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首页> 外文期刊>Journal of the Indian Society of Soil Science >Characterization and Classification of Sugarcane Growing Soils of North Coastal Districts of Andhra Pradesh
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Characterization and Classification of Sugarcane Growing Soils of North Coastal Districts of Andhra Pradesh

机译:北沿海地区甘蔗生长土壤的特征及分类

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Twelve Typical pedons from sugarcane growing soils of Visakhapatnam, Vizianagaram and Srikakulam district were studied for their morphological characteristics, physical, physicochemical and chemical properties and classified as per USDA soil taxonomy.All the pedons were confined to semi-arid mansoonic climate and occur on low lying to plain lands. The soils were deep with coarse texture in sandy soils and clay loam texture in black soils. Single grain to sub-angular blocky structure, wet consistenceof non-sticky, non plastic to plastic, sticky were the other features recognized. The results of physicochemical properties revealed that all the soils were neutral to moderately alkaline in soil reaction with non-saline conductivity. Among all the exchangeable bases calcium was the dominant cation followed by magnesium, potassium and sodium. All the surface layers exhibited low to medium in available nitrogen status and medium to high in available phosphorus and potassium status. Available copper andmanganese in all pedons were above critical limits. Sufficiency in available zinc and iron status (except pedon 8-12) was observed in all the surface layers. The study area falls under ustic moisture and isohyperthermic temperature regimes. The mineralogy is mixed type. The pedons of Visakhapatnam district are classified as fine loamy, mixed, isohyperthermic, Typic Haplustepts and coarse loamy, mixed isohyperthermic, Typic Haplustepts.
机译:研究了维萨卡帕特南、维齐亚纳加拉姆和斯里卡库拉姆地区甘蔗种植土壤中的12种典型土壤的形态特征、物理、理化和化学性质,并根据美国农业部土壤分类法进行了分类。所有土壤都局限于半干旱的季风气候,分布在低洼平原地区。土壤较深,砂土质地粗糙,黑土质地粘壤土。单颗粒到次棱角块状结构、湿稠度为非粘性、非塑性到塑性、粘性为其他特征。理化性质的结果表明,所有土壤在土壤反应中均为中性至中等碱性,具有非盐电导率。在所有交换性碱中,钙是主要阳离子,其次是镁、钾和钠。各表层土壤速效氮水平均为低中,速效磷钾水平均为中高。所有土壤中的有效铜和锰均高于临界限值。在所有表面层中观察到充足的锌和铁(pedon 8-12除外)。研究区域处于非均匀湿度和等温热温度条件下。矿物学为混合型。Visakhapatnam地区的土壤分为细壤土、混合型、等温热型、典型单粒土和粗壤土、混合型、等温热型、典型单粒土。

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