THE STRUCTURE OF ZONAL DISINTEGRATION OF MINING
STRUCTURES
S.V. Tynyna1*,
I.I. Chobotko1
1Institute for Physics of Mining Processes
of the National Academy of Sciences of Ukraine, Dnipro, Ukraine
*Corresponding author:
e-mail: haritonroots@gmail.com
Physical and
technical problems of mining production, 2021, (23), 98-107.
https://doi.org/10.37101/ftpgp23.01.007
full
text (pdf)
ABSTRACT
Purpose. There is
an expansion of ideas about
the structure of zonal disintegration
of the rock mass and
the nature of its development,
the study of the nature
of the formation of systems of disintegrated structures, the development of the hypothesis
of the emergence of zonal disintegration.
Methods. When
solving the set tasks, the method of critical analysis was applied in relation to the "Effect of zonal disintegration
of rocks", which is an
alternation of zones of disturbed
and undisturbed rocks.
Findings. The article
provides an analysis of scientific works on the disintegration
of rocks since the discovery
of this phenomenon in 1972. Recommendations are given to combat
this phenomenon in mining operations.
Originality. The proposed
generalizing hypothesis
of the formation of disintegration of the rock mass
around the workings. The structure of disintegrated formations is considered. The definition of the concept
"Systems of disintegrated structures"
is given. The dependence of the degree
of disintegration as a physical phenomenon on the types of
mining operations is shown.
Practical implications. A hypothesis
of the occurrence of the phenomenon of zonal disintegration
of the structure of rocks has been
developed. The structure of the zonal disintegration
of the rock mass around
the workings is considered. The definition is given to
Systems of disintegrated structures.
Keywords: stability
of mine workings, zonal disintegration, rock structure, stress and deformation field around the mine contour,
bearing armored shell zone, rock pressure, rings of zonal
disintegration, dynamic
action, active zone of the
stress field of the mine
contour, distribution of rock stress
concentrators
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