Method for calculating electrical evaluation standard of coal seam surrounding rock water yield property
A technology of evaluation standards and calculation methods, which is applied to earth-moving drilling, surveying, wellbore/well components, etc. It can solve the problems of long model establishment and analysis cycle, many factors to consider, and poor economic benefits, and achieve model establishment and analysis. Short cycle, strong universality, cost-saving effect
- Summary
- Abstract
- Description
- Claims
- Application Information
AI Technical Summary
Problems solved by technology
Method used
Image
Examples
Embodiment 1
[0049] This embodiment provides a specific structure of the calculation method of the water-rich electrical property evaluation standard of the surrounding rock of the coal seam, such as figure 1 shown, including the following steps:
[0050] Establish the electrical and lithological interpretation template of the coal seam surrounding rock, and screen the aquifer based on the lithology discrimination conditions of the aquifer;
[0051] Create a template for the interpretation of physical properties of the aquifer;
[0052] Determine the lower limit of the physical properties of the aquifer, and screen out the aquifer;
[0053] Calculate the water-richness evaluation index of the aquifer, and establish the water-richness electrical property evaluation standard of the aquifer based on the water-richness classification standard of the aquifer.
[0054] Specifically, an interpretation template for the electrical properties and lithology of the surrounding rock of the coal seam ...
Embodiment 2
[0078] In this embodiment, the T1 borehole flow logging in the Gaojiabao mining area is taken as an example. The T1 borehole flow logging results and water-rich evaluation results in the Gaojiabao mining area are shown in the following table. Among them, for the 620-660m well section and 680-700m well section, the evaluation index Q is 1.26L / (s m) and 1.10L / (s m) respectively. The classification standard is determined as strong water-rich aquifer, and the lower limit standard for calculating the porosity of the strong water-rich aquifer in the Gaojiabao mining area is 20%. The calculation method is:
[0079] PORlow=(23.8*21.1+13.6*18.6) / (23.8+13.6)≈20%
[0080] Similarly, the lower limit standard of Vsh for strong water-rich aquifer in Gaojiabao mining area is calculated as 18%.
[0081] The flow logging and water-rich evaluation table of Well T1 in the Gaojiabao mining area are as follows:
[0082]
[0083] From this calculation conclusion, it is determined that the elec...
PUM
Login to View More Abstract
Description
Claims
Application Information
Login to View More 

