Spatial prediction of topsoil salinity in the Chelif Valley, Algeria, using local ordinary kriging with local variograms versus whole-area variogram

被引:71
作者
Walter, C [1 ]
McBratney, AB
Douaoui, A
Minasny, B
机构
[1] INRA Rennes, ENSA, Soil Sci Lab, F-35042 Rennes, France
[2] Univ Sydney, Dept Agr Chem & Soil Sci, Sydney, NSW 2006, Australia
[3] Univ Chlef, Inst Agron, Chlef, Algeria
来源
AUSTRALIAN JOURNAL OF SOIL RESEARCH | 2001年 / 39卷 / 02期
关键词
soil salinity; spatial analysis; semivariogram;
D O I
10.1071/SR99114
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
A novel form of ordinary kriging, involving the local estimation and modelling of the variogram at each prediction site (OKLV), is tested at a regional scale on a large data set, in order to adapt to non-uniform spatial structures and improve the assessment of the salinity hazard in the lower Chelif Valley, Algeria. The spatial variability study was carried out on a 38000 ha area using 5141 topsoil electrical conductivity (EC) measurements systematically sampled on a 250 m by 250 m grid. Variography analysis confirmed the existence of large trends in the EC variability with differing spatial structures between sub-areas. OKLV performed better than ordinary kriging with a whole-area variogram (OKWV) in predicting the proportion of high saline soils in large blocks, but the predictions appeared mostly similar. In contrast, the estimation variance maps revealing the uncertainties of the spatial predictions were markedly different between the 2 methods. OKLV integrates the local spatial structure in the uncertainty assessment, whereas kriging with a whole-area variogram only considers the sampling intensity. Comparison with prediction errors on a validation set confirmed the consistency of the OKLV prediction variance. This appears to be a major improvement for decision-making procedures such as delineating areas where remediation should take place.
引用
收藏
页码:259 / 272
页数:14
相关论文
共 28 条
  • [11] HAJRASULIHA S, 1980, IRRIGATION SCI, V1, P197, DOI 10.1007/BF00277625
  • [12] HOSSEINI E, 1994, T ASAE, V37, P1799, DOI 10.13031/2013.28269
  • [13] Isaaks EH., 1989, Applied Geostatistics
  • [14] Isbell R. F., 1983, Soils: an Australian viewpoint., P107
  • [15] MCBRATNEY AB, 1996, P 3 INT C PREC AGR B, P331
  • [16] Status and trends of soil salinity at different scales: the case for the irrigated cotton growing region of eastern Australia
    Odeh, IOA
    Todd, AJ
    Triantafilis, J
    McBratney, AB
    [J]. NUTRIENT CYCLING IN AGROECOSYSTEMS, 1998, 50 (1-3) : 99 - 107
  • [17] Oliver M. A., 1990, International Journal of Geographical Information Systems, V4, P313, DOI 10.1080/02693799008941549
  • [18] Perspectives on desertification: western Mediterranean
    Puigdefabregas, J
    Mendizabal, T
    [J]. JOURNAL OF ARID ENVIRONMENTS, 1998, 39 (02) : 209 - 224
  • [19] ELECTRICAL-CONDUCTIVITY METHODS FOR MEASURING AND MAPPING SOIL-SALINITY
    RHOADES, JD
    [J]. ADVANCES IN AGRONOMY, VOL 49, 1993, 49 : 201 - 251
  • [20] Saidi D., 1999, ETUDE GEST SOLS, V6, P15