Universal Spatial Correlation Functions for Describing and Reconstructing Soil Microstructure

被引:92
作者
Karsanina, Marina V. [1 ,2 ]
Gerke, Kirill M. [3 ]
Skvortsova, Elena B. [4 ]
Mallants, Dirk [3 ]
机构
[1] Russian Acad Sci, Inst Geospheres Dynam, Moscow, Russia
[2] AIR Technol, Moscow, Russia
[3] CSIRO Land & Water, Adelaide, SA, Australia
[4] Russian Acad Sci, Dokuchaev Soil Sci Inst, Moscow, Russia
基金
俄罗斯科学基金会;
关键词
UNSATURATED HYDRAULIC CONDUCTIVITY; STOCHASTIC RECONSTRUCTION; SOLUTE TRANSPORT; POROUS-MEDIA; PORE-SPACE; PERMEABILITY; POROSITY; SIMULATION; SANDSTONE; MODELS;
D O I
10.1371/journal.pone.0126515
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Structural features of porous materials such as soil define the majority of its physical properties, including water infiltration and redistribution, multi-phase flow (e.g. simultaneous water/air flow, or gas exchange between biologically active soil root zone and atmosphere) and solute transport. To characterize soil microstructure, conventional soil science uses such metrics as pore size and pore-size distributions and thin section-derived morphological indicators. However, these descriptors provide only limited amount of information about the complex arrangement of soil structure and have limited capability to reconstruct structural features or predict physical properties. We introduce three different spatial correlation functions as a comprehensive tool to characterize soil microstructure: 1) two-point probability functions, 2) linear functions, and 3) two-point cluster functions. This novel approach was tested on thin-sections (2.21x2.21 cm(2)) representing eight soils with different pore space configurations. The two-point probability and linear correlation functions were subsequently used as a part of simulated annealing optimization procedures to reconstruct soil structure. Comparison of original and reconstructed images was based on morphological characteristics, cluster correlation functions, total number of pores and pore-size distribution. Results showed excellent agreement for soils with isolated pores, but relatively poor correspondence for soils exhibiting dual-porosity features (i.e. superposition of pores and microcracks). Insufficient information content in the correlation function sets used for reconstruction may have contributed to the observed discrepancies. Improved reconstructions may be obtained by adding cluster and other correlation functions into reconstruction sets. Correlation functions and the associated stochastic reconstruction algorithms introduced here are universally applicable in soil science, such as for soil classification, pore-scale modelling of soil properties, soil degradation monitoring, and description of spatial dynamics of soil microbial activity.
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页数:26
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