Site selection assessment method for water-bearing stratum underground gas storage
A gas storage and water layer technology, which is applied in the field of natural gas resource exploration and development, can solve problems such as scientific and effective evaluation of the location of underground gas storages that cannot aquifer, and achieves a scientific, effective, scientific and reasonable technical method for site selection and evaluation. Effect
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Embodiment 1
[0122]Block D5 is geographically located in a township in central Hebei Province. The surface is a farmland area, involving several villages, 45km away from the natural gas pipeline network. This area is a weak earthquake area, and there have been no natural disasters such as earthquakes and floods in recent years. The structure is located in the Litan Sag on the east side of the Dacheng Uplift in a depression in North China. The reverse traction anticline structure controlled by the Dacheng East Fault develops along the downthrown wall of the Dacheng Fault. The top of the Ordovician and the top of the Carboniferous-Permian sandstone have clear anticline shapes, and the long axis strikes northeast.
[0123] The Permian trap area of D5 block is about 12km 2 , the closure range is 150m, and the buried depth of the top surface is 2285m, see Figure 5 . The quality of the 2D seismic data is good, the confirmation degree of the trap is 90%, the structure is relatively confirmed...
Embodiment 2
[0125] The Ordovician trap area in block D5 is about 4.1km 2 , the closure range is 50m, and the buried depth of the top surface is 3075m, see Figure 6 . The quality of 2D seismic data is average, and the degree of confirmation of traps is low. Whether effective traps are formed depends on the sealing performance of faults. The Ordovician target layer is mainly limestone and dolomite, with a total thickness of 198.6m, a porosity of 3.5-7.5%, and a permeability of 0.12-2.0mD; the daily water production of the test well is 33.7m 3 , accumulative water production 111m 3 . The Ordovician overlying the Carboniferous Benxi Formation-Taiyuan Formation (3047m-3085m) is dominated by mudstone and coal rock, with a thickness of 38m, which is a good caprock.
[0126] The above-mentioned relevant information and data were summarized, sorted and screened according to the index parameters required for site selection and evaluation of aquifer gas storage, and the specific evaluation inde...
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