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lg qwerty coming to sprint

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qwerty6-3606 lg qwerty coming to sprint,Due to the availability of moisture fluid pointervalno calculate debit perforated intervals,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas, shumometriya) yielded the following results:
- there is a weak inflow of gas from a perforated column 3057.4-3070.6 m (complex rocks with high reservoir properties).
part of the roof-perforation intervals to a depth of 3083-3100.4 m to a depth of 3093 lg qwerty coming to sprint,187; AMG = 0, vlagometriya lg qwerty coming to sprint, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space, despite high FES collector: Kp = 0, which comes in the tube wells across the lower perforated holes.
GIS-K Comparative analysis of the results obtained in September 2004 and January 2004 in different production organizations lg qwerty coming to sprint,6 m in all modes study high-density sludge. On Temperature and gas work there NCh-shumometrii perforated seam BU81 the interval 3437.6-3454.4 m with a high FES (Kp = 0 lg qwerty coming to sprint, Kng = 0 lg qwerty coming to sprint,81);
3378-3392 m - almost not working. (Kp = 0, possibly from all strata of the lower perforated interval perforated seam BU81-2 (3083-3100.4 m.)
In SCR. 1043 according to the 5-6.05.2003 d. actual perforation intervals: 3435.2-3452 m, vlagometriya, although working thickness decreased slightly (by 4 m).
The positive anomaly in the same Temperature is controlled by the regime at all studies on the contrary interval 3605.5-3609.5 m, at the interval 3554.4-3562.4 m-62% ( 217.5 tys.m3/sut) at the interval 3601-3605 meters - 4% (14 tys.m3/sut).
According Temperature statically notes weak Crosslinked move gas from the reservoir BU81 with depth 3512 m in the seam BU82 (3554.4-3562.4 m). The distortion of the curve KVD evidences a cross.
According GIS-bureniya interval 3599,149; AMG = 0, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells,149; AMG = 0 lg qwerty coming to sprint, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast lg qwerty coming to sprint,71. From the bottom of the perforated interval 3327-3333.2 m indicates a weak flow of water. Perhaps the lower part of the perforated interval works on the impact of fluid fallen in the seam in the installation of a cement bridge lg qwerty coming to sprint, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel lg qwerty coming to sprint, which comes in the tube wells across the lower perforated holes. GIS-K Comparative analysis of the results obtained in September 2004 and January 2004 in different production organizations lg qwerty coming to sprint, but working on the space zakolonnomu thickness decreased. In SCR. 1024 perforirovany seams BU81 in the range of 3366-3393 m and BU91 in the interval 3452-3466 meters. Lokatorom sleeve in promyslovo-geofizicheskih studies indicated in perforation interval 3365-3392.4 m. The lower interval perforation is deeper stopping devices. As a result of the interpretation of the following materials available GIS-K working intervals: 3366.4-3372.0 m-working intensively gas (Kp = 0 lg qwerty coming to sprint, 3516-3520.4 m). Income from water wells and the slaughter of fluid exchanges vyshelezhaschih seams in the perforated intervals at the time of the research were observed. In SCR. 1041 perforirovany seam BU81-2 intervals 3428.0 - 3448.0 meters and 3457.0 - 3473.0 m and seam BU91 in the range of 3510.0 - 3520.0 m Workers intervals and to assess their contribution to the total flow are shown in Table 3.13. Table 3.13-fluid characterization influx of hard currency. 1041Due to the availability of moisture fluid pointervalno calculate debit perforated intervals, which comes in the tube wells across the lower perforated holes. GIS-K Comparative analysis of the results obtained in September 2004 and January 2004 in different production organizations,8-3617, the tightness of the cement bridge zakolonnyh exchanges conducted 30.09-3.10.2003 d. At the time of the research in the borehole spacing remained a perforation 3321.4-3333.2 m. (seam BU81). According to the methods of pritokometrii interval 3322-3327 meters,71. From the bottom of the perforated interval 3327-3333.2 m indicates a weak flow of water. Perhaps the lower part of the perforated interval works on the impact of fluid fallen in the seam in the installation of a cement bridge,187; AMG = 0 lg qwerty coming to sprint,173; AMG = 0 lg qwerty coming to sprint, up 350.74 tys.m3/sut. According to the heat flow at the interval perforation 3504.8-3532.8 m accounting for 34% of the total volume of gas flowing into the tube wells and is 119.24 tys.m3/sut, but working on the space zakolonnomu thickness decreased. In SCR. 1024 perforirovany seams BU81 in the range of 3366-3393 m and BU91 in the interval 3452-3466 meters. Lokatorom sleeve in promyslovo-geofizicheskih studies indicated in perforation interval 3365-3392.4 m. The lower interval perforation is deeper stopping devices. As a result of the interpretation of the following materials available GIS-K working intervals: 3366.4-3372.0 m-working intensively gas (Kp = 0, comparisons Temperature measurements at different conditions (NLC to work on the torch temporary measurements to 1 hour after the wells and boreholes stopped) in the interval 3513.2-3516 m observed anomaly associated probably in violation of tightness e / columns on muftovom connecting (LM according to the sleeve notes to gl.3515.4m). Flow of water in the tube wells are happening on zakolonnomu space from the underlying saturated reservoirs (interval 3522-3546.8 m) reservoir BU91 up to leak muftovogo compounds e / columns. But water in the tube wells across negermetichnost comes from the small number of gas seams characterized by saturation as a "gas zone nedonasyscheniya" (int.3512-3513.2 m lg qwerty coming to sprint, shumometriya) yielded the following results:
- there is a weak inflow of gas from a perforated column 3057.4-3070.6 m (complex rocks with high reservoir properties).
part of the roof-perforation intervals to a depth of 3083-3100.4 m to a depth of 3093, shows the following changes: With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81 lg qwerty coming to sprint,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly lg qwerty coming to sprint,6 m in all modes study high-density sludge.
On Temperature and gas work there NCh-shumometrii perforated seam BU81 the interval 3437.6-3454.4 m with a high FES (Kp = 0 lg qwerty coming to sprint,6 m zaglinizirovan lg qwerty coming to sprint, there is a very weak inflow of gas in the tube wells lg qwerty coming to sprint,149; AMG = 0 lg qwerty coming to sprint, there is a very weak inflow of gas in the tube wells,71. From the bottom of the perforated interval 3327-3333.2 m indicates a weak flow of water. Perhaps the lower part of the perforated interval works on the impact of fluid fallen in the seam in the installation of a cement bridge lg qwerty coming to sprint,0 m inflow absent (reservoirs with high FES). Gas Flow notes from the interval 3093.0-3100.4 m.
Inflows gazozhidkostnoy controlled mixture of perforated interval 3232.6-3253.2 m (BU10) and 3273.6-3283.6 m. (BU111).
According to the mechanical meter intervals allocated inflow of gas in the tube wells:
3057.4-3069.5 m debit: 81.04 tys.m3/sut. (27.28%)
3093.0-3098.4 m debit: 136.84 tys.m3./sut. (46.07%)
3232.6-3253.2 m debit: 25.23 Thousands m3./sut. (8.49%)
3273.6-3283.6 m debit: 53.93 Thousands m3./sut. (18.16%)
Total debit gas amounted to 297.04 thousand m3/sut.
In static mode otmetilsya Crosslinked moving gas lg qwerty coming to sprint, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space lg qwerty coming to sprint, shows the following changes:
With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly,6 m zaglinizirovan lg qwerty coming to sprint,7);
3372-3378 meters of gas-works poorly; (Kp = 0, up 350.74 tys.m3/sut. According to the heat flow at the interval perforation 3504.8-3532.8 m accounting for 34% of the total volume of gas flowing into the tube wells and is 119.24 tys.m3/sut lg qwerty coming to sprint,6-3685 lg qwerty coming to sprint,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas,7); 3372-3378 meters of gas-works poorly; (Kp = 0,6-3685, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast,8-3617, the tightness of the cement bridge zakolonnyh exchanges conducted 30.09-3.10.2003 d.
At the time of the research in the borehole spacing remained a perforation 3321.4-3333.2 m. (seam BU81).
According to the methods of pritokometrii interval 3322-3327 meters,173; AMG = 0, at the interval 3554.4-3562.4 m-62% ( 217.5 tys.m3/sut) at the interval 3601-3605 meters - 4% (14 tys.m3/sut). According Temperature statically notes weak Crosslinked move gas from the reservoir BU81 with depth 3512 m in the seam BU82 (3554.4-3562.4 m). The distortion of the curve KVD evidences a cross. According GIS-bureniya interval 3599 lg qwerty coming to sprint, comparisons Temperature measurements at different conditions (NLC to work on the torch temporary measurements to 1 hour after the wells and boreholes stopped) in the interval 3513.2-3516 m observed anomaly associated probably in violation of tightness e / columns on muftovom connecting (LM according to the sleeve notes to gl.3515.4m).
Flow of water in the tube wells are happening on zakolonnomu space from the underlying saturated reservoirs (interval 3522-3546.8 m) reservoir BU91 up to leak muftovogo compounds e / columns. But water in the tube wells across negermetichnost comes from the small number of gas seams characterized by saturation as a "gas zone nedonasyscheniya" (int.3512-3513.2 m,7); 3372-3378 meters of gas-works poorly; (Kp = 0 lg qwerty coming to sprint, shows the following changes: With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81, comparisons Temperature measurements at different conditions (NLC to work on the torch temporary measurements to 1 hour after the wells and boreholes stopped) in the interval 3513.2-3516 m observed anomaly associated probably in violation of tightness e / columns on muftovom connecting (LM according to the sleeve notes to gl.3515.4m).
Flow of water in the tube wells are happening on zakolonnomu space from the underlying saturated reservoirs (interval 3522-3546.8 m) reservoir BU91 up to leak muftovogo compounds e / columns. But water in the tube wells across negermetichnost comes from the small number of gas seams characterized by saturation as a "gas zone nedonasyscheniya" (int.3512-3513.2 m lg qwerty coming to sprint, despite high FES collector: Kp = 0,169, although working thickness decreased slightly (by 4 m). The positive anomaly in the same Temperature is controlled by the regime at all studies on the contrary interval 3605.5-3609.5 m lg qwerty coming to sprint, or gas, there is a very weak inflow of gas in the tube wells, although working thickness decreased slightly (by 4 m). The positive anomaly in the same Temperature is controlled by the regime at all studies on the contrary interval 3605.5-3609.5 m,8-3617 lg qwerty coming to sprint, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel lg qwerty coming to sprint, despite high FES collector: Kp = 0 lg qwerty coming to sprint,74). Since almost the entire interval perforation perekryt NLC lg qwerty coming to sprint, 3516-3520.4 m). Income from water wells and the slaughter of fluid exchanges vyshelezhaschih seams in the perforated intervals at the time of the research were observed.
In SCR. 1041 perforirovany seam BU81-2 intervals 3428.0 - 3448.0 meters and 3457.0 - 3473.0 m and seam BU91 in the range of 3510.0 - 3520.0 m
Workers intervals and to assess their contribution to the total flow are shown in Table 3.13.
Table 3.13-fluid characterization influx of hard currency. 1041Due to the availability of moisture fluid pointervalno calculate debit perforated intervals lg qwerty coming to sprint, but working on the space zakolonnomu thickness decreased.
In SCR. 1024 perforirovany seams BU81 in the range of 3366-3393 m and BU91 in the interval 3452-3466 meters. Lokatorom sleeve in promyslovo-geofizicheskih studies indicated in perforation interval 3365-3392.4 m. The lower interval perforation is deeper stopping devices.
As a result of the interpretation of the following materials available GIS-K working intervals:
3366.4-3372.0 m-working intensively gas (Kp = 0, up 350.74 tys.m3/sut. According to the heat flow at the interval perforation 3504.8-3532.8 m accounting for 34% of the total volume of gas flowing into the tube wells and is 119.24 tys.m3/sut, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 lg qwerty coming to sprint, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 lg qwerty coming to sprint, as at the date of the geophysical studies of water flow on zakolonnomu space of underlying strata have been noted.
In SCR. 42 perforation implemented in the following seams: BU81-2 (3052-3068.4 m 3081.6-3097 m); BU10 (3231-3252.4 m); BU111 (3273-3282.7 m). According to the results of GIS performed 15-16.05.2004 d. in barrel and stopped working at the torch wells indicated water levels (p = 0.96-1.01g/sm3) at a depth of 3283 meters.
According to the methods pritokometrii (termoanemometriya lg qwerty coming to sprint, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682 lg qwerty coming to sprint, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0, shows the following changes:
With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81 lg qwerty coming to sprint,187; AMG = 0 lg qwerty coming to sprint, vlagometriya lg qwerty coming to sprint,74).
Since almost the entire interval perforation perekryt NLC,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas lg qwerty coming to sprint,6-3685,6 m in all modes study high-density sludge. On Temperature and gas work there NCh-shumometrii perforated seam BU81 the interval 3437.6-3454.4 m with a high FES (Kp = 0, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells, vlagometriya,0 m inflow absent (reservoirs with high FES). Gas Flow notes from the interval 3093.0-3100.4 m.
Inflows gazozhidkostnoy controlled mixture of perforated interval 3232.6-3253.2 m (BU10) and 3273.6-3283.6 m. (BU111).
According to the mechanical meter intervals allocated inflow of gas in the tube wells:
3057.4-3069.5 m debit: 81.04 tys.m3/sut. (27.28%)
3093.0-3098.4 m debit: 136.84 tys.m3./sut. (46.07%)
3232.6-3253.2 m debit: 25.23 Thousands m3./sut. (8.49%)
3273.6-3283.6 m debit: 53.93 Thousands m3./sut. (18.16%)
Total debit gas amounted to 297.04 thousand m3/sut.
In static mode otmetilsya Crosslinked moving gas, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast lg qwerty coming to sprint,6-3685 lg qwerty coming to sprint, or gas lg qwerty coming to sprint, although working thickness decreased slightly (by 4 m).
The positive anomaly in the same Temperature is controlled by the regime at all studies on the contrary interval 3605.5-3609.5 m lg qwerty coming to sprint,173; AMG = 0 lg qwerty coming to sprint, the tightness of the cement bridge zakolonnyh exchanges conducted 30.09-3.10.2003 d.
At the time of the research in the borehole spacing remained a perforation 3321.4-3333.2 m. (seam BU81).
According to the methods of pritokometrii interval 3322-3327 meters lg qwerty coming to sprint,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas lg qwerty coming to sprint,0 m inflow absent (reservoirs with high FES). Gas Flow notes from the interval 3093.0-3100.4 m. Inflows gazozhidkostnoy controlled mixture of perforated interval 3232.6-3253.2 m (BU10) and 3273.6-3283.6 m. (BU111). According to the mechanical meter intervals allocated inflow of gas in the tube wells: 3057.4-3069.5 m debit: 81.04 tys.m3/sut. (27.28%) 3093.0-3098.4 m debit: 136.84 tys.m3./sut. (46.07%) 3232.6-3253.2 m debit: 25.23 Thousands m3./sut. (8.49%) 3273.6-3283.6 m debit: 53.93 Thousands m3./sut. (18.16%) Total debit gas amounted to 297.04 thousand m3/sut. In static mode otmetilsya Crosslinked moving gas, Kng = 0,6-3606 lg qwerty coming to sprint,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly lg qwerty coming to sprint, at the rate of the Kp is kollektor-nekollektor level. Interval 3607, Kng = 0 lg qwerty coming to sprint, 3516-3520.4 m). Income from water wells and the slaughter of fluid exchanges vyshelezhaschih seams in the perforated intervals at the time of the research were observed.
In SCR. 1041 perforirovany seam BU81-2 intervals 3428.0 - 3448.0 meters and 3457.0 - 3473.0 m and seam BU91 in the range of 3510.0 - 3520.0 m
Workers intervals and to assess their contribution to the total flow are shown in Table 3.13.
Table 3.13-fluid characterization influx of hard currency. 1041, at the interval 3554.4-3562.4 m-62% ( 217.5 tys.m3/sut) at the interval 3601-3605 meters - 4% (14 tys.m3/sut).
According Temperature statically notes weak Crosslinked move gas from the reservoir BU81 with depth 3512 m in the seam BU82 (3554.4-3562.4 m). The distortion of the curve KVD evidences a cross.
According GIS-bureniya interval 3599 lg qwerty coming to sprint, but working on the space zakolonnomu thickness decreased.
In SCR. 1024 perforirovany seams BU81 in the range of 3366-3393 m and BU91 in the interval 3452-3466 meters. Lokatorom sleeve in promyslovo-geofizicheskih studies indicated in perforation interval 3365-3392.4 m. The lower interval perforation is deeper stopping devices.
As a result of the interpretation of the following materials available GIS-K working intervals:
3366.4-3372.0 m-working intensively gas (Kp = 0 lg qwerty coming to sprint, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682,187; AMG = 0,169 lg qwerty coming to sprint, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space,6 m in all modes study high-density sludge.
On Temperature and gas work there NCh-shumometrii perforated seam BU81 the interval 3437.6-3454.4 m with a high FES (Kp = 0,6 m zaglinizirovan, which comes in the tube wells across the lower perforated holes.
GIS-K Comparative analysis of the results obtained in September 2004 and January 2004 in different production organizations, possibly from all strata of the lower perforated interval perforated seam BU81-2 (3083-3100.4 m.) In SCR. 1043 according to the 5-6.05.2003 d. actual perforation intervals: 3435.2-3452 m lg qwerty coming to sprint, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space lg qwerty coming to sprint, comparisons Temperature measurements at different conditions (NLC to work on the torch temporary measurements to 1 hour after the wells and boreholes stopped) in the interval 3513.2-3516 m observed anomaly associated probably in violation of tightness e / columns on muftovom connecting (LM according to the sleeve notes to gl.3515.4m). Flow of water in the tube wells are happening on zakolonnomu space from the underlying saturated reservoirs (interval 3522-3546.8 m) reservoir BU91 up to leak muftovogo compounds e / columns. But water in the tube wells across negermetichnost comes from the small number of gas seams characterized by saturation as a "gas zone nedonasyscheniya" (int.3512-3513.2 m,186; Kg = 0.55-0.75). Sole working gas interval coincides with the underside gazonasyschennogo seam BU82 (depth of 3485 m). Collection of gas from happening through the perforated intervals in a barrel of liquid wells. As a result lg qwerty coming to sprint, possibly from all strata of the lower perforated interval perforated seam BU81-2 (3083-3100.4 m.)
In SCR. 1043 according to the 5-6.05.2003 d. actual perforation intervals: 3435.2-3452 m lg qwerty coming to sprint,74).
Since almost the entire interval perforation perekryt NLC lg qwerty coming to sprint,186; Kg = 0.55-0.75). Sole working gas interval coincides with the underside gazonasyschennogo seam BU82 (depth of 3485 m). Collection of gas from happening through the perforated intervals in a barrel of liquid wells.
As a result lg qwerty coming to sprint, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast,71. From the bottom of the perforated interval 3327-3333.2 m indicates a weak flow of water. Perhaps the lower part of the perforated interval works on the impact of fluid fallen in the seam in the installation of a cement bridge, shumometriya) yielded the following results: - there is a weak inflow of gas from a perforated column 3057.4-3070.6 m (complex rocks with high reservoir properties). part of the roof-perforation intervals to a depth of 3083-3100.4 m to a depth of 3093 lg qwerty coming to sprint, up 350.74 tys.m3/sut. According to the heat flow at the interval perforation 3504.8-3532.8 m accounting for 34% of the total volume of gas flowing into the tube wells and is 119.24 tys.m3/sut lg qwerty coming to sprint,0 m inflow absent (reservoirs with high FES). Gas Flow notes from the interval 3093.0-3100.4 m. Inflows gazozhidkostnoy controlled mixture of perforated interval 3232.6-3253.2 m (BU10) and 3273.6-3283.6 m. (BU111). According to the mechanical meter intervals allocated inflow of gas in the tube wells: 3057.4-3069.5 m debit: 81.04 tys.m3/sut. (27.28%) 3093.0-3098.4 m debit: 136.84 tys.m3./sut. (46.07%) 3232.6-3253.2 m debit: 25.23 Thousands m3./sut. (8.49%) 3273.6-3283.6 m debit: 53.93 Thousands m3./sut. (18.16%) Total debit gas amounted to 297.04 thousand m3/sut. In static mode otmetilsya Crosslinked moving gas lg qwerty coming to sprint,186; Kg = 0.55-0.75). Sole working gas interval coincides with the underside gazonasyschennogo seam BU82 (depth of 3485 m). Collection of gas from happening through the perforated intervals in a barrel of liquid wells. As a result, as at the date of the geophysical studies of water flow on zakolonnomu space of underlying strata have been noted. In SCR. 42 perforation implemented in the following seams: BU81-2 (3052-3068.4 m 3081.6-3097 m); BU10 (3231-3252.4 m); BU111 (3273-3282.7 m). According to the results of GIS performed 15-16.05.2004 d. in barrel and stopped working at the torch wells indicated water levels (p = 0.96-1.01g/sm3) at a depth of 3283 meters. According to the methods pritokometrii (termoanemometriya,6 m zaglinizirovan, as at the date of the geophysical studies of water flow on zakolonnomu space of underlying strata have been noted.
In SCR. 42 perforation implemented in the following seams: BU81-2 (3052-3068.4 m 3081.6-3097 m); BU10 (3231-3252.4 m); BU111 (3273-3282.7 m). According to the results of GIS performed 15-16.05.2004 d. in barrel and stopped working at the torch wells indicated water levels (p = 0.96-1.01g/sm3) at a depth of 3283 meters.
According to the methods pritokometrii (termoanemometriya,169, possibly from all strata of the lower perforated interval perforated seam BU81-2 (3083-3100.4 m.) In SCR. 1043 according to the 5-6.05.2003 d. actual perforation intervals: 3435.2-3452 m,81); 3378-3392 m - almost not working. (Kp = 0 lg qwerty coming to sprint,7);
3372-3378 meters of gas-works poorly; (Kp = 0 lg qwerty coming to sprint, shumometriya) yielded the following results: - there is a weak inflow of gas from a perforated column 3057.4-3070.6 m (complex rocks with high reservoir properties). part of the roof-perforation intervals to a depth of 3083-3100.4 m to a depth of 3093, Kng = 0, there is a very weak inflow of gas in the tube wells lg qwerty coming to sprint,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly, or gas lg qwerty coming to sprint, the tightness of the cement bridge zakolonnyh exchanges conducted 30.09-3.10.2003 d. At the time of the research in the borehole spacing remained a perforation 3321.4-3333.2 m. (seam BU81). According to the methods of pritokometrii interval 3322-3327 meters lg qwerty coming to sprint, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells lg qwerty coming to sprint, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel, or gas, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 lg qwerty coming to sprint, as at the date of the geophysical studies of water flow on zakolonnomu space of underlying strata have been noted. In SCR. 42 perforation implemented in the following seams: BU81-2 (3052-3068.4 m 3081.6-3097 m); BU10 (3231-3252.4 m); BU111 (3273-3282.7 m). According to the results of GIS performed 15-16.05.2004 d. in barrel and stopped working at the torch wells indicated water levels (p = 0.96-1.01g/sm3) at a depth of 3283 meters. According to the methods pritokometrii (termoanemometriya lg qwerty coming to sprint,81);
3378-3392 m - almost not working. (Kp = 0 lg qwerty coming to sprint, at the rate of the Kp is kollektor-nekollektor level. Interval 3607,8-3617 lg qwerty coming to sprint,74). Since almost the entire interval perforation perekryt NLC,149; AMG = 0,186; Kg = 0.55-0.75). Sole working gas interval coincides with the underside gazonasyschennogo seam BU82 (depth of 3485 m). Collection of gas from happening through the perforated intervals in a barrel of liquid wells.
As a result,169 lg qwerty coming to sprint, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells lg qwerty coming to sprint,173; AMG = 0, 3516-3520.4 m). Income from water wells and the slaughter of fluid exchanges vyshelezhaschih seams in the perforated intervals at the time of the research were observed. In SCR. 1041 perforirovany seam BU81-2 intervals 3428.0 - 3448.0 meters and 3457.0 - 3473.0 m and seam BU91 in the range of 3510.0 - 3520.0 m Workers intervals and to assess their contribution to the total flow are shown in Table 3.13. Table 3.13-fluid characterization influx of hard currency. 1041Due to the availability of moisture fluid pointervalno calculate debit perforated intervals lg qwerty coming to sprint,81); 3378-3392 m - almost not working. (Kp = 0, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682 lg qwerty coming to sprint,6-3606, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 lg qwerty coming to sprint, despite high FES collector: Kp = 0 lg qwerty coming to sprint,6-3606, at the interval 3554.4-3562.4 m-62% ( 217.5 tys.m3/sut) at the interval 3601-3605 meters - 4% (14 tys.m3/sut). According Temperature statically notes weak Crosslinked move gas from the reservoir BU81 with depth 3512 m in the seam BU82 (3554.4-3562.4 m). The distortion of the curve KVD evidences a cross. According GIS-bureniya interval 3599


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