首页> 外文期刊>Land Degradation and Development >SPATIAL DISTRIBUTION OF SURFACE SOIL ACIDITY, ELECTRICAL CONDUCTIVITY, SOIL ORGANIC CARBON CONTENT AND EXCHANGEABLE POTASSIUM, CALCIUM AND MAGNESIUM IN SOME CROPPED ACID SOILS OF INDIA
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SPATIAL DISTRIBUTION OF SURFACE SOIL ACIDITY, ELECTRICAL CONDUCTIVITY, SOIL ORGANIC CARBON CONTENT AND EXCHANGEABLE POTASSIUM, CALCIUM AND MAGNESIUM IN SOME CROPPED ACID SOILS OF INDIA

机译:印度某些种植的酸性土壤中表面土壤酸度,电导率,土壤有机碳含量和可交换钾,钙和镁的空间分布

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摘要

Land degradation is a global problem. Best management of degraded land can be done by evaluating the spatial variability of soil properties including chemical properties of degraded land and mapping such variations. Since, a significant portion of arable land in India is chemically degraded due to soil acidity; the present study was conducted to study the spatial variability of soil acidity (pH), electrical conductivity (EC), soil organic carbon (OC) content, exchangeable potassium (K+), calcium (Ca2+) and magnesium (Mg2+) contents in some cropped acid soils of India. A total of four hundred (one hundred from each series) representative surface (0-0.15m depth) soil samples were collected from arable soils representing four soil series namely Hariharapur, Debatoli, Rajpora and Neeleswaram situated in Orissa, Jharkhand, Himachal Pradesh and Kerala states of India, respectively, and were analyzed. Soil acidity (pH between 3.90 and 6.45) showed a low variability, in contrast to other soil properties, which showed moderate variability. The coefficients of variation varied from 32.4 to 74.3, 31.2 to 50.9, 45.6 to 100, 71.9 to 93.0 and 59.0 to 79.8% for EC (mean between 0.05 and 0.09dSm(-1)), OC (mean between 0.29 to 1.86%), exchangeable K+ (mean between 39.1 and 77.7mgkg(-1)), Ca2+ (mean between 148 and 293mgkg(-1)) and Mg2+ (mean between 111 and 191mgkg(-1)), respectively. Soil pH and OC content were positively and significantly correlated with exchangeable K+, Ca2+ and Mg2+ content. Geostatistical analysis revealed that the best fit models were gaussian, exponential and spherical for different soil properties with moderate to strong spatial dependency. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:土地退化是一个全球性问题。可以通过评估土壤性质(包括退化土地的化学性质)的空间变异性并绘制此类变化的图来对退化土地进行最佳管理。由于印度的耕地中有很大一部分由于土壤酸度而化学降解;本研究旨在研究某些作物的土壤酸度(pH),电导率(EC),土壤有机碳(OC)含量,可交换钾(K +),钙(Ca2 +)和镁(Mg2 +)含量的空间变异性。印度的酸性土壤。从位于奥里萨邦,贾坎德邦,喜马al尔邦和喀拉拉邦的四个土壤系列的可耕土壤中收集了总共四百个(每个系列一百个)深度(0-0.15m深度)的土壤样品,这些土壤分别是Hariharapur,Debatoli,Rajpora和Neeleswaram印度分别进行了分析。与其他土壤特性(中等)相比,土壤酸度(pH在3.90和6.45之间)显示出较低的变异性。 EC(均值介于0.05至0.09dSm(-1)之间)和OC(均值介于0.29至1.86%之间)的变异系数从32.4至74.3、31.2至50.9、45.6至100、71.9至93.0和59.0至79.8%不等,可交换的K +(平均介于39.1和77.7mgkg(-1)之间),Ca2 +(平均介于148和293mgkg(-1)之间)和Mg2 +(平均介于111和191mgkg(-1)之间)。土壤的pH和OC含量与可交换的K +,Ca2 +和Mg2 +含量呈显着正相关。地统计分析表明,对于不同的土壤特性,具有最佳的空间依赖性的最佳拟合模型是高斯模型,指数模型和球形模型。版权所有(c)2014 John Wiley&Sons,Ltd.

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