6” imgContent =“ undefined” imgFormat =“ GIF” wi =“ 7” /> east <![CDATA [ U i e ]]> <图像文件=“ 00000025.GIF” he =“ 7” imgContent =“ undefined” imgFormat =“ GIF” wi =“ 5” /> 和垂直 <![CDATA [ U i v ]]> <图像文件=“ 00000026.GIF” he =“ 7” imgContent =“ undefined” imgFormat =“ GIF” wi =“ 7” /> 确定(i = 1,2,…,N geod )。对于相同的时间间隔,在卫星 <![CDATA [ U ]方向上稳定反射地面的位移N sat j L O S ]]> <图像文件=“ 00000027.GIF” he =“ 8” imgContent =“ undefined” imgFormat =“ GIF” wi =“ 9” /> (j = 1,2,…,N sat )是借助雷达卫星干涉测量法确定的。然后,将勘探领域划分为K个基本体积。计算得出以下内容:沿卫星方向稳定反射地面的j点的位移 <![CDATA [ V j k L O S ]]> <图像文件=“ 00000028.GIF” he =“ 8” imgContent =“ undefined” imgFormat =“ GIF” wi = “ 10” /> 这是由于单位基本单位k的压力增加,以及第i个大地测量基准点向北,向东和垂直方向的位移 <![CDATA [ V i k n ]]> <图像文件=“ 00000029.GIF” he =“ 6” imgContent =“ undefined” imgFormat =“ GIF” wi =“ 8” /> <![CDATA [ V i k e ]]> <图像文件=“ 00000030。 GIF“ he =” 6“ imgContent =” undefined“ imgFormat =” GIF“ wi =” 8“ /> <![CDATA [ V < / mi> i k v ]]> <图像文件=“ 00000031.GIF” he =“ 6” imgContent =“ undefined” imgFormat =“ GIF” wi =“ 8” /> 这是由于单位体积k的单位压力增加所致。在每个体积中定义压差ΔP k 。然后确定了地表位移矢量的三个分量。效果:确定地表位移的精度更高; 4 dwg

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