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State-space approach to evaluate effects of land levelling on the spatial relationships of soil properties of a lowland area

机译:评估土地平整对低地土壤特性空间关系影响的状态空间方法

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Land levelling is an agricultural practice to correct soil surface irregularities turning the area more efficient for management of agronomic inputs. The technique has been adopted mainly in lowland areas used for flood irrigation of rice. As a result sub-surface soil layers may be exposed with possible impact on crop production by changing soil properties. This study aimed to evaluate the effects of land levelling on the spatial relationships of soil properties. Relations among them were quantified using a state-space approach in different scenarios constructed from data sets in a 1 ha lowland area sampled as a grid. The grid consisted of 100 sampling points (10 m x 10 m), with samples collected from the 0-0.20 m soil layer, before and after levelling, totalizing 200 samples. Soil water contents at field capacity (theta(FC)) and permanent wilting point (theta(PWP)) were taken as response variables due to their importance on rice water management. Sand, silt and clay contents, soil microporosity (Micro) and bulk density (BD), cation exchange capacity (CEC), organic carbon content (Corg), and the depth of the top of the B horizon in relation to soil surface (DTB) were used as co-variables through an evaluation of their spatial auto- and cross-correlation behaviors with theta(FC) and theta(PWP). Eight data-array scenarios were tested. Results showed that levelling induced negative effects on soil quality since this procedure decreased theta(FC) and theta(PWP), Corg, and CEC as well as increased BD. Using the state-space approach, we concluded that its performance in estimating theta(FC) and theta(PWP) was affected by the scenarios after levelling, the best performance being for the vertical scenarios. DTB and CEC contributed to the estimation of both soil water contents for all scenarios after levelling. The main problem associated to the levelling is the cutting of shallow soils which decreases their capacity to store water and to exchange cations in the effective arable depth which will be explored by the crop root system. As DTB is directly related to the spatial distribution of taxonomic soil profile properties, the state-space approach, which considers sampling location coordinates, may be a potential on-site-specific tool aiming at the recuperation of degraded soils through amendments since it opens the possibility for farmers to manage a crop field based on local environmental properties, with their spatial association and localized variation being a function of the distance between their measurements. (C) 2014 Elsevier B.V. All rights reserved.
机译:土地平整是一种农业实践,可以纠正土壤表面的不规则性,从而使该地区更有效地管理农业投入物。该技术已主要用于水稻洪水灌溉的低地地区。结果,地下土壤层可能会通过改变土壤特性而暴露于土壤,对作物生产可能产生影响。这项研究旨在评估土地平整对土壤特性空间关系的影响。它们之间的关系在不同的场景中使用状态空间方法进行了量化,这些场景是从1公顷低地区域(以网格形式采样)中的数据集构建而成的。网格由100个采样点(10 m x 10 m)组成,在平整之前和之后从0-0.20 m的土壤层收集了样本,总共有200个样本。由于田间持水量(theta(FC))和永久枯萎点(theta(PWP))的土壤水分含量对稻米水分管理的重要性,因此将其作为响应变量。沙子,淤泥和粘土含量,土壤微孔率(Micro)和堆积密度(BD),阳离子交换容量(CEC),有机碳含量(Corg)以及相对于土壤表面的B层顶部的深度(DTB) )通过评估其与theta(FC)和theta(PWP)的空间自相关和互相关行为而用作协变量。测试了八个数据阵列方案。结果表明,流平对土壤质量产生负面影响,因为此过程降低了theta(FC)和theta(PWP),Corg和CEC以及BD的增加。使用状态空间方法,我们得出的结论是,平均化后的方案会影响其估算theta(FC)和theta(PWP)的性能,最佳性能是针对垂直方案。找平后,DTB和CEC有助于估算所有情况下的两种土壤含水量。与平整有关的主要问题是切割浅层土壤,这会降低其在有效耕种深度中的蓄水能力和交换阳离子的能力,这将由作物根系进行探索。由于DTB与分类土壤剖面特性的空间分布直接相关,因此考虑采样位置坐标的状态空间方法可能是针对现场潜在的特定工具,旨在通过修订来恢复退化土壤,因为它开放了农民有可能根据当地的环境特性来管理农田,他们的空间关联和局部变化是他们测量之间距离的函数。 (C)2014 Elsevier B.V.保留所有权利。

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