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Comparison of Density and Water Content Determinations Using Soil Cores and a Dual Probe Density Gauge

机译:土壤芯密度和水含量测定的比较及双探针密度计

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Wet bulk density and water content were determined with the standard soil-core method and by using a density and moisture gauge (gamma radiation and fast neutrons). Four soils collected at different forest sites were tested in the laboratory under different degrees of compression and at various water contents. Using the count ratios of the gauge for density and water as independent variables and wet bulk density and water content determined by soil cores as dependent variables, calibration equations were developed. For the soils used, the gauge values concerning wet bulk density were in close agreement with values determined with soil cores. However, the water content readings of the gauge had to be recalculated using the equations developed. The equations were tested on soil cores collected in the field after measurements with the gauge. The dry bulk density calculated as the wet bulk density given by the gauge minus the water content recalculated using the presented equations differed by an average of -1.6 percent from the soil-core values.
机译:用标准土芯法测定湿堆积密度和水含量,并使用密度和水分计(伽马辐射和快节奏)。在不同森林地点收集的四种土壤在实验室在不同程度的压缩和各种水含量下进行测试。使用规格的计数比为密度和水作为独立变量和湿堆积密度和土壤核心确定的水含量作为依赖变量,开发了校准方程。对于所用的土壤,有关湿堆积密度的规格值与土壤核心确定的值密切一致。然而,必须使用开发的方程来重新计算测量仪的水含量读数。在用仪表测量后,在田间收集的土芯上测试了方程。根据测量仪减去使用所示方程克重新计算的水含量的湿堆积密度计算的干堆积密度与土壤核心值的平均值为-1.6%。

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