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Measuring carbon dynamics in field soils using soil spectral reflectance: prediction of maize root density, soil organic carbon and nitrogen content

机译:利用土壤光谱反射率测量田间土壤中的碳动态:预测玉米根系密度,土壤有机碳和氮含量

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This paper reports the development of a proximal sensing technique used to predict maize root density, soil carbon (C) and nitrogen (N) content from the visible and near-infrared (Vis-NIR) spectral reflectance of soil cores. Eighteen soil cores (0-60 cm depth with a 4.6 cm diameter) were collected from two sites within a field of 90-day-old maize silage; Kairanga silt loam and Kairanga fine sandy loam (Gley Soils). At each site, three replicate soil cores were taken at 0, 15 and 30 cm distance from the row of maize plants (rows were 60 cm apart). Each soil core was sectioned at 5 depths (7.5, 15, 30, 45, and 60 cm) and soil reflectance spectra were acquired from the freshly cut surface at each depth. A 1.5 cm soil slice was taken at each surface to obtain root mass and total soil C and N reference (measured) data. Root densities decreased with depth and distance from plant and were lower in the silt loam, which had the higher total C and N contents. Calibration models, developed using partial least squares regression (PLSR) between the first derivative of soil reflectance and the reference data, were able to predict with moderate accuracy the soil profile root density (r po = 0.75; ratio of prediction to deviation [RPD] = 2.03; root mean square error of cross-validation [RMSECV] = 1.68 mg/cmpd), soil% C (r po = 0.86; RPD = 2.66; RMSECV = 0.48%) and soil% N (r po = 0.81; RPD = 2.32; RMSECV = 0.05%) distribution patterns. The important wavelengths chosen by the PLSR model to predict root density were different to those chosen to predict soil C or N. In addition, predicted root densities were not strongly autocorrelated to soil C (r = 0.60) or N (r = 0.53) values, indicating that root density can be predicted independently from soil C. This research has identified a potential method for assessing root densities in field soils enabling study of their role in soil organic matter synthesis.
机译:本文报道了一种近端传感技术的发展,该技术用于根据土壤核心的可见和近红外(Vis-NIR)光谱反射率来预测玉米根系密度,土壤碳(C)和氮(N)的含量。在90天龄的玉米青贮田中,从两个地点收集了18个土壤核心(0-60厘米深,直径4.6厘米直径)。 Kairanga粉质壤土和Kairanga细砂质壤土(Gley土壤)。在每个地点,在距玉米行0、15和30 cm处(行距相距60 cm)处分别取三个重复的土壤核心。将每个土壤芯切成5个深度(7.5、15、30、45和60 cm),并从每个深度的新切面中获取土壤反射光谱。在每个表面上取一个1.5厘米的土壤切片,以获取根质量以及土壤总C和N参考(测得)数据。根系密度随着距植物的深度和距离的增加而降低,而在粉壤土中较低,其总碳和氮含量较高。使用土壤反射率的一阶导数和参考数据之间的偏最小二乘回归(PLSR)开发的校准模型,能够以中等准确度预测土壤剖面根部密度(r po = 0.75;预测与偏差之比[RPD] = 2.03;交叉验证的均方根误差[RMSECV] = 1.68 mg / cmpd),土壤%C(r po = 0.86; RPD = 2.66; RMSECV = 0.48%)和土壤%N(r po = 0.81; RPD = 2.32; RMSECV = 0.05%)分布模式。 PLSR模型选择的用于预测根系密度的重要波长与预测土壤的C或N所选择的重要波长不同。此外,预测的根系密度与土壤C(r = 0.60)或N(r = 0.53)值之间不具有很强的自相关性。 ,表明可以独立于土壤C预测根系密度。这项研究发现了一种评估田间土壤根系密度的潜在方法,从而能够研究其在土壤有机质合成中的作用。

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