印度北阿坎德邦兰甘加河谷西部不同森林类型土壤理化性质

D. Rawat, D. Das, P. Tiwari, Preeti Naithani, J. K. Tiwari
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摘要

研究了印度北阿坎德邦查莫利Ramganga山谷西部不同海拔(低、中、高)、坡度、坡向和区系组成(L1(混合橡树)、L2(赤松)、M1(混合杜鹃)、M2(混合杜鹃)、U1(混合冷杉)和U2(混合冷杉))6种不同森林的土壤理化性质。在不同季节采集0 ~ 10 cm、11 ~ 20 cm和21 ~ 30 cm 3个深度的复合土壤样品,采用标准手册和方案对其理化参数进行分析。对各立地土壤样品的质地、容重、含水量、持水量、有机质、有机碳、pH、氮含量、速效磷、交换态钾和C:N比值进行了分析和讨论。结果表明,在0 ~ 10 cm、11 ~ 20 cm和21 ~ 30 cm三个深度,土壤的物理性质变化不大或变化不大,而化学性质变化较大。6种森林类型(研究点)土壤质地(砂、粉、粘)、含水量、持水量、氮含量差异显著(方差分析,P < 0.05)。土壤质地介于壤土和砂壤土之间,有利于植物生长。此外,土壤容重较低,土壤有机碳和其他确定参数的有机质含量较高,表明6个森林具有持续的营养土壤。结果表明,西喜马拉雅地区不同海拔植被组成(森林类型)不同,土壤理化性质也不同。将进行进一步的详细研究,以确定植被和土壤之间的相互关系。
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Physicochemical Properties of Soil under Different Forest Types in the Western Ramganga Valley (Uttarakhand Himalaya, India)
The physicochemical properties of soils of six forests varying in elevation (lower, middle, and upper), slope, aspects, and floristic composition viz. L1 (Oak mixed), L2 (Chir pine), M1 (Rhododendron mixed), M2 (Rhododendron mixed), U1 (Abies mixed) and U2 (Abies mixed) from Western Ramganga Valley (Chamoli, Uttarakhand Himalaya, India) were scrutinized. The composite soil samples from three depths (0–10 cm, 11–20 cm, and 21–30 cm) were collected during the different seasons and the physicochemical parameters were analyzed using standard manual and protocol. Texture, bulk density, moisture content, water holding capacity, organic matter, organic carbon, pH, nitrogen content, available phosphorus, exchangeable potassium and C:N ratio of soil samples from each forest site were analyzed and discussed. It was observed that the physical properties of soils either do not vary across the three depths (0–10 cm, 11–20 cm, and 21–30 cm) or show slight changes whereas chemical properties show notable variations comparatively. The significant variation (ANOVA, P < 0.05) was observed in the soil texture (sand, silt, and clay contents), moisture content, water holding capacity, and nitrogen content across the six forest types (study sites). The soil texture ranged between loam and sandy loam which is considered supportive for plant growth. Besides, the lower bulk density and higher soil organic carbon and organic matter with other determined parameters in the studied soils indicate that the studied six forests have sustained nutritive soils. It can be concluded from the present results that the soil physicochemical properties vary with changes in the vegetation composition (forest types) at different elevations in Western Himalaya. Further elaborative study will be done to ascertain interrelationship among the vegetation and soils.
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