Dynamics of Water-Soluble Carbon and Nitrogen Content in Soils in the First Years after Clearcutting

IF 1.4 4区 农林科学 Q4 SOIL SCIENCE Eurasian Soil Science Pub Date : 2024-06-03 DOI:10.1134/s1064229324600064
V. V. Startsev, D. A. Severgina, A. A. Dymov
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Abstract

Logging is one of the main anthropogenic factors that change forest ecosystems. An experiment was launched to study the effect of logging equipment on soil properties after cutting spruce forests in the middle taiga of the Komi Republic, during which skidding trails with different number of wheeled vehicle passes (forwarder PONSSE ELEPHANT) were set. Carbon (Cws) and nitrogen (Nws) of water-soluble compounds play an important role in the global cycle of elements. The paper presents the results of observations over the water-soluble organic matter content in the soils of original forests (podzolic soils—Albic Retisols) and the soils at different technological sites of the logging area that have experienced different loads, i.e., cutting strips and skidding trails with three passes of logging equipment (podzolic soil), ten passes (turbozem), and passes followed by leveling (turbozem). A significant increase in total carbon was revealed in soils in the first two years after cutting. The greatest changes were registered in the upper mineral horizons (EL and TURcwd), in which the carbon content increased 3–6 times (0.32–2.2%) versus 0.45% in the original forest soil. A considerable rise in the Cws content was found in organic and mineral soil horizons (up to 33.4 and 0.46 mg/g, respectively) after clear cutting, which thrice on average exceeds the initial values. The content of water-soluble nitrogen increases from 0.23 to 2.12 mg/g in the organic horizon two years after tree cutting. In the mineral horizons, the Nws content varied from 0.003 to 0.020 mg/g after cutting (versus 0.002–0.011 mg/g in the original forest soil). It is shown that an increase in water-soluble carbon and nitrogen contents can be considered a significant criterion of changing soil organic matter due to logging activities, since their concentrations differ substantially from the initial values.

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开垦后第一年土壤中水溶性碳和氮含量的动态变化
摘要 伐木是改变森林生态系统的主要人为因素之一。为了研究在科米共和国中泰加云杉林砍伐后采伐设备对土壤性质的影响,进行了一项实验,在实验过程中设置了不同轮式车辆通行次数的滑行道(PONSSE ELEPHANT)。水溶性化合物中的碳(Cws)和氮(Nws)在全球元素循环中发挥着重要作用。本文介绍了对原始森林土壤(podzolic soil-Albic Retisols)和伐木区不同技术地点土壤中水溶性有机物含量的观测结果,这些土壤经历了不同的负载,即伐木设备三次通过(podzolic soil)、十次通过(turbozem)和通过后再平整(turbozem)的伐木带和滑行道。在砍伐后的头两年,土壤中的总碳量明显增加。变化最大的是上层矿物层(EL 和 TURcwd),其碳含量增加了 3-6 倍(0.32-2.2%),而原始森林土壤的碳含量仅为 0.45%。砍伐后,有机土壤层和矿质土壤层中的 Cws 含量大幅上升(分别达到 33.4 和 0.46 mg/g),平均比初始值高出三倍。树木砍伐两年后,有机地层中的水溶性氮含量从 0.23 毫克/克增加到 2.12 毫克/克。在矿质层中,砍伐后的水溶性氮含量从 0.003 到 0.020 毫克/克不等(而原始森林土壤中的水溶性氮含量为 0.002-0.011 毫克/克)。这表明,水溶性碳和氮含量的增加可被视为伐木活动导致土壤有机质变化的一个重要标准,因为它们的浓度与初始值相差很大。
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来源期刊
Eurasian Soil Science
Eurasian Soil Science 农林科学-土壤科学
CiteScore
2.70
自引率
35.70%
发文量
137
审稿时长
12-24 weeks
期刊介绍: Eurasian Soil Science publishes original research papers on global and regional studies discussing both theoretical and experimental problems of genesis, geography, physics, chemistry, biology, fertility, management, conservation, and remediation of soils. Special sections are devoted to current news in the life of the International and Russian soil science societies and to the history of soil sciences. Since 2000, the journal Agricultural Chemistry, the English version of the journal of the Russian Academy of Sciences Agrokhimiya, has been merged into the journal Eurasian Soil Science and is no longer published as a separate title.
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