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Morphometric analysis of three-dimensional networks of karst conduits

Morphometric analysis of three-dimensional networks of karst conduits
Morphometric analysis of three-dimensional networks of karst conduits
The main idiosyncrasy of a typical karst system is the presence of a three-dimensional network of conduits behaving as drains in the system and being responsible of both the quick response of karst springs to rainfall events and the complex distribution of solutes in the system. A morphometric analysis of the three-dimensional geometry of conduits provides quantitative measures that can be used in a range of applications. These morphometric parameters can be used as descriptors of the underground geomorphology, they provide information on speleogenesis processes, they can be correlated with karst denudation ratios, they can be used to control the simulation of realistic stochastic karst networks of conduits, and they can be correlated with hydrogeologic behaviour of the karst system. The main purpose of this paper is to define, describe and illustrate a range of morphometric indexes and morphometric functions that can be calculated nowadays because the availability of three-dimensional topographies provided by speleological work and the availability of the computational and graphical power provided by modern computers. Some of the morphometric parameters describe the existence of preferential directions of karstification, others describe the kartification along the vertical and the possible presence of inception horizons. Other indexes describe the shape complexity of the karstic network, whilst other indexes describe spatial variability of the conduit geometry, and other parameters give account of the connectivity of the three-dimensional network. The morphometric analysis is illustrated with a three-dimensional karstic network in Southern France.
rose of directions, z-histograms, fractal dimension, semi-variogram of spatial density, connectivity index, sinuosity index
0169-555X
17-28
Pardo-Iguzquiza, Eulogio
0ef5d070-ab54-4d5e-8e8b-6268ba360e92
Durán-Valsero, Juan J.
42ac798a-aeda-439e-b85a-7e754504e055
Rodriguez-Galiano, Victor
be6ea36a-6613-41ba-a4da-9e7b565d8d0d
Pardo-Iguzquiza, Eulogio
0ef5d070-ab54-4d5e-8e8b-6268ba360e92
Durán-Valsero, Juan J.
42ac798a-aeda-439e-b85a-7e754504e055
Rodriguez-Galiano, Victor
be6ea36a-6613-41ba-a4da-9e7b565d8d0d

Pardo-Iguzquiza, Eulogio, Durán-Valsero, Juan J. and Rodriguez-Galiano, Victor (2011) Morphometric analysis of three-dimensional networks of karst conduits. Geomorphology, 132 (1-2), 17-28. (doi:10.1016/j.geomorph.2011.04.030).

Record type: Article

Abstract

The main idiosyncrasy of a typical karst system is the presence of a three-dimensional network of conduits behaving as drains in the system and being responsible of both the quick response of karst springs to rainfall events and the complex distribution of solutes in the system. A morphometric analysis of the three-dimensional geometry of conduits provides quantitative measures that can be used in a range of applications. These morphometric parameters can be used as descriptors of the underground geomorphology, they provide information on speleogenesis processes, they can be correlated with karst denudation ratios, they can be used to control the simulation of realistic stochastic karst networks of conduits, and they can be correlated with hydrogeologic behaviour of the karst system. The main purpose of this paper is to define, describe and illustrate a range of morphometric indexes and morphometric functions that can be calculated nowadays because the availability of three-dimensional topographies provided by speleological work and the availability of the computational and graphical power provided by modern computers. Some of the morphometric parameters describe the existence of preferential directions of karstification, others describe the kartification along the vertical and the possible presence of inception horizons. Other indexes describe the shape complexity of the karstic network, whilst other indexes describe spatial variability of the conduit geometry, and other parameters give account of the connectivity of the three-dimensional network. The morphometric analysis is illustrated with a three-dimensional karstic network in Southern France.

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More information

Published date: September 2011
Keywords: rose of directions, z-histograms, fractal dimension, semi-variogram of spatial density, connectivity index, sinuosity index
Organisations: Global Env Change & Earth Observation

Identifiers

Local EPrints ID: 360090
URI: http://eprints.soton.ac.uk/id/eprint/360090
ISSN: 0169-555X
PURE UUID: f1ea2885-b60b-4076-aafb-f4b0759a7b4c

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Date deposited: 25 Nov 2013 13:52
Last modified: 14 Mar 2024 15:33

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Contributors

Author: Eulogio Pardo-Iguzquiza
Author: Juan J. Durán-Valsero
Author: Victor Rodriguez-Galiano

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