Improved Stock Unearthing Method (ISUM) as a tool to determine the value of alternative topographic factors in estimating inter-row soil mobilisation in citrus orchards
J. Rodrigo‐Comino, Alexandre Marco da Silva, E. Moradi, E. Terol, A. Cerdà
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引用次数: 5
Abstract
The Improved Stock Unearthing Method (ISUM) was initially designed to assess soil mobilisation rates in vineyards; however, other grafted crops such as citrus orchards could also be successfully used. The results obtained from ISUM have been used for several goals, but have not yet been applied for computing the LS factor (length and slope) as a part of the Universal Soil Loss Equation (USLE), which could give useful information to improve soil management system plans. This investigation was conducted in an 8-year old clementine field located in Canals (Valencia, Spain) and values of the LS factor were calculated by means of two pre-established algorithms, which allowed us to calculate a Transect Length Index (TLI). Our results demonstrated that the micro-topographical changes can show frequent irregularities. For the values of the Transect Length Index (TLI), the mean values were 1.02% for the left side and 1.04% for the right one. The difference among the areas predicted at the moment of furrow construction and the moment of data survey permitted us to estimate a total volume of 56.9 m3 of soil mobilized in 19 years. Taking into account the studied area (360 m2), the volume of mobilised soil, and the bulk density for the local soil (1.3 g cm-3), we estimated a total soil mobilisation of 8.3 mm yr-1 or 10.4 kg m-2 yr-1. We did not observe any evidence or indicator of rill and inter-rill erosion by natural rainfall events, suggesting that the runoff homogenizes the sediment distribution during heavy rains (corroborated by the TLI data) or tillage practices. The data created following the ISUM was suitable to be used to calculate the LS-factor values. The amount of soil mobilised as predicted by USLE was always lower than the ones predicted by ISUM.
改良库存发掘法(ISUM)最初旨在评估葡萄园的土壤动员率;然而,柑橘园等其他嫁接作物也可以成功使用。ISUM获得的结果已用于多个目标,但尚未作为通用土壤损失方程(USLE)的一部分用于计算LS因子(长度和坡度),该方程可为改进土壤管理系统计划提供有用信息。这项调查是在位于Canals(西班牙巴伦西亚)的一块8年前的克莱门汀田中进行的,LS因子的值是通过两种预先建立的算法计算的,这使我们能够计算横断面长度指数(TLI)。我们的研究结果表明,微观地形变化可以显示出频繁的不规则性。对于横断面长度指数(TLI)的值,左侧和右侧的平均值分别为1.02%和1.04%。犁沟施工时和数据调查时预测的面积之间的差异使我们能够估计19年内动员的土壤总量为56.9 m3。考虑到研究面积(360 m2)、活动土壤的体积和当地土壤的堆积密度(1.3 g cm-3),我们估计总土壤活动量为8.3 mm yr-1或10.4 kg m-2 yr-1。我们没有观察到任何自然降雨事件造成细沟和细沟间侵蚀的证据或指标,这表明径流使暴雨期间的沉积物分布均匀化(TLI数据证实了这一点)或耕作实践。ISUM之后创建的数据适合用于计算LS系数值。USLE预测的土壤动员量总是低于ISUM预测的土壤。
期刊介绍:
The Spanish Journal of Soil Science (SJSS) is a peer-reviewed journal with open access for the publication of Soil Science research, which is published every four months. This publication welcomes works from all parts of the world and different geographic areas. It aims to publish original, innovative, and high-quality scientific papers related to field and laboratory research on all basic and applied aspects of Soil Science. The journal is also interested in interdisciplinary studies linked to soil research, short communications presenting new findings and applications, and invited state of art reviews. The journal focuses on all the different areas of Soil Science represented by the Spanish Society of Soil Science: soil genesis, morphology and micromorphology, physics, chemistry, biology, mineralogy, biochemistry and its functions, classification, survey, and soil information systems; soil fertility and plant nutrition, hydrology and geomorphology; soil evaluation and land use planning; soil protection and conservation; soil degradation and remediation; soil quality; soil-plant relationships; soils and land use change; sustainability of ecosystems; soils and environmental quality; methods of soil analysis; pedometrics; new techniques and soil education. Other fields with growing interest include: digital soil mapping, soil nanotechnology, the modelling of biological and biochemical processes, mechanisms and processes responsible for the mobilization and immobilization of nutrients, organic matter stabilization, biogeochemical nutrient cycles, the influence of climatic change on soil processes and soil-plant relationships, carbon sequestration, and the role of soils in climatic change and ecological and environmental processes.