不同林龄杉木人工林土壤团聚体及其有机碳变化特征

王心怡; 周聪; 冯文瀚; 陈金林; 蒋翔鹤

doi:10.13870/j.cnki.stbcxb.2019.05.019

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不同林龄杉木人工林土壤团聚体及其有机碳变化特征

更新时间：2025-03-12

- 不同林龄杉木人工林土壤团聚体及其有机碳变化特征
- Changes of Soil Aggregates and Its Organic Carbon in Chinese Fir Plantations with Different Forest Ages
- 水土保持学报 2019年33卷第5期页码：126-131
- 作者机构：
  
  南京林业大学现代林业协同创新中心,南京,210037
- 作者简介：
  
  [ "王心怡(1995-),女,硕士研究生,主要从事土壤改良利用研究。E-mail:wangxinyi0026@163.com" ]
- 基金信息：
  
  科技基础性工作专项（2014FY120700）江苏高校优势学科建设工程项目（PAPD）
- DOI：10.13870/j.cnki.stbcxb.2019.05.019
  中图分类号：
- 纸质出版：2019
- 稿件说明：
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王心怡, 周聪, 冯文瀚, 等. 不同林龄杉木人工林土壤团聚体及其有机碳变化特征[J]. 水土保持学报, 2019,33(5):126-131.

WANG Xinyi, ZHOU Cong, FENG Wenhan, et al. Changes of Soil Aggregates and Its Organic Carbon in Chinese Fir Plantations with Different Forest Ages[J]. 2019, 33(5): 126-131.
王心怡, 周聪, 冯文瀚, 等. 不同林龄杉木人工林土壤团聚体及其有机碳变化特征[J]. 水土保持学报, 2019,33(5):126-131. DOI： 10.13870/j.cnki.stbcxb.2019.05.019.

WANG Xinyi, ZHOU Cong, FENG Wenhan, et al. Changes of Soil Aggregates and Its Organic Carbon in Chinese Fir Plantations with Different Forest Ages[J]. 2019, 33(5): 126-131. DOI： 10.13870/j.cnki.stbcxb.2019.05.019.

摘要

土壤团聚体作为土壤结构性状的重要指标，对土壤孔隙、持水、保水等状况都有重要影响；土壤团聚体有机碳除了反映土壤固碳状况外，还与团聚体的稳定性能密切相关，研究森林土壤团聚体及其有机碳状况，旨在为合理利用土壤、提高人工林水源涵养功能提供依据。为此，以福建省洋口国有林场不同林龄杉木人工林（幼龄林、中龄林、成熟林）土壤为研究对象，通过野外调查、采样和室内分析，研究不同林龄杉木人工林土壤团聚体及其有机碳变化特征。结果表明：不同林龄杉木人工林对土壤团聚体及其有机碳具有重要影响，成熟林土壤大团聚体含量、团聚体平均重量直径（MWD）、团聚体有机碳含量及贡献率均分别大于幼龄林、中龄林；不同林龄的土壤水稳性团聚体均以大团聚体（粒径>0.25 mm）为主，占59.57%~80.97%，粒径<0.053 mm的仅占0.80%；土壤团聚体有机碳贡献率也以大团聚为主，其中以2~0.25 mm粒级贡献率最高，达58.43%；另外，土壤有机碳含量与团聚体MWD呈显著正相关，且具有明显的垂直变化特征，即随土层加深而下降。因此，土壤有机碳对团聚体稳定性具有积极作用，不同林龄土壤团聚体稳定性及有机碳变化规律为成熟林 > 幼龄林 > 中龄林。

Abstract

As an important indicator for soil structure

soil aggregates have a huge impact on soil porosity and water holding capacity. Soil aggregate organic carbon can not only reflect soil carbon sequestration capacity

but also be closely related to aggregate stability. Study on soil aggregates and organic carbon distribution characteristics in Chinese Fir plantations can provide theoretical basis for improving soil productivity and water use efficiency. In our research

soil samples were collected from Chinese Fir plantations with different forest ages (6

11 and 32 years)

which was located in Yangkou National Forest Farm

Fujian Province

China. The water-stable soil aggregate composition and organic carbon contents were measured. The results showed that forest age was very important in terms of soil aggregate and its organic carbon. Macro-aggregate contents (>0.25 mm)

MWD

organic carbon contents and its contribution of aggregates in mature forest were higher than that in young and middle forests. Water-stable macro-aggregates were the main part of soil aggregates

which accounting for about 59.57%~80.97%

while the aggregates with the partical size less than 0.053 mm only accounted for 0.80%. In terms of organic carbon contribution

macro-aggregates were the main contributor

and aggregates with the partical size 2~0.25 mm accounted for 58.43%. Furthermore

soil aggregate MWD and its carbon content had a typically vertical characteristic

decreasing with soil depth. A strong positive correction was found between aggregate MWD and organic carbon. Hence

organic carbon was beneficial for the stability of soil aggregate

and MWD and organic carbon contents of aggregate showed a trend as mature forest > young forest > middle forest.

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references

任镇江,罗友进,魏朝富.农田土壤团聚体研究进展[J].安徽农业科学,2011,39(2):1101-1105.

陈山,杨峰,林杉,等.土地利用方式对红壤团聚体稳定性的影响[J].水土保持学报,2012,26(5):211-216.

陈明霞,朱鹤健.漳州平原变性土粒径分布分形维数特征[J].科技导报,2010,28(23):86-90.

吴其聪,张丛志,张佳宝,等.不同施肥及秸秆还田对潮土有机质及其组分的影响[J].土壤,2015,47(6):1034-1039.

李金彪,刘广明,陈金林,等.不同物料掺拌对滨海重度盐土的改良效果研究[J].土壤通报,2017,48(6):14-18.

窦森,李凯,关松.土壤团聚体中有机质研究进展[J].土壤学报,2011,48(2):412-418.

国家林业局.中国森林资源报告:第八次全国森林资源清查[M].北京:中国林业出版社,2014:1-40.

刘恩科,赵秉强,梅旭荣,等.不同施肥处理对土壤水稳定性团聚体及有机碳分布的影响[J].生态学报,2010,30(4):1035-1041.

Wu Q C, Zhang C Z, Yu Z H, et al. Effects of elevated CO

and nitrogen addition on organic carbon and aggregates in soil planted with different rice cultivars[J]. Plant and Soil,2018,432(1/2):245-258.

Six J, Paustian K, Aggregate-associated soil organic matter as an ecosystem property and a measurement tool[J]. Soil Biology Biochemistry,2014,68(1):4-9.

温小荣,孟雪,刘俊,等.基于不同立地质量的杉林生物量遥感估测[J].林业科学研究,2016,29(14):494-499.

鲍士旦.土壤农化分析[M].3版.北京:中国农业出版社,1999:14-114.

Elliott E T, Cambardella C A. Physical separation of soil organic matter[J]. Agriculture Ecosystems & Environment,1991,34(1/4):407-419.

Bavel C H M V. Mean weight-diameter of soil aggregates as a statistical index of aggregation[J]. Soil Science Society of America Journal,1950,14(C):20-23.

Chivenge P, Vanlauwe B, Gentile R, et al. Organic resource quality influences short-term aggregate dynamics and soil organic carbon and nitrogen accumulation[J]. Soil Biology & Biochemistry,2011,43(3):657-666.

刘艳,查同刚,王伊琨,等.北京地区栓皮栎和油松人工林土壤团聚体稳定性及有机碳特征[J].应用生态学报,2013,24(3):607-613.

王连晓,史正涛,刘新有,等.不同林龄橡胶林土壤团聚体分布特征及其稳定性研究[J].浙江农业学报,2016,28(8):1381-1388.

张芸,李惠通,魏志超,等.不同发育阶段杉木人工林土壤有机质特征及团聚体稳定性[J]生态学杂志,2016,35(8):2029-2037.

王纪杰,鲍爽,梁关峰,等.不同林龄桉树人工林土壤有机碳的变化[J].四川林业科技,2015,36(4):92-95.

周纯亮,吴明.中亚热带四种森林土壤团聚体及其有机碳分布特征[J].土壤,2011,43(3):406-410.

刘宝,吴文峰,何盛强,等.不同林龄闽楠林土壤呼吸与碳储量研究[J].森林与环境学报,2018,38(4):49-56.

王肖楠,耿玉清,余新晓.栓皮栎林与油松林土壤有机碳及其组分的研究[J].土壤通报,2012,43(3):604-609.

曹小玉,李际平.不同龄组杉木人工林土壤有机碳贮量及分布特征[J].中南林业科技大学学报(自然科学版),2014,34(7):104-107.

张芸,李惠通,魏志超,等.不同发育阶段杉木人工林土壤有机质特征及团聚体稳定性[J].生态学杂志,2016,35(8):2029-2037.

郑子成,何淑勤,王永东,等.不同土地利用方式下土壤团聚体中养分的分布特征[J].水土保持学报,2010,24(3):170-174.

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