首页> 外文期刊>Journal of the Indian Society of Soil Science >Characterization, Classification and Evaluation of Soils of Olpad Taluka in Coastal Region of Surat District, Gujarat
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Characterization, Classification and Evaluation of Soils of Olpad Taluka in Coastal Region of Surat District, Gujarat

机译:古吉拉特邦苏拉特区沿海地区Olpad taluka土壤的表征、分类和评价

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© 2022, Indian journals. All rights reserved.Five representative pedons (P1 Barbodhan; P2 Tena; P3 Bhandut; P4 Takrama; and P5 Karanj) from different landforms of Olpad taluka in the coastal region of Surat district, Gujarat were studied for their morphological, physical, and chemical properties. The soils were deep to very deep (100-150 cm), well to imperfectly drained, neutral to strongly alkaline (pH 7.1-9.4), non-saline to highly saline (0.2-12.6 dS m-1), low to high in organic carbon (2.2-18.7 g kg-1) and CaCO3 (5.0-18.9), and medium to high in cation exchange capacity 35.7-70.0 cmol(p+)kg-1. Soil texture varied from clay loam to clay with the clay content ranging from 34.2 to 55.6. Bulk density was lower in Takrama soil (1.29-1.34 Mg m-3) than the other soils (1.30-1.55 Mg m-3). Saturated hydraulic conductivity of the soils varied from 0.1 to 1.7 cm h-1 and it was less than the critical limit of 1.0 cm h-1 in Bhandut and Karanj soils. The exchangeable sodium percentage varied from low to very high (3.6-83.6), and the pedons were generally high in exchangeable magnesium percentage (27.2-55.1). The Barbodhan pedon with the cambic horizon was classified as Typic Haplustepts, and the similar Tena pedon with vertic characteristics was classified as Vertic Haplustepts. The Bhandut, Takrama, and Karanj pedons were classified as Sodic Haplustepts, Typic Haplusterts and Sodic Haplusterts, respectively. The soils were grouped under II (Takrama), IIs (Barbodhan and Tena) and IIIws (Bhandut and Karanj) according to land capability classification.
机译:© 2022 年,印度期刊。保留所有权利。5个代表性蜥蜴(P1 Barbodhan;P2 特纳;P3 班杜特;P4 Takrama;和 P5 Karanj) 研究了古吉拉特邦苏拉特区沿海地区不同地貌的 Olpad taluka 的形态、物理和化学性质。土壤从深到很深(100-150 cm),排水良好至不完全,中性至强碱性(pH 7.1-9.4),无盐至高盐(0.2-12.6 dS m-1),有机碳含量低至高(2.2-18.7 g kg-1)和CaCO3(5.0-18.9%),阳离子交换能力中高[35.7-70.0 cmol(p+)kg-1]。土壤质地从粘壤土到粘土不等,粘土含量在34.2%-55.6%之间。塔克拉玛土壤的容重(1.29-1.34 Mg m-3)低于其他土壤(1.30-1.55 Mg m-3)。土壤的饱和导水率在0.1-1.7 cm h-1之间变化,在Bhandut和Karanj土壤中小于1.0 cm h-1的临界极限。可交换钠百分比从低到极高不等(3.6-83.6),可交换镁百分比普遍较高(27.2-55.1)。具有 cambic 地平线的 Barbodhan pedon 被归类为 Typic Haplustepts,具有垂直特征的类似 Tena pedon 被归类为 Vertic Haplustepts。Bhandut、Takrama 和 Karanj pedons 分别被归类为 Sodic Haplustepts、Typic Haplusterts 和 Sodic Haplusterts。根据土地能力分类,土壤分为II类(Takrama)、II类(Barbodhan和Tena)和IIIws(Bhandut和Karanj)。

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