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Soil respiration in six temperate forests in China
Author(s) -
WANG CHUANKUAN,
YANG JINYAN,
ZHANG QUANZHI
Publication year - 2006
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2006.01234.x
Subject(s) - larix gmelinii , deciduous , environmental science , larch , betula platyphylla , forest ecology , soil respiration , terrestrial ecosystem , evergreen , temperate forest , temperate deciduous forest , ecosystem , temperate rainforest , forestry , pinus koraiensis , fraxinus , soil carbon , ecology , botany , soil water , geography , biology , soil science
Scaling soil respiration ( R S ), the major CO 2 source to the atmosphere from terrestrial ecosystems, from chamber‐based measurements to ecosystems requires studies on variations and correlations of R S from various biomes and across geographic regions. However, few studies on R S are available for Chinese temperate forest despite the importance of this forest in the national and global carbon budgets. In this study, we conducted 18‐month R S measurements during 2004–2005 in six temperate forest types, representing the typical secondary forest ecosystems across various site conditions in northeastern China: Mongolian oak ( Quercus mongolica Fisch.), aspen‐birch ( Populous davidiana Dode and Betula platyphylla Suk.), mixed deciduous (no dominant tree species), hardwood (dominated by Fraxinus mandshurica Rupr., Juglans mandshurica Maxim., and Phellodendron amurense Rupr.) forests, Korean pine ( Pinus koraiensis Sieb. et Zucc.) and Dahurian larch ( Larix gmelinii Rupr.) plantations. Our specific objectives were to: (1) explore relationships of R S against soil temperature and water content for the six forest ecosystems, (2) quantify annual soil surface CO 2 flux and its relations to belowground carbon storage, (3) examine seasonal variations in R S and related environmental factors, and (4) quantify among‐ and within‐ecosystem variations in R S . The R S was positively correlated to soil temperature in all forest types, and was significantly influenced by the interactions of soil temperature and water content in the pine, larch, and mixed deciduous forests. The sensitivity of R S to soil temperature at 10 cm depth ( Q 10 ) ranged from 2.61 in the oak forest to 3.75 in the aspen‐birch forests. The Q 10 tended to increase with soil water content until reaching a threshold, and then decline. The annual R S for the larch, pine, hardwood, oak, mixed deciduous, and aspen‐birch forests averaged 403, 514, 781, 785, 786, and 813 g C m −2 yr −1 , respectively. The annual R S of the broadleaved forests was 72% greater than that of the coniferous forests. The annual R S was positively correlated to soil organic carbon (SOC) concentration at O horizon ( R 2 =0.868) and total biomass of roots <0.5 cm in diameter ( R 2 =0.748). The coefficient of variation (CV) of R S among forest types averaged 25% across the 18‐month measurements. The CV of R S within plots varied from 20% to 27%, significantly ( P <0.001) greater than those among plots (9–15%), indicating the importance of the fine‐scaled heterogeneity in R S . This study emphasized that variations in soil respiration and potential sampling bias should be appropriately tackled for accurate soil CO 2 flux estimates.