Abstract

The contribution of coarse woody debris (CWD) to forest carbon (C) and nitrogen (N) dynamics is poorly quantified. This study quantified total C and N content in CWD and estimated the decomposition rates of CWD at different decay stages in a 70-year-old naturally regenerated Korean red pine forest (Pinus densiflora S. et Z.). The N concentration in CWD varied among species and decay classes (from 0.15% to 0.82%), and exhibited a decreasing pattern in C:N ratios with increasing decay class. Total CWD amounts of 4.84 Mg C ha−1, dominated by pine logs (45.4%) and decay class III (40.0%), contained total N of 20.48 kg N ha−1, which was approximately nine times the N input from annual tree mortality. In addition, this study demonstrated that the decay constant rate k was 0.2497 for needle litter, whereas k values were 0.0438, 0.0693, 0.1054, and 0.1947 for red pine CWD of decay class I, II, III, and IV, respectively. The decay rates were significantly related to wood density, N concentration, and C:N ratio across the decay classes of CWD. The results suggest that the C:N ratio of CWD is a key factor affecting its decomposition.

Highlights

  • Coarse woody debris (CWD) and fine litter are critical components in forest carbon (C) and nitrogen (N) cycles [1,2]

  • The coarse woody debris (CWD) quantity and distribution is influenced by tree mortality and decomposition rate, which vary with climate, site characteristics, tree species, age, and disturbance dynamics [1,2,3,4,12,13,14,15]

  • Our results showed that the N concentration of CWD increases with increasing decay class, which is consistent with previous studies on decay class and time [13,25]

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Summary

Introduction

Coarse woody debris (CWD) and fine litter are critical components in forest carbon (C) and nitrogen (N) cycles [1,2]. CWD has been intensively examined because of its important role in forest C cycling [3,4,5]. CWD has been less studied in comparison to the contribution of fine litter to N and other nutrient cycles [6,7,8,9]. Global CWD contains approximately 36–72 Pg C, which may affect the total global forest C stock [10,11]. The CWD quantity and distribution is influenced by tree mortality and decomposition rate, which vary with climate, site characteristics, tree species, age, and disturbance dynamics [1,2,3,4,12,13,14,15].

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