
浏览全部资源
扫码关注微信
1. 福建林业职业技术学院 森林生态与碳汇计量研究所,福建,南平,353011
2. 福建省林业科学研究院,福建,福州,350012
3. 官庄国有林场,福建,三明,365504
4. 福建省罗卜岩自然保护区,福建,三明,365504
Published:2023
移动端阅览
Gao Wei, Chen Aiping, Huang Yongrong, et al. Effects of Three Forest Types on Soil Carbon and Nitrogen Storage and Enzyme Activity in Subtropical China[J]. Bulletin of Soiland Water Conservation, 2023, 43(1): 314-322.
Gao Wei, Chen Aiping, Huang Yongrong, et al. Effects of Three Forest Types on Soil Carbon and Nitrogen Storage and Enzyme Activity in Subtropical China[J]. Bulletin of Soiland Water Conservation, 2023, 43(1): 314-322. DOI: 10.13961/j.cnki.stbctb.20230220.008.
[目的] 探明森林类型对土壤碳氮含量和酶活性的影响,为亚热带针叶林改造过程中的树种选择和营林方式选择提供科学依据。[方法] 研究相同海拔高度和相近环境条件下的亚热带常绿阔叶林(米槠林)、常绿—落叶阔叶混交林(闽桦—闽楠林)和针叶林(马尾松林)3种森林类型对土壤碳氮储量和酶活性的影响。[结果] ①马尾松林的土壤总有机碳含量显著高于其他两种林分类型,土壤全氮含量与闽桦—闽楠林无显著差异,但二者均显著高于米槠林,马尾松林和闽桦—闽楠林的土壤氮储量和碳储量显著高于米槠林;马尾松林和闽桦—闽楠林的土壤可溶性有机碳含量显著高于米槠林。马尾松林的土壤可溶性有机氮含量显著小于米槠林和闽桦—闽楠林,米槠林和马尾松林的土壤微生物量碳氮含量均显著高于闽桦—闽楠林,3种林分的土壤铵态氮含量无显著差异,而闽桦—闽楠林的土壤硝态氮含量显著高于其他两种林分; ②米槠林的土壤脲酶活性显著高于闽桦—闽楠林。3种林分的土壤蔗糖酶活性差异显著,表现为:马尾松林>米槠林>闽桦—闽楠林,马尾松林和米槠林的土壤过氧化氢酶活性均显著高于闽桦—闽楠林。3种林分的土壤磷酸酶活性无显著差异,马尾松林的土壤β-葡糖糖苷酶活性显著大于米槠林和闽桦—闽楠林;RDA分析表明,影响3种林分土壤酶活性变化的因子主要为土壤全碳(解释率为59.5%)、全氮(解释率为11.0%)和硝态氮(解释率为14.6%)。[结论] 与米槠林相比,马尾松林和闽桦—闽楠林具有较高的土壤碳氮储量,土壤有机质的增加有利于提高土壤酶活性。
[Objective] The effects of forest types on soil carbon and nitrogen contents and enzyme activity were analyzed in order to provide a scientific basis for the selection of tree species and forest management methods in the transformation of subtropical coniferous forests. [Methods] The study evaluated data from a subtropical evergreen broad-leaved forest (Castanopsis carlesii forest)
an evergreen deciduous broad-leaved mixed forest (Betula fujianensis and Phoebe bournei mixed forest)
and a coniferous forest (Pinus massoniana forest) at the same altitude and similar environmental conditions. [Results] ① The total soil organic carbon content in the P. massoniana forest was significantly greater than in the other two forest types
and the total soil nitrogen content was not significantly different from that in the B. fujianensis and P. bournei mixed forest. However
both carbon and nitrogen contents were significantly greater than in the C. carlesii forest. The soil nitrogen and carbon reserves of the P. massoniana forest and the B. fujianensis and P. bournei mixed forest were significantly greater than the nitrogen and carbon reserves of the C. carlesii forest. The soil soluble organic carbon contents in the P. massoniana forest and the B. fujianensis and P. bournei mixed forest were significantly greater than in the C. carlesii forest. The soil soluble organic nitrogen content in the P. massoniana forest was significantly less than in the C. carlesii forest and the B. fujianensis and P. bournei mixed forest. The soil microbial biomass carbon and nitrogen contents in the C. carlesii forest and the P. massoniana forest were significantly greater than in the B. fujianensis and P. bournei mixed forest. There were no significant differences in the soil ammonium nitrogen contents among the three forest stands. However
the soil nitrate nitrogen content in the B. fujianensis and P. bournei mixed forest was significantly greater than in the other two forest types. ② The soil urease activity in the C. carlesii forest was significantly greater than in the B. fujianensis and P. bournei mixed forest. There were significant differences in soil invertase activities among the three stands
and the differences in activity followed the order of P. massoniana forest > C. carlesii forest > B. fujianensis and P. bournei mixed forest. The soil catalase activities in the P. massoniana forest and the C. carlesii forest were significantly greater than in the B. fujianensis and P. bournei mixed forest. There was no significant difference in soil phosphatase activity among the three forest stands. Soil β-glucosidase activity in the P. massoniana forest was significantly greater than in the C. carlesii forest and the B. fujianensis and P. bournei mixed forest. RDA analysis showed that the main factors affecting the change of soil enzyme activity in the three forests were total soil carbon (explanation rate of 59.5%)
total nitrogen (explanation rate of 11.0%)
and nitrate nitrogen (explanation rate of 14.6%). [Conclusion] The P. massoniana forest and the B. fujianensis and P. bournei mixed forest had greater soil carbon and nitrogen storage values than observed for the C. carlesii forest under the same disturbance background. The increased soil organic matter was conducive to increase soil enzyme activity.
Houghton R A. Balancing the global carbon budget [J]. Annual Review of Earth and Planetary Sciences, 2007,35:313-347.
阮超越,刘小飞,吕茂奎,等.杉木人工林凋落物添加与去除对土壤碳氮及酶活性的影响[J].土壤学报,2020,57(4):954-962.
Gao Wei, Huang Shide, Huang Yongrong, et al. Effects of tree species on soil carbon and nitrogen stocks in a coastal sand dune of southern subtropical China [J]. International Journal of Plant Research, 2019,32(2):142-150.
Gao Wei, Huang Zhiqun, Ye Gongfu, et al. Effects of forest cover types and environmental factors on soil respiration dynamics in a coastal sand dune of subtropical China [J]. Journal of Forestry Research, 2018,29(6):1645-1655.
王敬,李贤伟,荣丽,等.森林土壤氮贮量及氮素输入过程研究进展[J].世界林业研究,2008,21(1):14-19.
李若南,楚海燕,李一清,等.森林转换对不同土层土壤碳氮含量及储量的影响[J].亚热带资源与环境学报,2019,14(1):23-29.
杨萌,李永夫,李永春,等.集约经营对毛竹林土壤碳氮库及酶活性的影响[J].应用生态学报,2016,27(11):3455-3462.
鲍勇,高颖,曾晓敏,等.中亚热带3种典型森林土壤碳氮含量和酶活性的关系[J].植物生态学报,2018,42(4):508-516.
刘爽,王雅,刘兵兵,等.晋西北不同土地管理方式对土壤碳氮、酶活性及微生物的影响[J].生态学报,2019,39(12):4376-4389.
刘骏,薛莉,田地,等.森林转化对乔木地上部分与土壤的碳氮储量及分配格局的影响[J].生态学杂志,2018,37(10):3047-3052.
高伟,林捷,黄石德,等.南亚热带海岸沙地不同树种叶片化学计量学季节动态研究[J].热带作物学报,2018,39(11):2304-2312.
Wang Q K, Wang S L. Soil organic matter under different forest types in Southern China [J]. Geoderma,2007,142(3/4):349-356.
Wang Hui, Liu Shirong, Mo Jiangming, et al. Soil organic carbon stock and chemical composition in four plantations of indigenous tree species in subtropical China [J]. Ecological Research, 2010,25(6):1071-1079.
Augusto L, Ranger J, Binkley D, et al. Impact of several common tree species of European temperate forests on soil fertility [J]. Annals of Forest Science, 2002,59(3):233-253.
Kasel S, Bennett L T. Land-use history, forest conversion, and soil organic carbon in pine plantations and native forests of south eastern Australia [J]. Geoderma, 2007,137(3/4):401-413.
Schulp C J E, Nabuurs G J, Verburg P H, et al. Effect of tree species on carbon stocks in forest floor and mineral soil and implications for soil carbon inventories [J]. Forest Ecology and Management, 2008,256(3):482-490.
Sever H, Makineci E. Soil organic carbon and nitrogen accumulation on coal mine spoils reclaimed with maritime pine (
Pinus pinaster
Aiton) in Agacli-Istanbul [J]. Environmental Monitoring and Assessment, 2009,155(1):273-280.
黄茂根.中亚热带三种森林类型凋落物现存量及碳氮储量[J].福建林业,2018(5):37-40.
高伟,黄石德,林建丽,等.亚热带3种森林类型的群落特征与物种多样性的耦合关系[J].热带作物学报,2021,42(6):1756-1763.
高伟,黄雍容,林建丽,等.濒危树种闽桦天然林优势种群种间相关性[J].林业科学,2021,57(10):1-14.
Joergensen R G. The fumigation-extraction method to estimate soil microbial biomass: Calibration of the
k
EC
value [J]. Soil Biology and Biochemistry, 1996,28(1):25-31.
Joergensen R G, Mueller T. The fumigation-extraction method to estimate soil microbial biomass: Calibration of the
k
EN
value [J]. Soil Biology and Biochemistry, 1996,28(1):33-37.
李振高,骆永明,滕应.土壤与环境微生物研究法[M].北京:科学出版社,2008.
林先贵.土壤微生物研究原理与方法[M].北京:高等教育出版社,2010.
Eivazi F, Tabatabai M A. Glucosidases and galactosidases in soils [J]. Soil Biology and Biochemistry,1988,20(5):601-606.
Mueller K E, Eissenstat D M, Hobbie S E, et al. Tree species effects on coupled cycles of carbon, nitrogen, and acidity in mineral soils at a common garden experiment [J]. Biogeochemistry, 2012,111(1):601-614.
Sariyildiz T, Savaci G, Kravkaz I S. Effects of tree species, stand age and land-use change on soil carbon and nitrogen stock rates in northwestern Turkey [J]. iForest-Biogeosciences and Forestry, 2016,9(1):165-170.
林思祖,林开敏,吴擢溪.炼山对杉木人工幼林养分流失影响的定量研究[J].自然资源学报,1997,12(3):243-249.
马祥庆,何智英,俞新妥.不同林地清理方式对杉木人工林地力的影响[J].林业科学,1995,31(6):485-490.
杨玉盛,何宗明,马祥庆,等.论炼山对杉木人工林生态系统影响的利弊及对策[J].自然资源学报,1997,12(2):153-159.
杨玉盛,俞新妥,何智英,等.Ⅱ炼山初期土壤肥力变化初步研究[J].福建林学院学报,1989,9(3):248-255.
郑兴蕊,王克勤,宋娅丽,等.滇中亚高山不同森林土壤酶活性对模拟N沉降的响应[J].林业科学研究,2021,34(2):50-62.
王兵,刘国彬,薛萐.退耕地养分和微生物量对土壤酶活性的影响[J].中国环境科学,2010,30(10):1375-1382.
于镇华,李彦生,金剑,等.不同施肥措施对农田黑土剖面土壤酶活性特征的影响[J].土壤与作物,2018,7(3):276-283.
孙文颖,马维伟,李广,等.尕海湿地植被退化过程中土壤蔗糖酶和淀粉酶活性的动态特征[J].草地学报,2019,27(1):88-96.
邓欧平,李翰,熊雷,等.秸秆、猪粪混施对麦田根际土壤过氧化氢酶与蔗糖酶活性的影响[J].土壤,2018,50(1):86-92.
谢洪宝,于贺,陈一民,等.秸秆深埋对不同氮肥水平土壤蔗糖酶活性的影响[J].中国农学通报,2021,37(24):79-83.
李冰,李玉双,陈琳,等.沈北新区不同土地利用类型土壤过氧化氢酶活性特征及其影响因素分析[J].沈阳大学学报(自然科学版),2019,31(6):465-473.
0
Views
548
下载量
0
CSCD
Publicity Resources
Related Articles
Related Author
Related Institution
京公网安备11010802024621