Education of the republic of uzbekistan tashkent state technical university named after islam karimov



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Сборник журналя Техника Инновэйшн

Research methods. 
The criterion for estimating reserves using the pressure drop method was 
the volume of initial reserves involved in drainage and how it changes during operation. 
As a result of considering the reasons for achieving certain values of η
g
, all the deposits under 
consideration were divided into four groups. 
- A, deposits with η
g
= 0.8-0.95; 
- B, deposits with η
g
= 0.7-0.8; 
- C, deposits with η
g
= 0.6-0.7; 
- D, deposits with η
g
= 0.5-0.6. 
For deposits of groups A and B, the value of the final gas recovery factor is reliably 
determined by the 10th year of development, when the drilling of the field is completed and the 
entire deposit is involved in drainage. 
For fields of group C, the final gas recovery is determined by 14-16 years of development. 
For fields of group D, the final gas recovery is not determined even by the end of field 
development. 
This situation with the determination of gas recovery is explained by the fact that for fields of 
group D, in addition to geological and geological production factors, one of the decisive roles is.


110 
Predicted gas recovery factors for groups of fields 
Table 1. 
played by the reliability of determining the initial reserves and the efficiency of the selected development systems, which, of course, are determined at 
a later stage of reservoir exploitation. 
To confirm this hypothesis, statistical processing of the К
p
, К
g

r.w
), К
ex.g
sample was performed for deposits, considering these samples as 
random variables and using the methods of mathematical statistics widely used in geology [11].
In addition, there is no relationship between К

и К
p
, although it is known from the literature [8] that such a relationship exists for reservoirs with 
a granular pore structure, and especially high (r = 0.8 - 0.9) correlation coefficients have been established for terrigenous reservoirs represented by 
sandstones. Therefore, it should be assumed that the lack of communication is observed due to inaccurate definitions.
The presence of a correlation dependence between К
p
and Кex.g are interrelated and mutually determinable, and the probit function graph made 
it possible to isolate and exclude anomalous К
ex.g
values. 
After appropriate adjustments, a histogram of the К
ex.g
distribution was plotted (Fig. 1), which was calculated using mathematical statistics. Also, 
as in fig. 2, in Fig. 1, three groups of deposits are distinguished, which are consistent with the data. 

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