Details
| Originalsprache | Englisch |
|---|---|
| Aufsatznummer | 2215 |
| Seiten (von - bis) | 2215 |
| Fachzeitschrift | Scientific reports |
| Jahrgang | 15 |
| Ausgabenummer | 1 |
| Publikationsstatus | Veröffentlicht - 17 Jan. 2025 |
Abstract
Soil salinization becomes serious under climate change and human activities. Although the residue decomposition contributes lots to soil carbon storage and fertility, the decomposition process and microbial mechanisms on saline-alkali soils are still vague facing climate change. We measured the mass loss of residue (0, 4, 8, 15, 30, 60 and 90 days), CO 2 emission (every two days), and the microbial community structure (0, 4, 15 and 90 days) by using the litter bag method, gas chromatography and high-throughput sequencing technology during the residue decomposition (90 days) in a saline-alkali soil from the Tarim River Basin, China under various temperatures (15 °C, 25 °C, 35 °C) and soil moisture levels (20%, 40%, 60% water holding capacity). The decomposition stage consisted of fast (0-15 days) and slow periods (15-90 days). Using the double exponential equation, the decomposition rates of labile and recalcitrant components, the labile component and cumulative CO 2 emissions increased faster with increased moisture than with temperature. The Q 10 was greater at 15-25 °C than at 25-35 °C, which increased with the increased soil moisture in the leaf but with decreased soil moisture in the stem at 15-25 °C. Proteobacteria increased from 0 to 15 days on leaves (25-43%) and stems (25-29%) and showed no changes thereafter. Proteobacteria increased with increased soil moisture but decreased temperature. Actinomycetes was the opposite and more abundant on the stem than on the leaf. Bacteroidetes increased after 15 days and increased with increased soil moisture. Firmicutes were the main bacterial groups at 0-15 days, but decreased at 15-90 days (leaf: 44 - 15%, stem: 49 - 13%). In conclusion, warming, especially 15-25 °C, contributes to the decomposition of stems and wetting, especially 20-40% WHC, contributes to that of leaves within the first 15 days, afterwards wetting played an important role. Our results could also provide the adopting strategies for residue return to increase the soil carbon content while decreasing CO 2 emissions facing climate change.
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in: Scientific reports, Jahrgang 15, Nr. 1, 2215, 17.01.2025, S. 2215.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - The microbial mechanism of maize residue decomposition under different temperature and moisture regimes in a Solonchak
AU - Huang, Fan
AU - Zhang, Wan
AU - Xue, Lihua
AU - Razavi, Bahar
AU - Zamanian, Kazem
AU - Zhao, Xiaoning
N1 - © 2025. The Author(s).
PY - 2025/1/17
Y1 - 2025/1/17
N2 - Soil salinization becomes serious under climate change and human activities. Although the residue decomposition contributes lots to soil carbon storage and fertility, the decomposition process and microbial mechanisms on saline-alkali soils are still vague facing climate change. We measured the mass loss of residue (0, 4, 8, 15, 30, 60 and 90 days), CO 2 emission (every two days), and the microbial community structure (0, 4, 15 and 90 days) by using the litter bag method, gas chromatography and high-throughput sequencing technology during the residue decomposition (90 days) in a saline-alkali soil from the Tarim River Basin, China under various temperatures (15 °C, 25 °C, 35 °C) and soil moisture levels (20%, 40%, 60% water holding capacity). The decomposition stage consisted of fast (0-15 days) and slow periods (15-90 days). Using the double exponential equation, the decomposition rates of labile and recalcitrant components, the labile component and cumulative CO 2 emissions increased faster with increased moisture than with temperature. The Q 10 was greater at 15-25 °C than at 25-35 °C, which increased with the increased soil moisture in the leaf but with decreased soil moisture in the stem at 15-25 °C. Proteobacteria increased from 0 to 15 days on leaves (25-43%) and stems (25-29%) and showed no changes thereafter. Proteobacteria increased with increased soil moisture but decreased temperature. Actinomycetes was the opposite and more abundant on the stem than on the leaf. Bacteroidetes increased after 15 days and increased with increased soil moisture. Firmicutes were the main bacterial groups at 0-15 days, but decreased at 15-90 days (leaf: 44 - 15%, stem: 49 - 13%). In conclusion, warming, especially 15-25 °C, contributes to the decomposition of stems and wetting, especially 20-40% WHC, contributes to that of leaves within the first 15 days, afterwards wetting played an important role. Our results could also provide the adopting strategies for residue return to increase the soil carbon content while decreasing CO 2 emissions facing climate change.
AB - Soil salinization becomes serious under climate change and human activities. Although the residue decomposition contributes lots to soil carbon storage and fertility, the decomposition process and microbial mechanisms on saline-alkali soils are still vague facing climate change. We measured the mass loss of residue (0, 4, 8, 15, 30, 60 and 90 days), CO 2 emission (every two days), and the microbial community structure (0, 4, 15 and 90 days) by using the litter bag method, gas chromatography and high-throughput sequencing technology during the residue decomposition (90 days) in a saline-alkali soil from the Tarim River Basin, China under various temperatures (15 °C, 25 °C, 35 °C) and soil moisture levels (20%, 40%, 60% water holding capacity). The decomposition stage consisted of fast (0-15 days) and slow periods (15-90 days). Using the double exponential equation, the decomposition rates of labile and recalcitrant components, the labile component and cumulative CO 2 emissions increased faster with increased moisture than with temperature. The Q 10 was greater at 15-25 °C than at 25-35 °C, which increased with the increased soil moisture in the leaf but with decreased soil moisture in the stem at 15-25 °C. Proteobacteria increased from 0 to 15 days on leaves (25-43%) and stems (25-29%) and showed no changes thereafter. Proteobacteria increased with increased soil moisture but decreased temperature. Actinomycetes was the opposite and more abundant on the stem than on the leaf. Bacteroidetes increased after 15 days and increased with increased soil moisture. Firmicutes were the main bacterial groups at 0-15 days, but decreased at 15-90 days (leaf: 44 - 15%, stem: 49 - 13%). In conclusion, warming, especially 15-25 °C, contributes to the decomposition of stems and wetting, especially 20-40% WHC, contributes to that of leaves within the first 15 days, afterwards wetting played an important role. Our results could also provide the adopting strategies for residue return to increase the soil carbon content while decreasing CO 2 emissions facing climate change.
KW - Zea mays/metabolism
KW - Temperature
KW - Soil Microbiology
KW - Soil/chemistry
KW - Carbon Dioxide/metabolism
KW - Water/chemistry
KW - China
KW - Plant Leaves/chemistry
KW - Microbiota
KW - Climate Change
KW - Residue returning strategies
KW - Soil moisture
KW - CO2 emission
KW - Microorganisms
KW - Maize residue decomposition rate
KW - CO emission
UR - http://www.scopus.com/inward/record.url?scp=85216057245&partnerID=8YFLogxK
U2 - 10.1038/s41598-024-81292-3
DO - 10.1038/s41598-024-81292-3
M3 - Article
C2 - 39820291
VL - 15
SP - 2215
JO - Scientific reports
JF - Scientific reports
SN - 2045-2322
IS - 1
M1 - 2215
ER -