Shuotian Lai, Wanting Dai, Fuzhong Wu, Biao Zhu, Xiangyin Ni
{"title":"亚热带森林中植物枯落物的易变碳释放及其对土壤有机质形成的影响","authors":"Shuotian Lai, Wanting Dai, Fuzhong Wu, Biao Zhu, Xiangyin Ni","doi":"10.1007/s11104-024-06978-z","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Background and aims</h3><p>Plant litter is a primary source of soil organic matter (SOM) in forests, but which carbon (C) fraction of plant litter contributes directly to SOM formation remains not fully understood.</p><h3 data-test=\"abstract-sub-heading\">Methods</h3><p>We conducted a 2.5-year microcosm experiment in a subtropical forest to assess C release during <i>Cinnamomum camphora</i> litter (leaf and twig) decomposition. We also evaluated the temporal changes in soil microbial biomass (phospholipid fatty acids, PLFAs), enzymatic activities and soil C fractions with or without litter input until the foliar litter is decomposed by approximately 80%.</p><h3 data-test=\"abstract-sub-heading\">Results</h3><p>Decomposition rates of total C, dissolved organic C, hot-water extractable C, non-structural C, soluble sugars and starch in foliar litter estimated by the first-order exponential model were 0.689, 2.310, 8.272, 1.032, 13.509 and 0.718 yr<sup>−1</sup>, respectively. For twig litter, these rates were 0.359, 4.085, 2.756, 0.847, 2.274 and 0.675 yr<sup>−1</sup>, respectively. The C inputs from decomposing litter increased soil PLFAs at early periods, but did not significantly change soil enzymatic activities. Although soil particulate and mineral-associated organic C were not changed significantly, litter C input significantly increased the concentrations of soil non-structural C, soluble sugars and starch, which corresponded to labile C release from decomposing litter.</p><h3 data-test=\"abstract-sub-heading\">Conclusion</h3><p>Our findings suggested that the short-term effect of litter input on SOM formation is primarily driven by labile C input from decomposing litter in this subtropical forest.</p>","PeriodicalId":20223,"journal":{"name":"Plant and Soil","volume":"6 1","pages":""},"PeriodicalIF":3.9000,"publicationDate":"2024-10-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Labile carbon release from plant litter and its effect on soil organic matter formation in a subtropical forest\",\"authors\":\"Shuotian Lai, Wanting Dai, Fuzhong Wu, Biao Zhu, Xiangyin Ni\",\"doi\":\"10.1007/s11104-024-06978-z\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<h3 data-test=\\\"abstract-sub-heading\\\">Background and aims</h3><p>Plant litter is a primary source of soil organic matter (SOM) in forests, but which carbon (C) fraction of plant litter contributes directly to SOM formation remains not fully understood.</p><h3 data-test=\\\"abstract-sub-heading\\\">Methods</h3><p>We conducted a 2.5-year microcosm experiment in a subtropical forest to assess C release during <i>Cinnamomum camphora</i> litter (leaf and twig) decomposition. We also evaluated the temporal changes in soil microbial biomass (phospholipid fatty acids, PLFAs), enzymatic activities and soil C fractions with or without litter input until the foliar litter is decomposed by approximately 80%.</p><h3 data-test=\\\"abstract-sub-heading\\\">Results</h3><p>Decomposition rates of total C, dissolved organic C, hot-water extractable C, non-structural C, soluble sugars and starch in foliar litter estimated by the first-order exponential model were 0.689, 2.310, 8.272, 1.032, 13.509 and 0.718 yr<sup>−1</sup>, respectively. For twig litter, these rates were 0.359, 4.085, 2.756, 0.847, 2.274 and 0.675 yr<sup>−1</sup>, respectively. The C inputs from decomposing litter increased soil PLFAs at early periods, but did not significantly change soil enzymatic activities. 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Labile carbon release from plant litter and its effect on soil organic matter formation in a subtropical forest
Background and aims
Plant litter is a primary source of soil organic matter (SOM) in forests, but which carbon (C) fraction of plant litter contributes directly to SOM formation remains not fully understood.
Methods
We conducted a 2.5-year microcosm experiment in a subtropical forest to assess C release during Cinnamomum camphora litter (leaf and twig) decomposition. We also evaluated the temporal changes in soil microbial biomass (phospholipid fatty acids, PLFAs), enzymatic activities and soil C fractions with or without litter input until the foliar litter is decomposed by approximately 80%.
Results
Decomposition rates of total C, dissolved organic C, hot-water extractable C, non-structural C, soluble sugars and starch in foliar litter estimated by the first-order exponential model were 0.689, 2.310, 8.272, 1.032, 13.509 and 0.718 yr−1, respectively. For twig litter, these rates were 0.359, 4.085, 2.756, 0.847, 2.274 and 0.675 yr−1, respectively. The C inputs from decomposing litter increased soil PLFAs at early periods, but did not significantly change soil enzymatic activities. Although soil particulate and mineral-associated organic C were not changed significantly, litter C input significantly increased the concentrations of soil non-structural C, soluble sugars and starch, which corresponded to labile C release from decomposing litter.
Conclusion
Our findings suggested that the short-term effect of litter input on SOM formation is primarily driven by labile C input from decomposing litter in this subtropical forest.
期刊介绍:
Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.