Spatial modelling of soil hydraulic properties integrating different supports

被引:4
|
作者
Horta, Ana [1 ]
Pereira, Maria Joao [2 ]
Goncalves, Maria [3 ]
Ramos, Tiago [4 ]
Soares, Amilcar [2 ]
机构
[1] Univ Sydney, Fac Agr & Environm, Sydney, NSW 2006, Australia
[2] Univ Tecn Lisboa, Inst Super Tecn, Ctr Nat Resources & Environm, P-1049001 Lisbon, Portugal
[3] Inst Nacl Recursos Biol, INIA, Estacao Agron Nacl, P-2784505 Oeiras, Portugal
[4] Univ Tecn Lisboa, Inst Agron, CEER Biosyst Engn, P-1349017 Lisbon, Portugal
关键词
Geostatistics; Soil hydraulic properties; Data integration; Block simulation; Uncertainty; PEDOTRANSFER FUNCTIONS; SIMULATION; STATE; SITE;
D O I
10.1016/j.jhydrol.2014.01.027
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Modelling soil-water interactions provides important outputs for agriculture management and environmental monitoring. Most of the existing models rely on soil hydraulic properties (SHP) as input data. Geostatistical approaches based on stochastic simulations provide the spatial distribution of SHP and the uncertainty attached to their estimates. Frequently, SHP are measured in different data supports thus one needs to guarantee the integration of these different supports to provide a coherent and reliable model. One possible solution is to use block sequential simulation (Liu and Journel, 2009). Our work presents an application of this algorithm to map and quantify the spatial uncertainty of total porosity. Based on the simulation outputs and on the comparison with direct sequential simulation that does not account for the multiple supports of the data, we concluded that block sequential simulation should be used to produce reliable input data to dynamic soil-water models. (c) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:1 / 9
页数:9
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