Zobrazeno 1 - 10
of 10
pro vyhledávání: '"AP Khmelinin"'
Publikováno v:
Фундаментальные и прикладные вопросы горных наук. 7:213-219
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 773:012091
An overview of methods for mapping disturbances in a rock mass is given on the example of determining hydraulic fracture systems in an oil-filled formation. Methods of passive and active microseismic monitoring, as well as electromagnetic examining o
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 773:012001
Numerical modeling was performed for stress-strain state of the rock mass and lining of underground turbine hall of Rogun hydropower plant. The hall is located in a rock mass at great depths. Numerical modeling was conducted using the method of bound
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 523:012032
The authors discuss the problem connected with the assessment of hydraulic fracturing quality in oil-filled formations by means of location and sizing of hydrofractures. The proposed engineering solution is to design a down-the-hole measuring probe b
Autor:
AP Khmelinin, E.A. Khristolyubov, DV Baryshnikov, A. I. Konurin, V. N. Filippov, A. A. Eremenko
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 134:012015
The factors that influence geomechanical state of rock mass in Sheregesh Mine are determined. The authors discuss a variant of geotechnology with fan drilling. The drill-hole patterns and drilling-and-blasting parameters are presented. The revealed c
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 134:012030
Publikováno v:
IOP Conference Series: Earth & Environmental Science; Jun2019, Vol. 262 Issue 1, p1-1, 1p
Publikováno v:
IOP Conference Series: Earth & Environmental Science; Mar2018, Vol. 134 Issue 1, p1-1, 1p
Publikováno v:
IOP Conference Series: Earth & Environmental Science; Mar2018, Vol. 134 Issue 1, p1-1, 1p
Publikováno v:
IOP Conference Series: Earth & Environmental Science; 2021, Vol. 773, p1-5, 5p