Characterization of soils under different periods of eucalyptus cultivation and restoration in Malur and Hoskotetaluks of Karnataka, India

Haravina Manjunathaswamy Pruthvi Raj, Belvadi Nanjappa Dhananjaya, Bommalingaianapalya Narasahanumaiaha Maruthi Prasad, Ramapatna Lakshmaiah Raghunatha Reddy, Thyavanahally Hanumaiah Shankarappa
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Abstract

Considerable area under eucalyptus plantation in the form of farm forestry exists in Malur and Hoskotetaluks of Karnataka, India. But in the recent years, Government of Karnataka has checked the spread of eucalyptus and farmers are gradually converting their eucalyptus plantations into agricultural lands. This study was aimed to evaluate soils of eucalyptus during growing and after restoration and its adjacent croplands having no history of eucalyptus cultivation in Taluks of Malur and Hosakote, Karnataka for physico-chemical properties and evaluated during the year 2019-2020 at College of Horticulture, Kolar. The results revealed that soils under 12, 24 and 48 years of eucalyptus cultivation when compared to soils after two, six and ten years of restoration and adjacent soils, showed significantly high bulk density (1.28 to 1.51 Mg/m3) and low water holding capacity (30.30 to 45.61%). These soils were more acidic in reaction (pH: 6.21 to 6.65) and contained significantly lower amounts of total soluble salts (EC: 0.04 to 0.07 dS/m), organic carbon (OC: 0.24 to 0.59%), available N, P2O5 and K2O (163.07 to 235.42, 26.03 to 47.23 and 112.89 to 168.55 Kg/ha, respectively), exchangeable Ca and Mg (1.70 to 2.75 and 0.80 to 1.32 cmol (p+)/Kg, respectively) and available S (5.60 to 7.09 ppm) but contained significantly high amounts of available Fe, Mn, Zn and Cu (13.52 to 29.74, 14.06 to 20.14, 1.44 to 2.06 and 1.16 to 1.74 ppm, respectively). Further, bulk density, acidity and available micronutrient cations of soils tends to increase with prolonging the cultivation period of eucalyptus while, reverse trend was observed with respect to water holding capacity, organic carbon and available macronutrients contents. On the other hand, restored plots showed significantly decreased acidity, bulk density and available micronutrient cations and increased water holding capacity and macronutrients contents with increasing the restoration period.
印度卡纳塔克邦Malur和Hoskotetaluks桉树栽培和恢复不同时期土壤特征
印度卡纳塔克邦的Malur和Hoskotetaluks有相当大的桉树人工林。但近年来,卡纳塔克邦政府遏制了桉树的蔓延,农民们逐渐将桉树种植园转变为农业用地。本研究旨在评估卡纳塔克邦Malur和Hosakote Taluks地区桉树生长期间和恢复后的土壤及其邻近无桉树种植历史的农田的理化性质,并于2019-2020年在Kolar园艺学院进行评估。结果表明:桉树造林12年、24年和48年土壤的容重(1.28 ~ 1.51 Mg/m3)显著高于恢复2年、6年和10年土壤,持水量(30.30 ~ 45.61%)显著低于邻近土壤。这些土壤在反应中酸性更强(pH: 6.21 ~ 6.65),总可溶性盐(EC: 0.04 ~ 0.07 dS/m)和有机碳(OC: 0.07 dS/m)含量显著降低。有效N、P2O5和K2O(分别为163.07 ~ 235.42、26.03 ~ 47.23和112.89 ~ 168.55 Kg/ha)、交换态Ca和Mg(分别为1.70 ~ 2.75和0.80 ~ 1.32 cmol (p+)/Kg)和有效态S (5.60 ~ 7.09 ppm),而有效态Fe、Mn、Zn和Cu(分别为13.52 ~ 29.74、14.06 ~ 20.14、1.44 ~ 2.06和1.16 ~ 1.74 ppm)含量显著较高。随着桉树栽培年限的延长,土壤容重、酸度和速效微量元素阳离子呈增加趋势,持水量、有机碳和速效大量元素含量呈相反趋势。另一方面,随着恢复时间的延长,恢复地块的酸度、容重和有效微量元素阳离子显著降低,持水量和大量元素含量显著增加。
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