Application of generalized linear geostatistical model for regional soil organic matter mapping: The effect of sampling density

被引:9
作者
Zhang, Mei-Wei [1 ]
Hao, Chenkai [1 ]
Wang, Xiaoqing [1 ]
Sun, Xiao-Lin [1 ,2 ,3 ]
机构
[1] Sun Yat Sen Univ, Sch Geog & Planning, Guangzhou 510275, Peoples R China
[2] Guangxi Univ, Coll Agr, Guangxi Key Lab Agro Environm & Agro Prod Safety, Nanning 530004, Peoples R China
[3] Sun Yat Sen Univ, Rm 302,572 Bldg,135 Xingang West Rd, Guangzhou 510275, Peoples R China
关键词
Digital soil mapping; Pedometrics; Generalized linear geostatistical model; Sampling density; SPATIAL PREDICTION; REGRESSION; SCALE; PROPAGATION;
D O I
10.1016/j.geoderma.2023.116446
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The generalized linear geostatistical model (GLGM) is a formal approach of regression kriging that would be advantageous over commonly used modelling approaches for digital soil mapping (DSM). However, it has not been well explored in the literature, due to heavy computation. This study evaluates such formal approach for mapping soil organic matter at a regional scale (179,700 km2). We hypothesized that GLGM would be a better approach than other approaches as it can model nonlinear relationships and spatially consider the residuals. However, the accuracy would depend on sampling density. We compared GLGM with multiple linear regression (MLR), ordinary kriging (OK), regression kriging (RK), random forest (RF), generalized linear mixture model (GLMM), and generalized additive model (GAM). The effect of sampling density on the performance was also investigated by fitting the models based on resampling the samples with a series of sizes ranging from 100 to 1200. Results showed that GLGM generally improved the accuracy of DSM, compared with MLR, OK, RF, GLMM, and GAM, especially for large sample sizes, although the improvement was not significant. In a few cases, GLGM outperformed RK. The GLGM modelling and its prediction were largely influenced by sampling densities. Given small sample sizes, GLGM was unstable and the parameters were highly variable depending on the modelling realizations. Other influencing factors include linear and smooth correlations between soil and environmental covariates, spatial autocorrelation of the residuals, compatibility of spatial scales of soil samples and environ-mental covariates, and the scale of soil variation. For these factors, researchers with a more dense soil sampling are needed in future to explore the benefits of GLGM as a hybrid model for spatial prediction of soil.
引用
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页数:10
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