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Storage and Stability of Soil Organic Carbon in Two Temperate Forests in Northeastern China

文献类型： 外文期刊

作者： Liu, Dongwei 1 ; Li, Shanlong 1 ; Zhu, Weixing 1 ; Wang, Yongyang 7 ; Zhang, Shasha 8 ; Fang, Yunting 1 ;

作者机构： 1.Chinese Acad Sci, Inst Appl Ecol, CAS Key Lab Forest Ecol & Management, Shenyang 110016, Peoples R China

2.Natl Observat & Res Stn, Qingyuan Forest CERN, Shenyang 110016, Peoples R China

3.Key Lab Isotope Tech & Applicat, Shenyang 110016, Peoples R China

4.Key Lab Terr Ecosyst Carbon Neutral, Shenyang 110016, Peoples R China

5.Jilin Acad Agr Sci, Inst Agr Resource & Environm, Changchun 130033, Peoples R China

6.SUNY Binghamton, Dept Biol Sci, Binghamton, NY 13902 USA

7.Guangdong Univ Technol, Minist Educ, Key Lab City Cluster Environm Safety & Green Dev, Guangzhou 510006, Peoples R China

8.Univ Vienna, Dept Microbiol & Ecosyst Sci, Div Terr Ecosyst Res, A-1090 Vienna, Austria

关键词： soil carbon; stability; aggregates; mineral association; land use change

期刊名称：LAND （ 影响因子：3.9； 五年影响因子：4.0 ）

ISSN：

年卷期： 2023 年 12 卷 5 期

页码：

收录情况： SCI

摘要： Forests worldwide store large quantities of carbon (C), particularly in soils as soil organic C (SOC). In northeastern China, two dominant forest types, secondary mixed forest (MF) and larch plantation forest (LF), cover extensive areas. However, we lack an understanding of the patterns and the mechanisms of SOC storage and stabilization in MF and LF, especially in deep soil layers. This research aims to illustrate the vertical distribution and mineral protection of SOC over soil depth; we also used d(13)C values of soil fractions to evaluate SOC stability. Samples from the surface litter (O-i), organic layer (Oa+e), and 0-40 cm mineral soils were collected from both MF and LF plots. We used two different methods to separate bulk soils into distinguished fractions: (1) macro- and micro-aggregates and the non-aggregated fraction, and (2) particulate organic matter (POM) and mineral-associated organic matter (MAOM). The C concentrations, C stocks, and d(13)C of all soil fractions were determined. Our findings were as follows: (1) SOC was mainly stored in mineral soils and was 13.6% lower in LF (8609 +/- 1180 g C m(-2)) than MF (9969 +/- 2084 g C m(-2)). (2) In both MF and LF, the SOC stock was mainly stored in aggregates (averaged 92.7%); macroaggregates dominated in the surface layers (Oa+e layer and 0-10 cm) but microaggregates dominated in the deep layers (10-20 cm and 20-40 cm). In mineral soils, MAOM was the dominant fraction of the C stock (averaged 81.6%). (3) The proportion of C distributed in microaggregates and MAOM increased from Oa+e to the 20-40 cm layer. (4) The C/N ratios and d(13)C values of MAOM were smaller and heavier compared to those of POM. Our study demonstrated that in both forests, aggregate formation and mineral association predominantly contributed to SOC storage, and large stocks of SOC were distributed in the deep soil. The increasing proportion of SOC in microaggregates and MAOM along the soil depth, most likely derived from microbial turnover and microbial necromass, influenced SOC stability in both forest types.

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