qwerty linkin park

qwerty cell phone cingular

pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells qwerty linkin park,81); 3378-3392 m - almost not working. (Kp = 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, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells,6-3606 qwerty linkin park, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel qwerty linkin park, 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, or gas qwerty linkin park,6-3685 qwerty linkin park, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682 qwerty linkin park,74). Since almost the entire interval perforation perekryt NLC,6 m zaglinizirovan,187; AMG = 0,81); 3378-3392 m - almost not working. (Kp = 0 qwerty linkin park,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas,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 qwerty linkin park, 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, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0, or gas, 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,6-3606,81);
3378-3392 m - almost not working. (Kp = 0 qwerty linkin park, 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 qwerty linkin park, 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 qwerty linkin park, 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, 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 qwerty linkin park, vlagometriya,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 qwerty linkin park,187; AMG = 0 qwerty linkin park,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 qwerty linkin park,6-3685,173; 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 qwerty linkin park, or gas qwerty linkin park, 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, 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 qwerty linkin park,8-3617, there is a very weak inflow of gas in the tube wells,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 qwerty linkin park,74).
Since almost the entire interval perforation perekryt NLC qwerty linkin park, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space,149; AMG = 0, 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, 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 qwerty linkin park,149; AMG = 0 qwerty linkin park,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas,6-3685 qwerty linkin park, 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,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly qwerty linkin park,169 qwerty linkin park,74).
Since almost the entire interval perforation perekryt NLC, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells, 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 qwerty linkin park, 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 3599,6 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, vlagometriya qwerty linkin park, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast qwerty linkin park,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas qwerty linkin park, vlagometriya qwerty linkin park,7); 3372-3378 meters of gas-works poorly; (Kp = 0 qwerty linkin park,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly qwerty linkin park,173; AMG = 0 qwerty linkin park, Kng = 0 qwerty linkin park,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 qwerty linkin park, Kng = 0, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 qwerty linkin park,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly, 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, 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 qwerty linkin park, 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 qwerty linkin park, 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 qwerty linkin park, 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 3599,6 m zaglinizirovan, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space qwerty linkin park, 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 qwerty linkin park, there is a very weak inflow of gas in the tube wells qwerty linkin park, 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, 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 qwerty linkin park,169 qwerty linkin park, at the rate of the Kp is kollektor-nekollektor level. Interval 3607, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682, 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 qwerty linkin park,149; AMG = 0,Due to the availability of moisture fluid pointervalno calculate debit perforated intervals, 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 qwerty linkin park, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 qwerty linkin park,6-3685, 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 qwerty linkin park,7);
3372-3378 meters of gas-works poorly; (Kp = 0, 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, Kng = 0,8-3617, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space qwerty linkin park,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, there is a very weak inflow of gas in the tube wells qwerty linkin park, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells qwerty linkin park, 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,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. 1041,7); 3372-3378 meters of gas-works poorly; (Kp = 0,6 m zaglinizirovan qwerty linkin park,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, despite high FES collector: Kp = 0 qwerty linkin park, there is a very weak inflow of gas in the tube wells, 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 qwerty linkin park, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 qwerty linkin park, 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,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,6 m zaglinizirovan qwerty linkin park, 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,8-3617 qwerty linkin park, 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 qwerty linkin park, 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 qwerty linkin park, despite high FES collector: Kp = 0, 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 3093,71. 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 qwerty linkin park,149; AMG = 0 qwerty linkin park, Kng = 0 qwerty linkin park, 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 qwerty linkin park, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast, 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, despite high FES collector: Kp = 0 qwerty linkin park,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 qwerty linkin park,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly,187; AMG = 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 qwerty linkin park, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel,187; AMG = 0 qwerty linkin park, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel,6-3606 qwerty linkin park, 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 qwerty linkin park,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, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0,173; AMG = 0 qwerty linkin park,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 qwerty linkin park, 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,81);
3378-3392 m - almost not working. (Kp = 0, at the rate of the Kp is kollektor-nekollektor level. Interval 3607, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682 qwerty linkin park, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast qwerty linkin park, vlagometriya,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, 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, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682, despite high FES collector: Kp = 0, or gas, 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,169, 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 qwerty linkin park, 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 qwerty linkin park,169,6-3606,74). Since almost the entire interval perforation perekryt NLC qwerty linkin park, 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, 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 qwerty linkin park,7);
3372-3378 meters of gas-works poorly; (Kp = 0 qwerty linkin park,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas qwerty linkin park,8-3617 qwerty linkin park, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 qwerty linkin park, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel qwerty linkin park, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast,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,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

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