1. 南昌工程学院, 江西省退化生态系统修复与流域生态水文重点实验室,江西,南昌,330099
2. 汕头华侨经济文化合作试验区管委会,广东,汕头,515000
纸质出版:2023
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朱丽琴, 黄荣珍, 王金平, 等. 凋落物输入对木荷林土壤微团聚体有机碳及其化学结合形态的影响[J]. 水土保持通报, 2023,43(1):307-313.
Zhu Liqin, Huang Rongzhen, WangJinping, et al. Effects of Litter Input on Organic Carbon and Its Chemical-Bound Forms of Soil Microaggregate in Schima Superba Forest[J]. Bulletin of Soiland Water Conservation, 2023, 43(1): 307-313.
朱丽琴, 黄荣珍, 王金平, 等. 凋落物输入对木荷林土壤微团聚体有机碳及其化学结合形态的影响[J]. 水土保持通报, 2023,43(1):307-313. DOI: 10.13961/j.cnki.stbctb.20230220.006.
Zhu Liqin, Huang Rongzhen, WangJinping, et al. Effects of Litter Input on Organic Carbon and Its Chemical-Bound Forms of Soil Microaggregate in Schima Superba Forest[J]. Bulletin of Soiland Water Conservation, 2023, 43(1): 307-313. DOI: 10.13961/j.cnki.stbctb.20230220.006.
[目的] 探究地上凋落物、地下根系和菌根输入对红壤恢复林地土壤微团聚体的影响,为退化地进行森林恢复后土壤功能重建和生态系统碳循环提供依据。[方法] 以亚热带红壤侵蚀退化地恢复形成的典型阔叶林分木荷纯林为研究对象,设置无凋落物(CT)、菌根(M)、根系+菌根(RM)、地上+地下凋落物(LRM)和地上凋落物加倍(DLRM) 5种输入处理,对土壤微团聚体组成、有机碳及其化学结合形态进行分析。[结果] 木荷恢复林土壤微团聚体质量百分比、有机碳、钙键结合态有机碳(Ca-SOC)、铁铝键结合态有机碳〔Fe(Al)-SOC〕和Ca-SOC/SOC在不同处理间均无显著差异(p>0.05);相对于CT,LRM处理使20~50 μm和50~200 μm粒级微团聚体Fe(Al)-SOC/SOC分别降低了40.06%和46.67%(p<0.05)。土壤微团聚体质量百分比、有机碳、Ca-SOC和Fe(Al)-SOC均随粒级的增大而减小,有机碳及结合态有机碳趋于在较小粒级的微团聚体颗粒组(<20 μm)中富集。微团聚体Ca-SOC含量(0.55~1.28 g/kg)远低于Fe(Al)-SOC含量(6.88~13.34 g/kg),但其在不同粒级中的变化幅度大于Fe(Al)-SOC;Ca-SOC/SOC(1.54%~3.44%)亦小于Fe(Al)-SOC/SOC(16.75%~42.54%)。微团聚体质量百分比、有机碳、Ca-SOC和Fe(Al)-SOC两两之间呈极显著正相关关系(r=0.497~0.757,p<0.01)。[结论] 木荷恢复林土壤微团聚体及其有机碳受粒级的影响,对地上凋落物、地下根系和菌根的短期输入有所响应,但未达到显著水平,需要在更长的时间尺度上开展研究。
[Objective] The effects of changes in aboveground litter
underground roots
and mycorrhizal inputs on soil microaggregates of restored red soil forestland were analyzed in order to provide a basis for soil function reconstruction and understanding the ecosystem carbon cycle after forest restoration of degraded lands. [Methods] The study was conducted in a pure Schima superba forest
a typical broad-leaved forest recovered from eroded and degraded red soil in a subtropical region. Five input treatments were established: no litter (CT)
mycorrhiza (M)
root+mycorrhiza (RM)
aboveground+underground litter (LRM)
and double aboveground+underground litter (DLRM). The composition of soil microaggregates
organic carbon
and their chemically bound forms were analyzed. [Results] There were no significant differences in soil microaggregate mass percentage
organic carbon
Ca-SOC
Fe (Al)-SOC
and Ca-SOC/SOC among the different treatments (p>0.05). Compared with CT
LRM reduced Fe (Al)-SOC/SOC of microaggregates of size 20—50 μm and 50—200 μm by 40.06% and 46.67%
respectively (p<0.05). Soil microaggregate mass percentage
organic carbon
Ca-SOC
and Fe (Al)-SOC decreased as particle size increased
and organic carbon and bound organic carbon tended to be enriched in smaller particle size groups (<20 μm). The content of Ca-SOC in microaggregates (0.55—1.28 g/kg) was much lower than observed for Fe (Al)-SOC (6.88—13.34 g/kg)
but its variation range in different particle sizes was greater than that of Fe (Al)-SOC. The percentage of Ca-SOC/SOC (1.54%—3.44%) was also less than the percentage of Fe (Al)-SOC/SOC (16.75%—42.54%). Microaggregate mass percentage
organic carbon
Ca-SOC
and Fe (Al)-SOC were positively correlated (r=0.497—0.757
p<0.01). [Conclusion] Soil microaggregates and their organic carbon in a restored S. superba forest were affected by particle size. Both quantities responded to short-term inputs of aboveground litter
underground roots
and mycorrhiza
but did not reach a significant level
and therefore need to be studied over a longer time period.
Daly K R, Mooney S J, Bennett M J, et al. Assessing the influence of the rhizosphere on soil hydraulic properties using X-ray computed tomography and numerical modelling [J]. Journal of Experimental Botany, 2015,66(8):2305-2314.
黄荣珍,王金平,朱丽琴,等.杉木人工林土壤微团聚体中铁铝氧化物与微生物的分布及其关系[J].水土保持通报,2022,42(1):1-9.
Puget P, Chenu C, Balesdent J. Dynamics of soil organic matter associated with particle-size fractions of water-stable aggregates [J]. European Journal of Soil Science, 2000,51(4):595-605.
Six J,Elliott E T, Paustian K. Soil macroaggregate turnover and microaggregate formation: A mechanism for C sequestration under no-tillage agriculture [J]. Soil Biology and Biochemistry, 2000,32(14):2099-2103.
Kong A Y Y, Six J, Bryant D C, et al. The relationship between carbon input, aggregation, and soil organic carbon stabilization in sustainable cropping systems [J]. Soil Science Society of America Journal, 2005,69(4):1078-1085.
Volikov A B, Kholodov V A, Kulikova N A, et al. Silanized humic substances act as hydrophobic modifiers of soil separates inducing formation of water-stable aggregates in soils [J]. Catena, 2016,137:229-236.
Mikutta R, Kleber M, Torn M S, et al. Stabilization of soil organic matter: Association with minerals or chemical recalcitrance? [J]. Biogeochemistry, 2006,77(1):25-56.
雷敏,周萍,黄道友,等.长期施肥对水稻土有机碳分布及化学结合形态的影响[J].生态学杂志,2012,31(4):967-974.
陈晓旋,安婉丽,陈优阳,等.模拟酸雨对福州平原水稻田土壤化学结合态有机碳含量的影响[J].环境科学学报,2018,38(12):4796-4804.
吴铭,郑子成,李廷轩,等.不同植茶年限土壤微团聚体及有机碳分布特征[J].长江流域资源与环境,2014,23(7):1041-1047.
Rillig M C, Mummey D L. Mycorrhizas and soil structure [J]. The New Phytologist, 2006,171(1):41-53.
李燕燕,吴春生,刘亮英,等.退化红壤区植被恢复对土壤惰性碳和酶活性的影响[J].南昌工程学院学报,2020,39(3):44-47.
申思佳.亚热带不同森林植被恢复类型红壤微团聚体胶结物特征[D].江西南昌:南昌工程学院,2019.
Blaud A, Chevallier T, Virto I, et al. Bacterial community structure in soil microaggregates and on particulate organic matter fractions located outside or inside soil macroaggregates [J]. Pedobiologia, 2014,57(3):191-194.
国家林业局.LY/T 1237—1999森林土壤有机质的测定及碳氮比的计算[S].北京:1999年.
徐建民,赛夫,袁可能.土壤有机矿质复合体研究(Ⅸ):钙键复合体和铁铝键复合体中腐殖质的性状特征[J].土壤学报,1999,36(2):168-178.
Gentile R, Vanlauwe B, Six J. Litter quality impacts short-but not long-term soil carbon dynamics in soil aggregate fractions [J]. Ecological Applications, 2011,21(3):695-703.
魏强.亚热带典型森林凋落物输入对土壤有机碳累积和稳定性影响[D].福建福州:福建农林大学,2018.
陈冠陶,李顺,彭天驰,等.根系隔离和氮添加对湿性常绿阔叶林土壤碳氮组分的影响[J].应用与环境生物学报,2018,24(1):125-131.
Gill R A, Jackson R B. Global patterns of root turnover for terrestrial ecosystems [J]. New Phytologist, 2000,147(1):13-31.
钟思远,张静,褚国伟,等.南亚热带森林丛枝菌根真菌与土壤结构的关系[J].生态科学,2018,37(5):16-24.
Six J, Bossuyt H, Degryze S, et al. A history of research on the link between (micro)aggregates, soil biota, and soil organic matter dynamics [J]. Soil and Tillage Research, 2004,79(1):7-31.
李世朋,汪景宽,王开勇,等.土壤中钙键和铁/铝键结合的有机碳差异的比较[J].土壤通报,2003,34(6):501-504.
吴景贵.土壤颗粒的功能研究进展[J].吉林农业大学学报,2008,30(4):529-537.
王晟强,郑子成,李廷轩.四川茶园土壤微团聚体组成及其分形特征[J].林业科学,2014,50(9):10-17.
刘敏英,郑子成,李廷轩.不同植茶年限土壤团聚体的分布特征及稳定性研究[J].茶叶科学,2012,32(5):402-410.
周国华,贺灵,白金峰,等.安溪茶园土壤团聚体组成及其对元素分配的影响[J].中国地质,2016,43(2):628-637.
Jastrow J D. Soil aggregate formation and the accrual of particulate and mineral-associated organic matter [J]. Soil Biology and Biochemistry, 1996,28(4/5):665-676.
Bonnard P, Basile-Doelsch I, Balesdent J, et al. Organic matter content and features related to associated mineral fractions in an acid, loamy soil [J]. European Journal of Soil Science, 2012,63(5):625-636.
李雄飞,刘奋武,樊文华.五台山土壤水稳性团聚体Ca-SOC和Fe(Al)-SOC分布特征[J].水土保持学报,2018,32(2):198-203.
Zhou Ping, Song Guohan, Pan Genxing, et al. Role of chemical protection by binding to oxyhydrates in SOC sequestration in three typical paddy soils under long-term agro-ecosystem experiments from South China [J]. Geoderma, 2009,153(1/2):52-60.
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