期刊
SOIL BIOLOGY & BIOCHEMISTRY
卷 115, 期 -, 页码 346-356出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2017.09.004
关键词
Pyrogenic organic matter; Soil organic carbon; Mineralization; Stabilization; Respiration
类别
资金
- NSW Office of Environment and Heritage
- NSW Department of Primary Industries
Understanding the temperature sensitivity (Q(10)) of carbon (C) mineralization and priming of organic matter with different stabilities in a soil with aged biochar is required to enable better forecasting of biochar C sequestration potential under a warming climate. Here, we quantified the Q(10) and priming of C mineralization in a Vertisol from: (i) newly added labile organic matter (LOM) in the presence of aged biochars; and (ii) stable (aged) native soil organic matter in the presence of aged biochars or new LOM. We also quantified the Q(10) of aged biochar-C (BC) or aged soil organic carbon (SOC)+BC mineralization. Leaf litter from Eucalyptus saligna (a source of LOM) was applied at 4% w/w (delta C-13 38 parts per thousand) to a Vertisol (delta C-13 14 parts per thousand), containing either wood, leaf or poultry litter biochar (delta C-13 -25 to -28 parts per thousand), and nil biochar (control soil), previously incubated for 4 years. These biochar soil mixtures and the control soil, with or without LOM, were re-incubated at 10, 20, 30 and 40 C for 252 days. The results showed that 22-39% of LOM-C, 0.10-2.81% of aged BC and 2.4-77.0% of aged SOC mineralized across all temperatures over 252 days. The Qio of C mineralization increased with decreasing quality of C substrates in the soil, that is, LOM (1.17-1.21) < SOC (1.23-1.66), SOC + BC (1.23-1.60) < aged BC (1.92-2.26). Positive priming of SOC mineralization was greater by LOM (cE aged biochar), causing a significant decrease in the SOC Q(10) at all temperatures. The aged biochars resulted in negative priming of LOM-C mineralization, mainly at 10 degrees C, with no impact on the LOM Qio. The results suggest that global warming and tropical climates may lower the C sequestration potential of biochar, by reducing its capacity to slow the mineralization of LOM-C, while increasing the mineralization of native SOC. (C) 2017 Elsevier Ltd. All rights reserved.
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