喀拉拉邦的椰子种植土壤:1。特点与分类

Q4 Agricultural and Biological Sciences
K. M. Nair, K. A. Kumar, S. Kumar, V. Ramamurty, M. Lalitha, S. Srinivas, A. Koyal, S. Parvathy, K. Sujatha, Shivanand, R. Hegde, S. K. Singh
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引用次数: 6

摘要

椰子种植园是喀拉拉邦主要的土地利用系统。该州的热带湿热气候和土壤被认为适合棕榈树生长,除了海拔600米以上的高地。然而,该邦的椰子产量极低,平均每棵棕榈树每年只能产40颗坚果。为查明在热带湿热气候下发育的高风化淋滤低活性粘土是否为低产量的原因,对该州椰子种植土壤进行了土壤质量评价。根据农业气候和土壤的可变性,确定并划定了该邦六个不同的椰子种植区域,即帕拉卡德中部和东部、喀拉拉邦北部、喀拉拉邦中部、喀拉拉邦南部、奥纳图卡拉沙质平原和沿海沙质平原。对各地区代表性地点的土壤剖面进行了研究。研究了土壤的形态特征,并横向取样分析了土壤的物理和化学性质。喀拉拉邦种植椰子的土壤通常很深,排水良好,粘土或沙质具有良好的结构,可以快速输送水分。帕拉卡德、喀拉拉邦南部和沿海沙质平原的土壤具有接近中性的反应,而喀拉拉邦北部和中部的大面积红土土壤以及奥纳图卡拉的沙土具有强酸性,并且具有高水平的KCl可提取铝。酸性土壤还分析了碱性阳离子、钾、钙和镁的低含量。除了Palakkad以外,所有地区的土壤CEC都很低。喀拉拉邦中北部和奥纳图卡拉沙质平原土壤的表层和底土基态极低。根据土壤分类学,将帕拉卡德中部和东部土壤划分为典型haplustfs,喀拉拉邦北部划分为plinthults,喀拉拉邦中部划分为典型Plinthustults,喀拉拉邦南部划分为Rhodic Kandiustults,沙质平原划分为Ustipsamments。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coconut-growing soils of Kerala: 1. Characteristics and classification
Coconut plantations are the major land use systems in Kerala state. The tropical hot humid climate and soils of the state are considered suitable for the palm, with the exception of highlands occurring 600 m above MSL. However, the productivity of coconut is abysmally low in the state with an average productivity of around 40 nuts per year per palm. To find out whether the highly weathered and leached low activity clay soils developed in tropical hot humid climate is responsible for the low yield, an assessment of soil qualities in the coconut-growing soils of the state was made. Six distinct regions of coconut cultivation in the state were identified and delineated based on the variability of agro-climate and soils, viz., Central and Eastern Palakkad, Northern Kerala, Central Kerala, Southern Kerala, Onattukara sandy plains and coastal sandy plains. Soil profiles were studied at representative sites in each region. Investigated morphological features and sampled horizon-wise for the analysis of physical and chemical properties of the soil. Coconut-growing soils of Kerala state are in general deep and well drained, clayey or sandy having good structure permitting rapid transmission of water. The soils of Palakkad, Southern Kerala and Coastal Sandy Plains have near neutral reaction whereas the extensive areas of laterite soils of Northern and Central Kerala and sandy soils of Onattukara were strongly acid and had high levels of KCl extractable aluminium. The acid soils also analysed for low levels of basic cations, potassium, calcium and magnesium. Soils from all regions except Palakkad have low CEC. Surface and sub-soils base status were extremely low for soils of Northern and Central Kerala and Onattukara sandy plain. The soils of Central and Eastern Palakkad were classified as Typic Haplustalfs, Northern Kerala as Plinthic Humults, Central Kerala as Typic Plinthustults, Southern Kerala as Rhodic Kandiustults and the soils of sandy plains as Ustipsamments, according to soil taxonomy.
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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
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