Coconut-growing soils in southern Karnataka: Characterization and classification

Q4 Agricultural and Biological Sciences Journal of Plantation Crops Pub Date : 2019-08-20 DOI:10.25081/JPC.2019.V47.I2.5774
R. Avinash
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引用次数: 2

Abstract

A study was carried out to characterize and classify major coconut-growing soils of southern Karnataka and to evaluate the suitability of these soils for coconut cultivation. Seven locations were selected on the map of coconut-growing areas in southern Karnataka and delineated based on the variability of agro-climate with the help of land resource map and report of Karnataka state, generated at 1: 2,50,000 scale by ICAR-NBSSLUP. The regions included Hosadurga (central dry zone), Gubbi and Turuvekere (eastern dry zone), Krishnarajapet (southern dry zone), Arasikere (southern transition zone), Belthangadi and Brahmavara (coastal zone) representing the density of coconut-growing areas in different agro-climatic zones. Soil profiles were studied at these selected sites. The coconut growing soils of southern Karnataka are generally deep, gravelly and well drained, sandy clay loam to clayey in texture with good structure. Soils of high rainfall areas of Belthangadi and Brahmavara were strongly acidic and rich in soil organic carbon, whereas other locations of sub-humid to semi-arid were near neutral to moderately alkaline soils with medium organic carbon content. Cation Exchange Capacity and base saturation were very low in coastal red and lateritic coconut soils and ranged from medium to high in other areas. The major taxa of the soils identified at sub-group level of soil taxonomy are Rhodic Kanhaplustults, Ustic Kandihumults, Rhodic Paleustalfs, Typic Rhodustalfs and Vertic Haplustepts.
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卡纳塔克邦南部椰子种植土壤:特征和分类
对卡纳塔克邦南部主要椰子种植土壤进行了特征和分类研究,并评价了这些土壤对椰子种植的适宜性。在卡纳塔克邦南部椰子种植区地图上选择了7个地点,并利用ICAR-NBSSLUP以1:25万比例尺生成的卡纳塔克邦土地资源图和报告,根据农业气候的变率进行了圈定。这些地区包括Hosadurga(中部干旱区)、Gubbi和Turuvekere(东部干旱区)、Krishnarajapet(南部干旱区)、Arasikere(南部过渡区)、Belthangadi和Brahmavara(沿海区),代表了不同农业气气区椰子种植区的密度。在这些选定的地点研究了土壤剖面。卡纳塔克邦南部种植椰子的土壤通常是深的,砾石质,排水良好,砂质粘土壤土到粘土质地,结构良好。Belthangadi和Brahmavara高降雨量地区的土壤呈强酸性,土壤有机碳含量丰富,而其他半湿润至半干旱地区的土壤接近中性至中碱性,土壤有机碳含量中等。沿海红壤和红壤椰子土阳离子交换容量和碱饱和度极低,其他地区为中等至高。在土壤分类亚群水平上鉴定出的土壤类群主要有Rhodic Kanhaplustults、Ustic Kandihumults、Rhodic Paleustalfs、typical Rhodustalfs和Vertic Haplustepts。
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来源期刊
Journal of Plantation Crops
Journal of Plantation Crops Agricultural and Biological Sciences-Agronomy and Crop Science
CiteScore
0.60
自引率
0.00%
发文量
15
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