首页> 外文期刊>Acta Horticulturae >Identification, Description and Taxonomical Classification of Major Cashew (Anacardium occidentale L.) Growing Soils of Southern Karnataka, India
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Identification, Description and Taxonomical Classification of Major Cashew (Anacardium occidentale L.) Growing Soils of Southern Karnataka, India

机译:印度南部卡纳塔克邦主要腰果(Anacardium occidentale L.)生长土壤的鉴定,描述和分类学分类

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Six typical pedons representing major cashew growing soils of Dakshina Kannada district of Southern Karnataka developed from granite-gneiss and uvium parent materials were studied for their morphological; physical and emical properties. The soils werestrongly to moderately acidic in reaction, non-ne, deep to very deep in depth and have iso-hyperthermic temperature and ustic moisture regimes. The soils were sandy clay loam to clay in texture, sub-angular tocky in structure, dark brown to red in colour, medium to high in organic carbon ntent and low cation exchange capacity and base saturation. The soils also had high amounts of coarse fragments and clay fractions. Among the exchangeable cations, calcium was found to be high in most soils, followed by magnesium, sodium and potassium. Among the DTPA extractable micronutrients, iron and manganese were sufficient in most soils, and available copper and zinc were deficient. The dry consistency varied from slightly hard to hard, moist consistency from loose to very friable/firm and wet consistency from slightly sticky/sticky to plastic. The exchangeable acidity was very high in all the pedons. The soil orders identified in the study areas were Ultisols and Inceptisols. Based on the characteristics, these cashew soils were classified as Ustic Haplohumults, Oxic Dystrustepts, Rhodic Kanhaplustults, Ustic Palehumults and Typic Paleustults.
机译:研究了六种典型的花and的形态,这些花代表了南部的卡纳塔克邦达克西纳·卡纳达地区主要的腰果生长土壤,这些花from是由花岗片麻岩和铀母材制成的。物理和仿真特性。土壤在反应中呈强酸性至中等酸性,非Ne,深至非常深,并且具有等温温度和ustic水分状态。土壤是质地为砂壤土到粘土的壤土,结构为近角的曲折,颜色为深棕色至红色,有机碳含量中等至较高,阳离子交换容量和碱饱和度较低。土壤中也有大量的粗碎屑和粘土碎片。在可交换的阳离子中,大多数土壤中的钙含量很高,其次是镁,钠和钾。在DTPA可提取的微量营养素中,大多数土壤中铁和锰足够,而有效铜和锌则不足。干稠度从稍硬到坚硬不等,湿稠度从松散到非常脆/坚硬不等,湿稠度从稍粘/粘性到塑料不等。在所有的脚踏板上,可交换的酸度都很高。在研究区域中确定的土壤次序是Ultisols和Inceptisols。根据这些特征,这些腰果土壤分为Ustic Haplohumults,Oxy Dystrustepts,Rhodic Kanhaplustults,Ustic Palehumults和Typic Paleustults。

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