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Estimating soil organic matter using interpolation methods with a electromagnetic induction sensor and topographic parameters: a case study in a humid region

机译:用电磁感应传感器的插值方法估算土壤有机物及地形参数:潮湿区域的案例研究

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Soil organic matter (SOM) is a key indicator of soil quality although, usually, detailed data for a given area is difficult to obtain at low cost. This study was conducted to evaluate the usefulness of soil apparent electrical conductivity (ECa), measured with an electromagnetic induction sensor, to improve the spatial estimation of SOM for site-specific soil management purposes. Apparent electrical conductivity was measured in a 10-ha prairie in NW Spain in November 2011. The ECa measurements were used to design a sampling scheme of 80 locations, at which soil samples were collected from 0 to 20 cm depth and from 20 cm to the boundary of the A horizon (ranging from 25 to 48 cm). The SOM values determined at the two depths considered were weighted to obtain the results for the entire A Horizon. SOM distribution maps were obtained by inverse distance weighting and geostatistical techniques: ordinary kriging (OK), cokriging (COK), regression kriging either with linear models (LM-RK) or with random forest (RF-RK). SOM ranged from 46.3 to 78.0 g kg(-1), whereas ECa varied from 6.7 to 14.7 mS m(-1). These two variables were significantly correlated (r = -0.6, p < 0.05); hence, ECa was used as an ancillary variable for interpolating SOM. A strong spatial dependence was found for both SOM and ECa. The maps obtained exhibited a similar spatial pattern for SOM; COK maps did not show a significant improvement from OK predictions. However, RF-RK maps provided more accurate spatial estimates of SOM (error of predictions was between four and five times less than the other interpolators). This information is helpful for site-specific management purposes at this field.
机译:土壤有机物(SOM)是土壤质量的关键指标,但通常,难以以低成本获得给定区域的详细数据。进行该研究以评估用电磁感应传感器测量的土壤表观电导率(ECA)的有用性,以改善针对特定现场土壤管理目的的SOM的空间估计。在2011年11月的NW Spain的10-HA Prairie中测量了表观电导率。ECA测量用于设计80个位置的采样方案,其中将土壤样品从0到20cm深度收集和20厘米到20厘米地平线的边界(范围从25到48厘米)。在考虑的两个深度确定的SOM值被加权以获得整个地平线的结果。通过逆距离加权和地质统计技术获得SOM分布图:普通克里格汀(OK),Cokriging(Cok),回归克里格与线性模型(LM-RK)或随机森林(RF-RK)。 SOM的范围从46.3到78.0g kg(-1),而ECA从6.7变化到14.7 ms m(-1)。这两个变量显着相关(r = -0.6,p <0.05);因此,ECA被用作插值SOM的辅助变量。 SOM和ECA都发现了强烈的空间依赖。所获得的地图表现出类似的SOM的空间模式; COK地图没有从OK预测中显示出显着的改进。然而,RF-RK地图提供了更多精确的SOM空间估计(预测误差在4到五倍之间比其他内插器少4之间)。此信息对此字段的特定于网站的管理目的有帮助。

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