Full text: Proceedings, XXth congress (Part 4)

  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B4. Istanbul 2004 
  
6. CONCLUSION 
The subsurface engineering is truly three-dimensional and is 
required a real 3D data model. For the purpose of describing 
different subsurface objects, many 3D data models and data 
structures have been investigated. Our experimental results 
demonstrated that the proposed 3D data model based on QTPV 
is feasible and efficient in modeling irregular geological objects 
and regular subsurface engineering. The following conclusions 
can be drawn: 
(1) The developed 3D QTPV data model has the ability of 
modeling regular and irregular 3D objects. Although it is a 
volumetric model, but we can also get the surface model of 
the modeled objects by designing a special algorithm. For 
example, for the purpose of obtaining a stratigraphy 
interface, we should seek all the triangles which have the 
same positive-negative attribute while the attribute of 
positive side and negative side are different for one triangle. 
The QTPV data structure could not only overcome the strict 
data restriction, i.e. the captured points should be located on 
a regular 3D grid, but also overcome the disadvantages of 
TEN, such as huge data volume, complex topological 
relationship and modeling algorithm complex. 
ro 
— 
— 
UG 
— 
) The complex geological objects could be described by using 
only QTPV data structure while hybrid data structure does 
not need. Thus it is convenient for database management. 
(4 
— 
When adding attribute structure on the vertices and 
attaching digitized borehole log to the edges of QTPV, we 
can get thc inner attribute of geological objects at any 
position by using linear or finite element interpolation 
methods. Thus the real 3D management of geological 
bodies can be achieved. 
Our applicable cases are only stratigraphy modeling according 
to real borehole captured data and simulated laneway data. The 
further works are taking into account for more complex 
geological objects and consummate modeling, visualization and 
model manipulation methods. 
ACKNOWLEDGEMENTS 
The research is financially supported by the Hong Kong 
Polytechnic University ASD research fund under contract 
number of No. 1.34.4222 and the Open Research Fund 
Program of LIESMARS under the contract number of No. WKL 
(01) 0302. 
REFERENCES 
Breuning, M., 1996. Integration of spatial information for geo- 
information systems: Lecture Notes in Earth Sciences. Springer. 
Berlin, 167 pp. 
Chen, X.Y.. Doihara, H. and Nasu, M., 1995. A workstation for 
three-dimensional spatial data research. In: the 4th International 
Symposium of LIESMARS: Towards | three-dimensional, 
temporal and dynamic spatial data modeling and analysis, 
Wuhan, China, pp.42-51. 
Cheng. P.G. and Gong, J.Y., 2001. Design of three-dimensional 
spatial data model and its data structure in geological 
44 
exploration engineering. Acta Geodatica et Cartographica 
Sinica, 30(1), pp.74-81. (in Chinese) 
Fritsch, D., 1996. Three-dimensional geographic information 
system---status and prospects. In: International Archives of 
Photogrammetry and Remote Sensing, Vienna, Austria, Vol. 31, 
Part B3, pp.215-221. 
Gong, J. Y. and Cheng P.G. 2002. Study on 3D modeling and 
Visualization in Geological Exploration Engineering. In: The 
International Archives of the Photogrammetry, Remote Sensing 
and Spatial Information Sciences, Xi'an, P.R.China, Vol. 
XXXIV, Part 2/11, pp. 456-469. 
Gong, J.Y. and Xia, Z.G., 1997. An integrated data model in 
three-dimensional GIS. Journal of Wuhan Technical University 
of Surveying and Mapping, 22(1), pp.7-15. (in Chinese) 
Houlding, S.W., 1994. 3D geoscience modeling---computer 
techniques for geological characterization. Springer-Verlag, 
New York, (303 pp.). 
Li, D.R. and Li, Q.Q., 1997. A study on hybrid data structurc in 
3D GIS. Acta Geodatica et Cartographica Sinica, 26 (2), 
pp. 128-133. (in Chinese) 
Molenaar, M., 1992. A topology for 3D vector maps. /7C 
Journal, 1992-1, pp.25-33. 
Pilout, M., Tempfli, K.and Molenaar, M., 1994. A tetrahedron- 
based on 3D vector data model for geoinformation. In: 
Molenaar, M. and S. de Hoop, (Eds.), Advanced Geographic 
Data Modeling. | Netherlands ^ Geodetic — Commission, 
Publications on Geodesy, Delft, The Netherlands, Vol.40. pp. 
129-140. 
Qi, A. W., Wu, L.X. and Li, B. et al., 2002. Anologic tri-prim: a 
new 3D geological modeling methodology, Journal of China 
Coal Society, 27 (2), pp.158-163. (in Chinese) 
Shi, W.Z., 1996. A hybrid model for 3D GIS. Geoinformatics, 
1996-1, pp.400-409. 
Sun. M., Chen, IK, Zhang, X.Z., 2000. A 3D CM data model 
based on surface partition. Acta Geodatica et Cartographica 
Sinica, 29 (3), pp.257-265. (in Chinese) 
Wu, L.X, Shi, W.Z. and Gold, C., 2003. Spatial modeling 
technologies for 3D GIS and 3D GMS. Geography and Geo- 
Information Science, 19 (1), pp.5-11. (in Chinese) 
development. 
Zlatanova, $.,. 2000, 3D GIS’ for‘ urban 
Netherlands: ITC dissertation, pp.154-159. 
Zhang, Y. and Bai, S.W., 2001. An approach of 3D stratum 
modeling based on tri-prism volume elements. Journal of Image 
and Graphics, 6 (3). pp.285-290. (in Chinese) 
KEY WORDS: 
ABSTRACT: 
Efficient modelli 
analysis and man 
of MI content is ¢ 
Towards this goa 
and the developn 
movement and de 
as they are captur 
extension of exis 
context of geospa 
and spatiotempor 
objects over time. 
transition (MST) 
in detail, and proc 
The image proce: 
of object represei 
are techniques th: 
over time. Motio 
feeds or multitem 
typically address 
spatiotemporal in 
to the involved 
spatiotemporal v 
1996; Hornsby ai 
programs (Pope, 
represent some aj 
image  processin 
information. 
In order to accon 
databases we hav 
helix as a modell 
information hand 
and Stefanidis 2( 
that they not only 
mass, but also i 
outlinc. Furtherm 
in an objects hi: 
are more than ju: 
databases and d: 
query for particul 
an overview of 
comparison metri
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.