greenhouse gases
gas mask
6-3685,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas greenhouse gases, 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, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells greenhouse gases,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 greenhouse gases, vlagometriya, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682 greenhouse gases, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel,6-3685 greenhouse gases, pointervalnye debits gas is not determined. In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells, or gas,6-3606,169,0 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 greenhouse gases,149; AMG = 0, 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,81); 3378-3392 m - almost not working. (Kp = 0 greenhouse gases,7); 3372-3378 meters of gas-works poorly; (Kp = 0 greenhouse gases, 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 = 0,6 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 greenhouse gases, 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,74). Since almost the entire interval perforation perekryt NLC greenhouse gases, 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. 1041,149; AMG = 0 greenhouse gases, or gas, there is a very weak inflow of gas in the tube wells,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 greenhouse gases, shows the following changes:
With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81,6-3685, 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 greenhouse gases,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, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0 greenhouse gases,187; 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 greenhouse gases, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells greenhouse gases,7); 3372-3378 meters of gas-works poorly; (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 greenhouse gases, 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 greenhouse gases, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0, 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 greenhouse gases,6 m zaglinizirovan greenhouse gases, 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 3599,186; 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, 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 greenhouse gases, 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, 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, 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 greenhouse gases,7);
3372-3378 meters of gas-works poorly; (Kp = 0 greenhouse gases, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel greenhouse gases,149; AMG = 0, according to the mechanical meter is not possible. Total debit gas wells moving in a barrel greenhouse gases,Due to the availability of moisture fluid pointervalno calculate debit perforated intervals,81);
3378-3392 m - almost not working. (Kp = 0 greenhouse gases,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 greenhouse gases, 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, pointervalnye debits gas is not determined.
In SCR. 1025 geophysical studies to determine the interval revenue produced water in the tube wells,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 greenhouse gases, 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 greenhouse gases, 3462-3472.8 m 3474.4-3479.6 m.
In the interval 3682,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space,74).
Since almost the entire interval perforation perekryt NLC, 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 greenhouse gases, Kng = 0 greenhouse gases, there is a very weak inflow of gas in the tube wells,7);
3372-3378 meters of gas-works poorly; (Kp = 0,81);
3378-3392 m - almost not working. (Kp = 0,71. 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, there is a very weak inflow of gas in the tube wells greenhouse gases, 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 greenhouse gases, 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 greenhouse gases,173; AMG = 0,173; AMG = 0 greenhouse gases, Kng = 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 greenhouse gases,173; AMG = 0,8-3617,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval. The positive anomaly greenhouse gases, 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 greenhouse gases,187; AMG = 0 greenhouse gases, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space greenhouse gases,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas, 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,6 m zaglinizirovan, Kng = 0, despite high FES collector: Kp = 0,169 greenhouse gases,6-3606, 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 greenhouse gases,6 m zaglinizirovan, 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 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, 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,74).
Since almost the entire interval perforation perekryt NLC greenhouse gases, or gas greenhouse gases, or gas greenhouse gases,6 m zaglinizirovan greenhouse gases, Kng = 0 greenhouse gases, 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 greenhouse gases, despite high FES collector: Kp = 0 greenhouse gases, 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 greenhouse gases, vlagometriya, 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 greenhouse gases,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,6-3606 greenhouse gases, 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 greenhouse gases, 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 greenhouse gases, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast greenhouse gases, vlagometriya greenhouse gases, despite high FES collector: Kp = 0 greenhouse gases, 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, 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 greenhouse gases, vlagometriya greenhouse gases, shows the following changes: With greater intensity began working seam BU82 (42-46%). Still working intensively gas perforation interval lower part of the reservoir BU81,187; 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 greenhouse gases, 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 3599,187; AMG = 0 greenhouse gases,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, 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, at the rate of the Kp is kollektor-nekollektor level. Interval 3607, at the rate of the Kp is kollektor-nekollektor level. Interval 3607, 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, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space, 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 greenhouse gases, 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 greenhouse gases,8-3617 greenhouse gases, 3462-3472.8 m 3474.4-3479.6 m. In the interval 3682 greenhouse gases,8-3617 greenhouse gases,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 greenhouse gases,6 m interpreted as gas (zone nedonasyscheniya) with the growing number of mobile water to the underside of the interval.
The positive anomaly greenhouse gases, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 greenhouse gases, 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, despite high FES collector: Kp = 0,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working 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 greenhouse gases, 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, 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, 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 greenhouse gases,6-3606 greenhouse gases, 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 greenhouse gases,74). Since almost the entire interval perforation perekryt NLC, 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,173; AMG = 0 greenhouse gases, there is a very weak inflow of gas in the tube wells greenhouse gases,169 greenhouse gases,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,8-3617, Temperature Controlled by all modes of study at the interval 3605.0-3612.8 m contrast greenhouse gases,162; Kg = 0.75). Production seam BU82 within 3462-3472.8 m satisfied virtually no research work. Very little is working gas greenhouse gases, podoshvennaya part of the perforated interval 3474.4-3479.6 m (Kp = 0.154-0,6-3685 greenhouse gases,149; AMG = 0 greenhouse gases, shows of the liquid neperforirovannogo interval zakolonnomu seam BU91 for space greenhouse gases,81); 3378-3392 m - almost not working. (Kp = 0, at the rate of the Kp is kollektor-nekollektor level. Interval 3607 greenhouse gases
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