Effect of landforms and vegetations on pedological variability and crop yield along the toposequence of Eastern Coastal Plain of Odisha, India

IF 16.4 1区 化学 Q1 CHEMISTRY, MULTIDISCIPLINARY
Srinivasan Ramasamy, Lalitha Manickam, Shelton Padua, Tejashvini Ashwathappa, Jagdish Prasad, Surendra Kumar Singh
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Abstract

Topography and vegetation have a significant role in soil development in different ecosystems. Interactions between soil and landforms help to understand the pedogenic processes and soil variability. The present study assessed the impact of various landforms and vegetation on pedological variability along the toposequence of the eastern coastal plain. We characterized 46 soil profiles from five landforms, viz., foothills, upland, alluvial plains, coastal plains, and sandbars and performed factor analysis. The frequency distribution of the soil properties was significantly skewed with each other’s. Soils are classified into three orders: Alfisols, Inceptisols, and Entisols from hills to sandbars. The soils were characterized by clay (2.50–65.8%), AWC (4.0–28.0%), pH (5.40–9.40), EC (0.03–5.60 dSm−1), OC (0.01–1.13%), CEC (1.0-31.60 cmol (p+) kg−1), BS (57–95%) and ESP (0.54–27.8%). Whereas alluvial plain soils are rich in clay and organic carbon, foothill and upland soils experience severe to moderate soil erosion, leading to the leaching of basic cations. Coastal plains face regular seawater intrusion and flooding, causing excess deposition of salts, which alter the soil pedogenic process under different landforms and land use. Soil pH, EC, clay, CEC and ESP significantly influenced the paddy yield in alluvial and coastal plains landforms. Development of landform and soil relationships concerning land uses in coastal regions helps to identify factors involved in soil development, pedogenic processes and crop productivity.

Abstract Image

地貌和植被对印度奥迪沙东部沿海平原地形变化和作物产量的影响
在不同的生态系统中,地形和植被在土壤发育过程中起着重要作用。土壤与地貌之间的相互作用有助于了解成土过程和土壤变异。本研究评估了东部沿海平原地形序列中各种地貌和植被对成土变化的影响。我们对山麓、高地、冲积平原、滨海平原和沙洲等五种地貌的 46 个土壤剖面进行了特征描述,并进行了因子分析。土壤特性的频率分布相互之间有明显的偏斜。土壤分为三个等级:从丘陵到沙洲的土壤被分为三个等级:Alfisols、Inceptisols 和 Entisols。这些土壤的特征是:粘土(2.50-65.8%)、AWC(4.0-28.0%)、pH(5.40-9.40)、EC(0.03-5.60 dSm-1)、OC(0.01-1.13%)、CEC(1.0-31.60 cmol (p+) kg-1)、BS(57-95%)和 ESP(0.54-27.8%)。冲积平原土壤富含粘土和有机碳,而山麓和高地土壤则遭受严重至中度的土壤侵蚀,导致基本阳离子被沥滤。沿海平原经常面临海水入侵和洪水泛滥,导致盐分过度沉积,从而改变了不同地貌和土地利用条件下的土壤成土过程。土壤 pH 值、导电率、粘度、CEC 和 ESP 对冲积平原和沿海平原地貌下的水稻产量有显著影响。发展与沿海地区土地利用有关的地貌和土壤关系,有助于确定与土壤发育、成肥过程和作物产量有关的因素。
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来源期刊
Accounts of Chemical Research
Accounts of Chemical Research 化学-化学综合
CiteScore
31.40
自引率
1.10%
发文量
312
审稿时长
2 months
期刊介绍: Accounts of Chemical Research presents short, concise and critical articles offering easy-to-read overviews of basic research and applications in all areas of chemistry and biochemistry. These short reviews focus on research from the author’s own laboratory and are designed to teach the reader about a research project. In addition, Accounts of Chemical Research publishes commentaries that give an informed opinion on a current research problem. Special Issues online are devoted to a single topic of unusual activity and significance. Accounts of Chemical Research replaces the traditional article abstract with an article "Conspectus." These entries synopsize the research affording the reader a closer look at the content and significance of an article. Through this provision of a more detailed description of the article contents, the Conspectus enhances the article's discoverability by search engines and the exposure for the research.
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