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首页> 外文期刊>International Research Journal of Pure and Applied Chemistry >Morpho-physical Properties of Soils of Kanamadi South Sub-watershed of Karnataka
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Morpho-physical Properties of Soils of Kanamadi South Sub-watershed of Karnataka

机译:卡纳塔克卡神器南水域土壤的态度性质

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An investigation was carried out to determine the morpho-physical status of soils of Kanamadi South sub- watershed in Karnataka state of India. A detailed soil survey of Kanamadi South sub watershed was carried out using IRS P6 LISS-IV image and a total of ten pedon location? which were well distributed in Kanamadi South sub-watershed was selected. The soils were shallow to deep. Colour of pedons varied from 10 YR 2/1 (black) to 10 YR 4/3 (brown). Soil texture varied from clay to clay loam, having loose to moderately subangular to angular blocky in structure with few fine roots distributed in surface horizons. Generally, the clay content increased with depth. Consistency of soil pedons ranged from slightly hard to hard when dry, friable to firm when moist, slightly sticky to very sticky and slightly plastic to very plastic when wet. The maximum water holding capacity of soil horizons ranged from 59.65 to 79.15 per cent and generally increased down the depth. The bulk density of pedons varied from 1.17 to 1.37 Mg m-3. In general, bulk density varied with depth with lowest bulk density at surface and highest recorded in sub surface depths. The field capacity varied from 28.21% to 41.32 %.The morphological and physical properties study in area helps for resource inventorization for successful watershed planning for soil and water conservation to enhance the potential of fertility of soils and major fertility enhancement to increase the soil productivity.
机译:进行了调查,以确定印度卡纳塔卡州卡纳纳塔卡州的卡纳马迪南部土壤的态势状况。使用IRS P6 Liss-IV图像进行了Kanamadi South Sub流域的详细土壤调查,共进行了十个佩丁位置?选择了在Kanamadi South Sub-shatershed中分布得很好。土壤深入深入。施行的颜色从10 yr 2/1(黑色)变化到10 yr 4/3(棕色)。土壤纹理从粘土到粘土壤土的变化,在结构中具有较小的中间与角度块,在表面视野中分布很少。通常,粘土含量随深度增加。土壤施用的一致性在干燥时略微难以努力,在湿润时易碎,稍微粘在非常粘稠,略带塑料时湿润。土壤范围的最大水持续能力范围为59.65至79.15%,一般增加深度。施用的堆积密度从1.17变化到1.37mg m-3。通常,堆积密度随深度而具有最低堆积密度的深度,并且在子表面深度中记录最高。现场容量从28.21%变化至41.32%。地区的形态和物理性质研究有助于资源库存,以获得土壤和水资源的成功流域规划,以提高土壤肥力的潜力和重大生育能力,以提高土壤生产力。

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