Abstract

A total of 89 legacy soil organic matter (SOM) data (0–20 cm) sourced from the soil survey in 1980 in Hailun County of Northeastern China and 268 SOM data (0–20 cm) measured in the area in 2008 were collected in this study. The most straightforward mapping methods such as ordinary kriging (OK), inverse distance weighting interpolation (IDW), and the soil type-based method (ST) were used to derive the spatial patterns of changes in SOM; and the uncertainties associated with the mapping methods were quantitatively assessed through the uncertainty intervals of SOM realizations that were generated by sequential Gaussian simulation and/or Monte Carlo simulation. Results showed that the overall trend of changes in SOM over the last 28 years in the area decreased. The spatial patterns of changes in SOM derived by OK2008–OK1980 (abbreviations before and after the dash represent the mapping method for SOM data in 2008 and 1980, respectively) and IDW2008–OK1980, OK2008–IDW1980 and IDW2008–IDW1980, OK2008–ST1980 and IDW2008–ST1980 are similar. The change map obtained by the ST2008–ST1980 method is also similar to those derived by OK2008–ST1980 and IDW2008–ST1980 methods, but local details of changes in SOM presented by the ST2008–ST1980 method are coarser than those obtained by the OK2008–ST1980 and IDW2008–ST1980 methods. The OK2008–ST1980 method, with an uncertainty tradeoff compared to the OK2008–OK1980 and ST2008–ST1980 methods, can be considered as the most suitable method for mapping changes in SOM in the area due to the limited legacy soil survey data and inaccurate sample location information records in the area.

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