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Characteristics of dissolved inorganic carbon in produced water from coalbed methane wells and its geological significance
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YANG Zhaobiao,QIN Yong,QIN Zonghao,YI Tongsheng,LI Cunlei,ZHANG Zhengguang
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Table 1 Basic development parameters and stable carbon isotope test results of CBM wells in the study area.
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Well number | Syncline | Ro,max/ % | Developedcoal seam | Depth/ m | Daily pro- duction/m3 | δ13CDIC/ ‰ | δ13C1/ ‰ | Starting time of produc- tion (year-month) | GP-1 | Tucheng | 1.4-1.69 | 6/9/12/13/15/16/29 | 847.00 | 337 | -0.82 | -42.90 | 2014-01 | GP-2 | 1.4-1.69 | 1+3/5/9/10/11/13/15/16 | 764.00 | 408 | 11.27 | unsampled | 2014-01 | GP-3 | 1.4-1.69 | 6/9/12/13/15/29 | 610.00 | 607 | 4.50 | -43.60 | 2015-01 | GP-4 | 1.4-1.69 | 6/9/13/15/16/29 | 564.50 | 464 | 6.64 | unsampled | 2015-01 | GP-5 | 1.4-1.69 | 1+3/4/5/6/9/13/15/29 | 654.00 | 213 | -2.73 | -43.50 | 2015-01 | GP-6 | 1.4-1.69 | 1+3/4/5/6/9/15/16/26/27/29 | 617.00 | 570 | 3.93 | -41.90 | 2015-01 | GP-7 | 1.4-1.69 | 1+3/4/5/12/15/27/29 | 902.00 | 277 | 0.19 | unsampled | 2015-01 | GP-8 | 1.4-1.69 | 1+3/4/5/12/13/15/26/27/29 | 977.08 | 341 | 7.49 | -42.30 | 2015-01 | ZH1 | Dahebian | 1.09 | C406/C409 | 852.35 | 1070 | 2.73 | -44.10 | 2016-06 | N1 | Bide | 2.39 | 30/32 | 876.00 | 111 | 27.156 | -34.80* | 2016-02 | N3 | 2.20 | 30/32 | 918.00 | 674 | -2.15 | -34.30 | 2016-02 | B1 | 2.19 | 2/3/6 | 596.70 | 882 | -2.13 | -34.50 | 2015-04 | F2 | Changgang | 3.66 | 4/7/10 | 692.70 | 264 | 0.98 | -33.70 | 2015-11 | D2 | Huangnitang | 3.11 | 6/7/10 | 542.00 | 1152 | -1.22 | -34.80 | 2015-09 | ZP1 | Zhuzang | 3.60 | 23 | 1105.00 | 3146 | 1.71 | -34.40 | 2015-10 | Z2 | 3.60 | 20/23/27/30 | 739.80 | 887 | 0.11 | -34.00 | 2015-02 | Z3 | 3.60 | 20/23/27/30 | 567.10 | 993 | -1.07 | -34.90 | 2015-05 | Z4 | 3.60 | 20/23/27/30 | 561.50 | 1271 | -6.68 | -35.20 | 2015-02 | Z5 | 3.60 | 20/23/27/30 | 689.40 | 1348 | -1.84 | -34.60 | 2015-05 | Z6 | 3.60 | 20/23/27/30 | 759.00 | 1059 | 4.91 | unsampled | 2015-02 |
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