Unexpected mechanism for glucose-primed soil organic carbon mineralization under an anaerobic aerobic transition

被引:10
作者
Dunham-Cheatham, Sarrah M. [1 ,2 ]
Zhao, Qian [3 ,4 ]
Obrist, Daniel [5 ]
Yang, Yu [2 ,3 ]
机构
[1] Univ Nevada, Dept Nat Resources & Environm Sci, 1664 N Virginia St,Mail Stop 186, Reno, NV 89557 USA
[2] Univ Nevada, Global Water Ctr, 1664 N Virginia St,Mail Stop 186, Reno, NV 89557 USA
[3] Univ Nevada, Dept Civil & Environm Engn, 1664 N Virginia St,Mail Stop 258, Reno, NV 89557 USA
[4] Pacific Northwest Natl Lab, Environm Mol Sci Lab, 3335 Innovat Blvd, Richland, WA 99354 USA
[5] Univ Massachusetts, Dept Environm Earth & Atmospher Sci, 220 Pawtucket St, Lowell, MA 01854 USA
关键词
Glucose; Iron reduction; Priming effect; Redox fluctuations; Reductive dissolution; Soil organic carbon; MICROBIAL BIOMASS; IRON REDUCTION; FOREST SOILS; TRACE AMOUNTS; MATTER; DYNAMICS; ACID; QUANTIFICATION; DECOMPOSITION; ACCUMULATION;
D O I
10.1016/j.geoderma.2020.114535
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Redox reactions are important for cycling of carbon (C) in soils frequently subject to fluctuations in redox conditions, such as wetland soils, which contribute around one third of the global terrestrial C reservoir. Priming effects (PE), induction of changes in C mineralization due to additions of energy-rich organic carbon (OC) substrates, have been largely ignored during redox transitions in current modelling and experimental efforts for evaluating C cycles. In this study, we investigated the effects of glucose input on the mineralization of soil OC during an anaerobic-aerobic transition. Substantially more soil OC was mineralized under aerobic conditions in samples that received glucose under preceding anaerobic conditions compared to controls that did not receive glucose and to samples that received glucose under aerobic-only conditions. Our results reveal a novel PE by which glucose indirectly primes the mineralization of soil OC by increasing the reductive release of iron oxide-associated OC under anaerobic conditions, followed by a dramatic positive PE when aerobic conditions are reestablished. Inclusion of this novel indirect priming mechanism is crucial for accurately predicting the contribution of atmospheric greenhouse gases from soils experiencing redox fluctuations (e.g., wetlands).
引用
收藏
页数:9
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