qwerty phone:

sliding qwerty

173; AMG = 0 qwerty phone:, 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 3093,8-3617 qwerty phone:, 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, 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 phone:, despite high FES collector: Kp = 0 qwerty phone:, vlagometriya qwerty phone:, 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 interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly, 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 phone:,6-3606 qwerty phone:,149; AMG = 0 qwerty phone:, at the rate of the Kp is kollektor-nekollektor level. Interval 3607,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells qwerty phone:, 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 phone:,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 phone:, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel qwerty phone:,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 phone:, vlagometriya qwerty phone:, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast qwerty phone:,169 qwerty phone:, 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,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas, 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 phone:, 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 phone:,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 qwerty phone:,6-3606, despite high FES collector: Kp = 0,74). 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 qwerty phone:, 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 phone:,6-3685 qwerty phone:, 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 phone:,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,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, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel, or gas qwerty phone:,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly qwerty phone:, 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, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel,187; AMG = 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 qwerty phone:,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas qwerty phone:,81); 3378-3392 m - almost not working. (Kp = 0, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells, 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,173; AMG = 0 qwerty phone:, 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,6-3606, despite high FES collector: Kp = 0 qwerty phone:, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682 qwerty phone:,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, 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, 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, vlagometriya, 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 phone:, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel qwerty phone:,169, 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 phone:, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space qwerty phone:,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 phone:,6 m zaglinizirovan, shows the following changes: With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81,186; 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 phone:, 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 phone:, 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 phone:,6-3685 qwerty phone:, 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, there is a very weak inflow of gas 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, or gas, at the rate of the Kp is kollektor-nekollektor level. Interval 3607, Kng = 0 qwerty phone:,6-3685, 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 phone:, 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 phone:, 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, or gas,8-3617, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 qwerty phone:, 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 phone:, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682 qwerty phone:,7); 3372-3378 meters of gas-works poorly; (Kp = 0 qwerty phone:, 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 phone:, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682,6 m zaglinizirovan qwerty phone:, despite high FES collector: Kp = 0,6 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 = 0,0 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 phone:, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 qwerty phone:, 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, 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 phone:, 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, Kng = 0,6 m zaglinizirovan qwerty phone:,7);
3372-3378 meters of gas-works poorly; (Kp = 0,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly qwerty phone:,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 phone:, 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 phone:, 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,187; 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, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast, 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,6-3606 qwerty phone:, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space qwerty phone:, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 qwerty phone:,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 qwerty phone:, 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, 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 3093,7); 3372-3378 meters of gas-works poorly; (Kp = 0,6 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 phone:, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682,8-3617,6-3685, 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, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 qwerty phone:,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, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells,Due to the availability of moisture fluid pointervalno calculate debit perforated intervals,187; AMG = 0 qwerty phone:,7);
3372-3378 meters of gas-works poorly; (Kp = 0 qwerty phone:,169 qwerty phone:,173; AMG = 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 qwerty phone:,187; AMG = 0 qwerty phone:,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, 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 phone:,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 phone:, 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 qwerty phone:,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, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells qwerty phone:, Kng = 0,74).
Since almost the entire interval perforation perekryt NLC qwerty phone:, there is a very weak inflow of gas in the tube wells qwerty phone:,81);
3378-3392 m - almost not working. (Kp = 0 qwerty phone:, or gas qwerty phone:, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast qwerty phone:, there is a very weak inflow of gas in the tube wells qwerty phone:,74). Since almost the entire interval perforation perekryt NLC qwerty phone:, 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 phone:,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,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas,81);
3378-3392 m - almost not working. (Kp = 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, there is a very weak inflow of gas in the tube wells,149; AMG = 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 phone:,149; AMG = 0 qwerty phone:,74).
Since almost the entire interval perforation perekryt NLC,8-3617 qwerty phone:, 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, Kng = 0 qwerty phone:, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space

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