利用外漂移遥感和克里格法改进稀疏的近端土壤传感数据并确定精准农业管理区

H. Rodrigues, M. B. Ceddia, G. Vasques, Vera L. Mulder, G. Heuvelink, Ronaldo P. Oliveira, Z. Brandão, J. P. S. Morais, Matheus L. Neves, Sílvio R. L. Tavares
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引用次数: 0

摘要

精准农业科学领域采用越来越多的创新技术来优化投入,最大化盈利能力,减少对环境的影响。因此,获得大量的土壤样本使精准农业可行是具有挑战性的。这一数据瓶颈已通过通过近端土壤传感设备获得的数据来确定子区域来克服。这些数据可以与免费提供的遥感数据相结合,以创建更准确的土壤属性地图。此外,这些地图可以通过管理区域最佳地汇总和解释土壤异质性。因此,本工作旨在从近端土壤遥感和遥感数据中创建和结合土壤管理区。为此,使用EM38-MK2近端土壤传感器测量了电导率和磁化率数据,并通过Medusa MS1200近端土壤传感器测量了巴西圣保罗72公顷粮食产区的钍和铀元素含量,两者都相当。使用普通克里格(OK)绘制近端土壤感知属性。地图的制作还使用了kriging外部偏移(KED)和近端土壤传感器属性数据,结合遥感数据,如Landsat-8、Aster和Sentinel-2图像,以及来自数字高程模型Alos Palsar的10个地形辅助变量。结果,通过k-means聚类算法生成了三个管理区域地图:使用近端传感器(OK)、近端传感器与远程传感器(KED)结合的数据,以及远程传感器的数据。在实验室中收集并分析了72个样本(深度为0-10厘米)(每公顷1个样本)的粘土、钙、有机碳和镁的浓度,以评估使用方差分析创建的管理区地图的能力。使用三个数据组创建的所有区域都可以区分不同的治疗区域。用于绘制管理区域地图的三种数据源产生了相似的地图区域,但使用近端和远程数据组合的区域地图在定义管理区域方面没有显示出改进,并且与OK和KED地图相比,仅使用遥感数据降低了区分每个区域的显著性水平。总之,本研究不仅强调了近端和遥感技术在精准农业中的全球适用性,而且揭示了它们整合的细微差别。这项研究的发现肯定了这些先进技术在解决土壤异质性带来的挑战方面的有效性,为全球范围内更细致和具体的农业实践铺平了道路。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Remote Sensing and Kriging with External Drift to Improve Sparse Proximal Soil Sensing Data and Define Management Zones in Precision Agriculture
The precision agriculture scientific field employs increasingly innovative techniques to optimize inputs, maximize profitability, and reduce environmental impacts. Therefore, obtaining a high number of soil samples to make precision agriculture feasible is challenging. This data bottleneck has been overcome by identifying sub-regions based on data obtained through proximal soil sensing equipment. These data can be combined with freely available remote sensing data to create more accurate maps of soil properties. Furthermore, these maps can be optimally aggregated and interpreted for soil heterogeneity through management zones. Thus, this work aimed to create and combine soil management zones from proximal soil sensing and remote sensing data. To this end, data on electrical conductivity and magnetic susceptibility, both apparent, were measured using the EM38-MK2 proximal soil sensor and the contents of the thorium and uranium elements, both equivalent, via the Medusa MS1200 proximal soil sensor for a 72-ha grain-producing area in São Paulo, Brazil. The proximal soil sensing attributes were mapped using ordinary kriging (OK). Maps were also made using kriging with external drift (KED), and the proximal soil sensor attributes data, combined with remote sensing data, such as Landsat-8, Aster, and Sentinel-2 images, in addition to 10 terrain covariables derived from the digital elevation model Alos Palsar. As a result, three management zone maps were produced via the k-means clustering algorithm: using data from proximal sensors (OK), proximal sensors combined with remote sensors (KED), and remote sensors. Seventy-two samples (0–10 cm in depth) were collected and analyzed in a laboratory (1 sample per hectare) for concentrations of clay, calcium, organic carbon, and magnesium to assess the capacity of the management zone maps created using analysis of variance. All zones created using the three data groups could distinguish the different treatment areas. The three data sources used to map management zones produced similar map zones, but the zone map using a combination of proximal and remote data did not show an improvement in defining the management zones, and using only remote sensing data lowered the significance levels of differentiating each zone compared to the OK and KED maps. In summary, this study not only underscores the global applicability of proximal and remote sensing techniques in precision agriculture but also sheds light on the nuances of their integration. The study’s findings affirm the efficacy of these advanced technologies in addressing the challenges posed by soil heterogeneity, paving the way for more nuanced and site-specific agricultural practices worldwide.
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