Status Of Soil Chemical Properties As Affected By Seasonal Variation In The Sub-Tropical Forest Zone Of Western Himalaya

B. Kumari, A. Tiwari, Sangeeta Sharma, Jasra Anjum
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Abstract

The forest ecosystem plays a crucial role in maintaining the inter-related complexity between vegetation and soil. Anthropogenic pressure, not only reduces the forest biodiversity but also leads to the deterioration of the soil quality. Thus, it is essential to understand the soil condition to promote the growth of the forest ecosystem. The current study analyzes the physicochemical properties of soils under pine forest stand, by collecting the samples at three different soil depths (0-10 cm, 10-20 cm, and 20-30 cm). The study mainly focused on the available soil cations (sodium, calcium, and potassium) because they act as an immediate source for vegetation. The main objective of the present study was to determine the variation in soil available cations (K+, Ca+ , and Na + ) concentration along with the soil depth during different seasons. Seasonal alterations occurred in the soil's chemical attributes, influenced by ecological changes occurred in vegetation. Results showed seasonal fluctuations in soil pH, EC, and soil cations during the study period. Results also showed that variation in potassium and calcium concentration during different seasons does not differ significantly on the other side variation in sodium concentration differs significantly during different seasons. Sodium and calcium content also showed significant differences among the different sites.
西喜马拉雅亚热带林区土壤化学性质随季节变化的状况
森林生态系统在维持植被与土壤相互关联的复杂性方面起着至关重要的作用。人为压力不仅减少了森林生物多样性,而且导致土壤质量恶化。因此,了解土壤状况对促进森林生态系统的生长至关重要。本研究通过收集3种不同土壤深度(0-10 cm、10-20 cm和20-30 cm)的样品,分析了松林林下土壤的理化性质。这项研究主要集中在可用的土壤阳离子(钠、钙和钾)上,因为它们是植被的直接来源。本研究的主要目的是确定不同季节土壤有效阳离子(K+、Ca+和Na +)浓度随土壤深度的变化。受植被生态变化的影响,土壤化学属性发生了季节性变化。结果表明,研究期间土壤pH、EC和阳离子呈季节性波动。钾、钙浓度在不同季节的变化差异不显著;钠浓度在不同季节的变化差异显著。不同部位的钠、钙含量也存在显著差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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