ISPRS Workshop on Service and Application of Spatial Data Infrastructure, XXXVI(4/W6), Oct. 14-16, Hangzhou, China
VISUALIZED APPLICATION OF GIS IN MINING SUBSIDENCE ANALYSIS
Huayang Dai a , Zuorua, Yin b , Zhiyi Deng a,c
‘'China University of Mining and Technology, Beijing campus, Beijing, 100083, China - daihuayang@263.net
b Kailuan (Group) Ltd. Liability Corporation , Tangshan, 063000, China - yzru@kailuan.com.cn
c Kailuan (Group) Ltd. Liability Corporation , Tangshan, 063000, China - dengzy@kailuan.com.cn
KEY WORDS: Visualized Application with GIS, Mining Subsidence Analysis System, Maplnfo/ MapBasic, Seam Inclination-
based Subsidence Model
ABSTRACT:
To determine the degree of mining affection on surface or in strata, the GIS technique is used, with Mapinfo as the platform.
Through programming of seam inclination-based subsidence mathematical models and mining disturbance analysis visualization,
Mapbasic/Vc++/Vfortran programming design is realized under Windows. The program system provides not only an effective
approach for model analysis, but also an efficient visual tool and interface for subsidence model application, laying therefore a solid
foundation for widespread use of the model.
1. INTRODUCTION ON MINING SUBSIDENCE
MODEL
1.1 General Instructions
A new subsidence model is put forward to calculate surface
movement and deformation induced by coal seam mining[l,2].
The approach features that: the seam inclination angle, as the
most prominent influential factor, among others, governing the
pattern of ground movement, is reckoned as a principal
parameter while the individual elements in working seams with
any dip angles are considered to be surface micro-element
vectors which are then resolved according to the parallelogram
law; introduction of mining influential functions respectively
for vertical and horizontal components of surface micro-element,
based on random medium theory; introduction of rock
movement parameters irrespective of the occurrence pattern
and size of workings; determination of the unit movement
trough through integrating both vertical and horizontal
components according to equivalent influence principle;
development of a continuous mining subsidence mathematical
model through surface integral of influential functions over the
entire area above the workings, according to the principle of
superimposition. A totally new theory and method, so-called
vector prediction method that is applicable for seams with dip
angles ranging 0-90° is thus developed through combining the
seam dip angle based maximum subsidence calculation model,
mining influence propagation angle calculation model as well as
the design routine of these models' programmed algorithms.
W eh (x,y)
x 2 + (,y-Hctg0 o ) 2
cos a * r i
—
(1)
dSv is the vertical mining unit with an area of l*sina and a
thickness of 1. It can also be reckoned as a horizontal mining
unit with an area of 1><1 and a thickness of sina. Similarly, the
expression for the subsidence basin for the vertical component
dSv can be obtained as follows:
x 2 +(y-Hctg0 o ) 2
X ,
(2)
sin Cl
W ev (x,y) = — r e
In Equations (1) and (2):
Weh(x, y), Wev (x, y) - Mining subsidence basins of dSh and
dSv respectively
rh, rv - Main influence radii of mining of flat and vertical
seams respectively
H - Mining depth of dS at point P
00 - Mining influence propagation angle
By superimposition of the subsidence basins of the horizontal
component and vertical component, we obtain the expression
for the subsidence basin for dS:
W e {x,y) = W eh {x,y)+W ev {x,y) (3)
Considering the orthogonality of the micro-unit vector’s two
basic components of dSh and dSv, we have:
f
I \[w eh {x,y)dS v =0
and hence
V' (w) = W mn iH s WJx,y)dS h + fjW tv (x,y)dSv (4)
As can be seen from Equation (4), the rock and surface
movements caused by mining of a pitching seam may be
attributed to two mining influences. One is the influence
produced by the horizontal component and the other by the
vertical component. The superimposed area of the horizontal
mining component is equal to the projected area of the working
face on the horizontal plane; while the superimposed area of the
vertical component is equal to the projected area of the working
face on the vertical plane. Therefore, the horizontal and vertical
projections can respectively be taken as the field of integration
in the integration operation. The integrand is the function in the
domain of area of S with varying Z coordinates. The
significance of Equation (4) lies in that it enables the integration
over the domain of area S to be converted to integration over its
vertical and horizontal projected areas. This lays the foundation
for the design of the algorithm of the vector method.
According to the basic theory of ground movement, there
exists a functional relation between ground movement and the