The 4D microgravity method for waterflood surveillance: Part 3-4D absolute microgravity surveys at Prudhoe Bay, Alaska

被引:34
作者
Ferguson, John F. [1 ]
Klopping, F. J. [2 ]
Chen, Tianyou [3 ]
Seibert, John E. [4 ]
Hare, Jennifer L. [5 ]
Brady, Jerry L. [6 ]
机构
[1] Univ Texas Dallas, Richardson, TX 75083 USA
[2] Microg LaCoste, Lafayette, CO USA
[3] Fugro Airborne Surveys, Mississauga, ON, Canada
[4] Seibert & Associates LLC, Anchorage, AK USA
[5] Zonge Engn & Res Org Inc, Tucson, AZ USA
[6] BP Explorat Alaska Inc, Anchorage, AK USA
关键词
geophysical equipment; geophysical techniques; Global Positioning System; gravimeters; gravity; hydrocarbon reservoirs;
D O I
10.1190/1.2992510
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The 4D microgravity method is becoming a mature technology. A project to develop practical measurement and interpretation techniques was conducted at Prudhoe Bay, Alaska, from 1994 through 2002. Beginning in 2003 these techniques have been systematically applied to monitor a waterflood in the gas cap of the Prudhoe Bay reservoir. Approximately 300 stations in a 150 km(2) area are reoccupied in each survey year with sub-5 mu Gal precision absolute gravity and centimeter precision Global Positioning System (GPS) geodetic measurements. The 4D gravity measured over epochs 2005-2003, 2006-2003, and 2007-2003 has been successfully modeled to track the mass of water injected since late in 2002. A new and improved version of the A-10 field-portable absolute gravity meter was developed in conjunction with this project and has proven to be a key element in the success of the 4D methodology. The use of an absolute gravity meter in a field survey of this magnitude is unprecedented. There are substantial differences between a 4D absolute microgravity survey and a conventional gravity survey in terms of station occupation procedures, GPS techniques, and the 4D elevation correction. We estimate that the overall precision of the 4D gravity signal in each epoch is less than 10 mu Gal.
引用
收藏
页码:WA163 / WA171
页数:9
相关论文
共 18 条
[1]  
Braasch M., 1996, GLOBAL POSITIONING S, V14, P547
[2]  
BRADY JL, 1993, W REG M SPE, P645
[3]  
BRADY JL, 2008, RESULTS WORLDS 1 4D, V11, P824
[4]  
Chapin D.A., 1996, LEADING EDGE, V15, P361, DOI [10.1190/1.1437341, DOI 10.1190/1.1437341]
[5]   DEFORMATION OF EARTH BY SURFACE LOADS [J].
FARRELL, WE .
REVIEWS OF GEOPHYSICS AND SPACE PHYSICS, 1972, 10 (03) :761-&
[6]   The 4D microgravity method for waterflood surveillance II - Gravity measurements for the Prudhoe Bay reservoir, Alaska [J].
Ferguson, J. F. ;
Chen, T. ;
Brady, J. ;
Aiken, C. L. V. ;
Seibert, J. .
GEOPHYSICS, 2007, 72 (02) :I33-I43
[7]   The 4-D microgravity method for waterflood surveillance: A model study for the Prudhoe Bay reservoir, Alaska [J].
Hare, JL ;
Ferguson, JF ;
Aiken, CLV ;
Brady, JL .
GEOPHYSICS, 1999, 64 (01) :78-87
[8]  
Hofmann-Wellenhof B., 2001, Global Positioning System: Theory and Practice, V5th ed.
[9]  
KLOBUCHAR JA, 1996, GLOBAL POSITIONING S, V12, P485
[10]   Ellipsoid, geoid, gravity, geodesy, and geophysics [J].
Li, X ;
Götze, HJ .
GEOPHYSICS, 2001, 66 (06) :1660-1668