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首页> 外文期刊>Soil Science >Variation in the precision of soil organic carbon maps due to different laboratory and spatial prediction methods.
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Variation in the precision of soil organic carbon maps due to different laboratory and spatial prediction methods.

机译:由于不同的实验室和空间预测方法,土壤有机碳图的精度会发生变化。

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Digital mapping of soil organic carbon (SOC) is important for site-specific crop management and for environmental modelling and planning. Our objective was to evaluate how the precision of SOC maps is affected by the laboratory method used for measuring SOC and by the spatial prediction method used for mapping. In two irrigated maize fields in Nebraska, soil samples were collected, and SOC was either determined directly by automated CN analyzer (reference method, SOCC) or estimated from weight loss-on-ignition (LOI) as a cheaper alternative. The latter involved conversion of LOI to soil organic matter (SOM) content using a standard laboratory calibration, followed by converting SOM to SOC values by assuming a constant C mass fraction in SOM (estimates denoted as SOCL) or by regressing SOC on LOI (denoted as SOCR). Interpolation methods evaluated were ordinary kriging (OK) and regression kriging (RK). Exhaustive ancillary variables used in RK included relative elevation, slope, soil electrical conductivity, and remotely sensed soil surface reflectance. Soil organic C was correlated with most of these ancillary variables, but the magnitudes of correlation varied among locations. Direct measurement of SOCC in combination with RK as spatial prediction method resulted in the most precise SOC maps. The relative improvement in map precision was 15% in Field 1 and 6% in Field 2 over OK of SOCC. Maps of SOC derived from LOI estimates were biased and less precise than maps that were based on direct measurement of SOC, but utilizing secondary information for spatial prediction alleviated some of the loss in precision. Using SOCL or SOCR estimates of SOC decreased map precision by 10% to 14% in OK or by 7% to 10% with RK as compared to the SOCC method. Regardless of the laboratory method chosen, secondary information should be used in SOC mapping to reduce sampling cost and/or increase map precision. However, the relative improvement of hybrid geostatistical techniques over OK largely depends on the strength of the correlation between SOC and ancillary variables..
机译:土壤有机碳(SOC)的数字绘图对于特定地点的作物管理以及环境建模和规划非常重要。我们的目标是评估用于测量SOC的实验室方法和用于映射的空间预测方法如何对SOC地图的精度产生影响。在内布拉斯加州的两个灌溉玉米田中,收集土壤样品,或者通过自动CN分析仪(参考方法,SOCC)直接确定SOC,或者从点火失重(LOI)估算出SOC,以作为更便宜的选择。后者涉及使用标准实验室校准将LOI转换为土壤有机物(SOM)含量,然后通过假设SOM中C的质量分数恒定(将其表示为SOCL)或通过将LOI上的SOC回归(表示为SOC),将SOM转换为SOC值。作为SOCR)。评估的插值方法为普通克里金法(OK)和回归克里金法(RK)。 RK中使用的详尽的辅助变量包括相对海拔,坡度,土壤电导率和遥感土壤表面反射率。土壤有机碳与大多数这些辅助变量相关,但相关程度因位置而异。与RK作为空间预测方法结合使用SOCC的直接测量可得出最精确的SOC映射。与SOCC的OK相比,地图精度在字段1中的相对提高为15%,在字段2中为6%。与基于直接测量SOC的图相比,从LOI估计得出的SOC的图有偏差且不那么精确,但是利用辅助信息进行空间预测可以减轻一些精度损失。与SOCC方法相比,使用SOCL或SOCR估计的SOC可以使地图精度(正常情况下)降低10%至14%,而使用RK则降低7%至10%。无论选择哪种实验室方法,都应在SOC映射中使用辅助信息以降低采样成本和/或提高映射精度。但是,混合地统计学技术相对于OK的相对改进在很大程度上取决于SOC和辅助变量之间的相关强度。

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