Changing rainfall frequency affects soil organic carbon concentrations by altering non-labile soil organic carbon concentrations in a tropical monsoon forest
- 1. School of Geographical Sciences, Guangzhou University, Guangzhou 510006 (China)
- 2. Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650 (China)
- 3. Institute of Water Resources Protection in Yangtze River, Wuhan 430051 (China)
- 4. Department of Ecology, South China Agricultural University, Guangzhou 510642 (China)
Description
Highlights: • This study was conducted to clarify effects of precipitation changes on SOC fractions. • Increased rainfall frequency and decreased rainfall amount were manipulated. • Rainfall frequency increase with the amount unaltered increased the SOC concentration. • The non-labile fraction contributed a substantial proportion to this increase. • Rainfall amount decrease by 50% did not significantly change the SOC concentration. Soil stores a substantial proportion of carbon (C), making it the greatest terrestrial C pool and pivotal to stabilizing the global climate system. Rainfall amounts and regimes have been changing in many places, but effects of precipitation changes on soil organic C (SOC) stabilization are not completely understood. Considerable attention has been focused on the consequences of changes in rainfall amounts, with rainfall regimes having been less studied. This study was conducted in a tropical climax forest to clarify the effects of rainfall changes on SOC fractions, with permanganate oxidation and density fractionations employed to divide the labile and non-labile SOC fractions. Two rainfall manipulation treatments, i.e., increased rainfall frequency with the total rainfall amount unchanged (IRF) and decreased rainfall amount by 50% with rainfall frequency unaltered (DRA), were conducted for two years, with ambient rainfall (AR) as the control. As a result, the IRF treatment increased the SOC concentration that mainly originated from increases in the non-labile SOC content. Relative to the AR control, the DRA treatment did not change the total SOC concentration although the labile SOC concentration increased. This typically is due to a small proportion of the labile fraction to the total SOC content. Our results suggest that this water-rich mature forest is resistant to rainfall amount changes to a great extent (e.g., decrease of 50% as in the present study) from the SOC stabilization perspective, while changes in rainfall frequency could exert more notable effects.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2018.07.035Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2018.07.035;
- PII
- S0048969718325166;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 644
- Journal Page Range
- p. 762-769
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53034410
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- ATMOSPHERIC PRECIPITATIONS; CARBON; CLIMATES; ECOLOGICAL CONCENTRATION; FORESTS; FRACTIONATION; MONSOONS; OXIDATION; PERMANGANATES; POLLUTION CONTROL; SOILS; WATER
- Descriptors DEC
- CHEMICAL REACTIONS; CONTROL; ELEMENTS; HYDROGEN COMPOUNDS; MANGANESE COMPOUNDS; NONMETALS; OXYGEN COMPOUNDS; SEPARATION PROCESSES; STORMS; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier B.V. All rights reserved.