The Effects of Stand Development Stages on Soil Carbon and Nitrogen Stocks in Black Pine, Scots Pine and Fir Stands in Türkiye

G. Savacı, Yunus Doğan
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Abstract

The influence of stand development stages on soil organic carbon (SOC) and total nitrogen (TN) stocks was examined in black pine (Pinus nigra Arnold.), Scots pine (Pinus sylvestris L.), and Kazdağı fir (Abies nordmanniana subsp. equi-trojanı (Aschers. & Sint. ex Boiss) Coode et Cullen), differing in the mean tree diameters in which reproduction stages (RS)=<8 cm, sapling or pole stages (SPS)= 8-19.9 cm, large pole stages (LPS)= 20-35.9 cm, and medium wood stages (MWS)=36-51.9 cm in three tree species located in northwestern Turkey. A total of 216 soil samples were collected and analyzed for pH, organic matter, bulk density, maximum water holding capacity, carbon, and nitrogen concentrations, and the SOC and TN stocks were calculated. SOC and TN stocks varied significantly among the four stand development stage classes. The SOC stock at 0-30 cm increased significantly due to an increase in the diameter of black stands (BPLPS and BPMWS). SOC stocks in all stand development stages peaked in the large pole (44.94 Mg/ha) and declined as the sapling or pole (37.71 Mg/ha) was replaced by medium wood stands (30.17 Mg/ha), and a low point (27.94 Mg/ha) was found in the reproduction stages of stand development for Scots pine. The TN stock at a soil depth of 0-30 cm ranged from 1.66 to 6.46 Mg/ha. The highest TN stock was observed in the SPSPS (6.46 Mg/ha) and FirRS (5.48 Mg/ha), and the lowest was observed in the BPLPS (1.66 Mg/ha) stands. The results illustrate that soil was the main storage of C and N in all different stand development stages of tree species.
图尔基耶黑松、苏格兰松和冷杉林分发育阶段对土壤碳氮储量的影响
研究了黑松(Pinus nigra Arnold.)、苏格兰松(Pinus sylvestris L.)和卡兹达冷杉(Abies nordmanniana subsp.ex Boiss) Coode et Cullen)的平均树体直径不同,在土耳其西北部的三个树种中,繁殖期(RS)=<8 厘米,树苗或树干期(SPS)= 8-19.9 厘米,大树干期(LPS)= 20-35.9 厘米,中等木质期(MWS)= 36-51.9 厘米。共收集了 216 份土壤样本,分析了 pH 值、有机质、容重、最大持水量、碳和氮浓度,并计算了 SOC 和 TN 储量。SOC 和 TN 储量在四个林分发展阶段等级之间存在显著差异。由于黑色林分(BPLPS 和 BPMWS)直径的增加,0-30 厘米处的 SOC 储量明显增加。所有林分发展阶段的 SOC 储量在大杆(44.94 兆克/公顷)时达到峰值,随着树苗或树杆(37.71 兆克/公顷)被中材林分(30.17 兆克/公顷)取代而下降,苏格兰松在林分发展的繁殖阶段出现了低点(27.94 兆克/公顷)。土壤深度为 0-30 厘米的 TN 储量介于 1.66 至 6.46 毫克/公顷之间。TN 储量最高的是 SPSPS(6.46 毫克/公顷)和 FirRS(5.48 毫克/公顷),最低的是 BPLPS(1.66 毫克/公顷)。结果表明,在所有树种的不同林分发展阶段,土壤都是碳和氮的主要储存地。
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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