广西主要森林土壤有机碳空间分布及其影响因素

doi:10.17521/cjpe.2015.0199

植物生态学报 ›› 2016, Vol. 40 ›› Issue (4): 282-291.DOI: 10.17521/cjpe.2015.0199

广西主要森林土壤有机碳空间分布及其影响因素

杜虎^1,², 曾馥平^1,^2,^*(), 宋同清^1,², 温远光³, 李春干^3,⁴, 彭晚霞^1,², 张浩^1,², 曾昭霞^1,²

¹中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室, 长沙 410125
²中国科学院环江喀斯特生态系统观测研究站, 广西环江 547100
³广西大学林学院, 南宁 530004
⁴广西林业勘测设计院, 南宁 530004

收稿日期:2015-06-03 接受日期:2015-12-27 出版日期:2016-04-29 发布日期:2016-04-30
通讯作者: 曾馥平
基金资助:
中国科学院战略性先导科技专项(XDA05050205和XDA05070404)和国家自然科学基金(31370485、31370623和31400412)

Spatial pattern of soil organic carbon of the main forest soils and its influencing factors in Guangxi, China

Hu DU^1,², Fu-Ping ZENG^1,^2,^*(), Tong-Qing SONG^1,², Yuan-Guang WEN³, Chun-Gan LI^3,⁴, Wan-Xia PENG^1,², Hao ZHANG^1,², Zhao-Xia ZENG^1,²

¹Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China

²Huanjiang Observation and Research Station of Karst Ecosystem, Chinese Academy of Sciences, Huanjiang, Guangxi 547100, China

³Forestry College of Guangxi University, Nanning 530004, China

⁴Guangxi Forest Inventory & Planning Institute, Nanning 530004, China

Received:2015-06-03 Accepted:2015-12-27 Online:2016-04-29 Published:2016-04-30
Contact: Fu-Ping ZENG

摘要/Abstract

摘要：

为阐明广西森林土壤有机碳密度分布格局及其主要影响因素, 基于森林资源清查资料和345个调查样地的土壤数据, 估算了广西主要森林土壤有机碳储量, 采用地统计学方法描绘了土壤有机碳密度的空间分布, 并利用主成分分析和逐步回归分析方法分析了影响土壤有机碳密度的主要因子。结果表明: 广西主要森林土壤有机碳储量(0-100 cm)达到1686.88 Tg, 土壤有机碳密度为124.70 Mg·hm^-2, 低于全国森林土壤平均水平。广西主要森林土壤有机碳密度最佳拟合模型为指数模型, 呈中等强度空间相关, Kriging插值显示土壤碳密度高值区在东北区域, 低值区在西北区域, 表现为喀斯特区域低、非喀斯特区域高的特点。广西主要森林土壤碳密度在不同植被类型和土壤类型下表现出一定差异, 其中竹林>落叶阔叶林>暖性针叶林>常绿落叶阔叶林>常绿阔叶林, 黄壤>红壤>赤红壤>石灰土。主成分分析和逐步回归分析结果发现土层深度、经纬度、海拔是影响广西森林土壤有机碳的主要因子, 其中以土层深度影响最大, 主要受岩溶地貌的影响。

关键词: 土壤有机碳, 空间异质性, 影响因子, 森林类型, 广西

Abstract:

Aims
Our objectives were to study the spatial distribution of soil organic carbon (SOC) density and its influencing factors in the main forest ecosystems in Guangxi.
Methods
A total of 345 sample plots were established in Guangxi, and the size of each plot was 50 m × 20 m. Based on the forest resource inventory data and field investigation, the SOC storage of the main forests in Guangxi was estimated. Geostatistics was applied to analyze the spatial pattern of SOC density and the main influencing factors on SOC density were also explored by principal component analysis and stepwise regression.
Important findings
The total SOC storage in the main forests in Guangxi was 1686.88 Tg, and the mean SOC density was 124.70 Mg·hm^-2, which is lower than that of China. The best fitted semivariogram model of SOC density was exponential model, and the spatial autocorrelation was medium. The contour map based on Kriging indicated that northeastern Guangxi had high SOC density and northwestern Guangxi had low SOC density, which corresponded to high SOC density in non-karst region and low SOC density in karst region. The SOC density followed the sequence of bamboo forest > deciduous broadleaf forest > warm coniferous forest > mixed evergreen and deciduous broadleaf forest > evergreen broadleaf forest, and yellow soil > red soil > lateritic red soil > limestone soil. The dominant environment factors affecting SOC density included soil depth, longitude, latitude, and altitude. Soil depth was the most influential factor, which was mainly attributed to the karst landscape.

Key words: soil organic carbon, spatial heterogeneity, influencing factor, forest type, Guangxi

杜虎, 曾馥平, 宋同清, 温远光, 李春干, 彭晚霞, 张浩, 曾昭霞. 广西主要森林土壤有机碳空间分布及其影响因素. 植物生态学报, 2016, 40(4): 282-291. DOI: 10.17521/cjpe.2015.0199

Hu DU, Fu-Ping ZENG, Tong-Qing SONG, Yuan-Guang WEN, Chun-Gan LI, Wan-Xia PENG, Hao ZHANG, Zhao-Xia ZENG. Spatial pattern of soil organic carbon of the main forest soils and its influencing factors in Guangxi, China. Chinese Journal of Plant Ecology, 2016, 40(4): 282-291. DOI: 10.17521/cjpe.2015.0199

导出引用管理器 EndNote|Ris|BibTeX

链接本文: https://www.plant-ecology.com/CN/10.17521/cjpe.2015.0199

https://www.plant-ecology.com/CN/Y2016/V40/I4/282

图/表 12

参考文献 22

1	Bao SD (2000). Soil Agricultural Chemistry Analysis. 3rd edn. China Agriculture Press, Beijing. (in Chinese)[鲍士旦 (2000). 土壤农化分析. 第三版. 中国农业出版社, 北京.]
2	Dixon RK, Brown S, Houghton RA, Solomon AM, Trexier MC, Wisniewski J (1994). Carbon pools and flux of global forest ecosystems.Science, 263, 185-190.
3	Du H, Song TQ, Peng WX, Wang KL, Liu L, Lu SY, Zeng FP (2011). Spatial heterogeneity of mineral compositions in surface soil in Mulun National Nature Reserve karst areas.Transactions of the Chinese Society of Agricultural Engineering, 27, 79-84. (in Chinese with English abstract)[杜虎, 宋同清, 彭晚霞, 王克林, 刘璐, 鹿士杨, 曾馥平 (2011). 木论喀斯特自然保护区表层土壤矿物质的空间异质性. 农业工程学报, 27, 79-84.]
4	Du H, Wang K, Peng W, Zeng F, Song T, Zhang H, Lu S (2014). Spatial heterogeneity of soil mineral oxide components in depression between karst hills, Southwest China.Chinese Geographical Science, 24, 163-179.
5	Du H, Zeng FP, Wang KL, Song TQ, Wen YG, Li CG, Peng WX, Liang HW, Zhu HG, Zeng ZX (2014). Dynamics of biomass and productivity of three major plantation types in southern China.Acta Ecologica Sinica, 34, 2712-2724. (in Chinese with English abstract)[杜虎, 曾馥平, 王克林, 宋同清, 温远光, 李春干, 彭晚霞, 梁宏温, 朱宏光, 曾昭霞 (2014). 中国南方3种主要人工林生物量和生产力的动态变化. 生态学报, 34, 2712-2724.]
6	Du YX, Song ZX, He CL, Zhou SX, Huang Q (2013). Organic carbon content and influencing factors of different forest soils in Jiujiang, Jiangxi Province.Chinese Journal of Soil Science, 44, 575-579. (in Chinese with English abstract)[杜有新, 宋祖祥, 何春林, 周赛霞, 黄强 (2013). 江西九江地区森林土壤有机碳含量及其影响因素. 土壤通报, 44, 575-579.]
7	Gao Y, Jin JW, Cheng JM, Su JS, Zhu RB, Ma ZR, Liu W (2014). Carbon sequestration status of forest ecosystems in Ningxia Hui Autonomous Region.Chinese Journal of Applied Ecology, 25, 639-646. (in Chinese with English abstract)[高阳, 金晶炜, 程积民, 苏纪帅, 朱仁斌, 马正锐, 刘伟 (2014). 宁夏回族自治区森林生态系统固碳现状. 应用生态学报, 25, 639-646.]
8	Huang CD, Zhang J, Yang WQ, Zhang GQ, Wang YJ (2009). Spatial distribution characteristics of forest organic carbon stock in Sichuan Province.Acta Ecologica Sinica, 29, 1217-1225. (in Chinese with English abstract)[黄从德, 张健, 杨万勤, 张国庆, 王永军 (2009). 四川森林土壤有机碳储量的空间分布特征. 生态学报, 29, 1217-1225.]
9	Li B, Fang X, Li Y, Xiang WH, Tian DL, Chen XY, Yan WD, Deng DH (2015). Dynamic properties of soil organic carbon in Hunan’s forests.Acta Ecologica Sinica, 35, 4265-4278. (in Chinese with English abstract)[李斌, 方晰, 李岩, 项文化, 田大伦, 谌小勇, 闫文德, 邓东华 (2015). 湖南省森林土壤有机碳密度及碳库储量动态. 生态学报, 35, 4265-4278.]
10	Li TT, Ji HB, Sun YY, Luo JM, Jiang YB, Wang LX (2007). Advances in researches on soil organic carbon storages and affecting factors in China. Journal of Capital Normal University (Natural Science Edition), 28, 93-97. (in Chinese with English abstract)[李甜甜, 季宏兵, 孙媛媛, 罗建美, 江用彬, 王丽新 (2007). 我国土壤有机碳储量及影响因素研究进展. 首都师范大学学报: 自然科学版, 28, 93-97.]
11	Luo YJ, Zhang XQ, Wang XK, Zhu JH, Hou ZH, Zhang ZJ (2009). Forest biomass estimation methods and their prospects. Scientia Silvae Sinicae, 45(8), 129-134. (in Chinese with English abstract)[罗云建, 张小全, 王效科, 朱建华, 侯振宏, 张治军 (2009). 森林生物量的估计方法及其研究进展. 林业科学, 45(8), 129-134.]
12	Nong SQ, Zhang W, Cai HD (2014). The dynamic change and main driving factors of forest resources in Guangxi from 1977 to 2010.Guangxi Forestry Science, 43, 171-178. (in Chinese with English abstract)[农胜奇, 张伟, 蔡会德 (2014). 1977-2010年广西森林资源变化动态及其主要驱动因素分析. 广西林业科学, 43, 171-178.]
13	Pan Y, Birdsey RA, Fang J, Houghton R, Kauppi PE, Kurz WA, Phillips OL, Shvidenklo A, Lewis SL, Canadell JG, Ciais P, Jackson RB, Pacala S, McGuire AD, Piao S, Rautiainen A, Sitch S, Hayes D (2011). A large and persistent carbon sink in the world’s forests.Science, 333, 988-993.
14	Shao YH, Pan JJ, Sun B (2005). Study on characteristics of soil organic carbon decompositions and carbon pool under different vegetations.Journal of Soil and Water Conservation, 9(3), 24-28. (in Chinese with English abstract)[邵月红, 潘剑君, 孙波 (2005). 不同森林植被下土壤有机碳的分解特征及碳库研究. 水土保持学报, 9(3), 24-28.]
15	Wang SQ, Zhou CH (1999). Estimating soil carbon reservoir of terrestrial ecosystem in China.Geographical Research, 18, 349-356. (in Chinese with English abstract)[王绍强, 周成虎 (1999). 中国陆地土壤有机碳库的估算. 地理研究, 18, 349-356.]
16	Wang XC, Qi G, Yu DP, Zhou L, Dai LM (2011). Carbon storage, density, and distribution in forest ecosystems in Jilin Province of Northeast China.Chinese Journal of Applied Ecology, 22, 2013-2020. (in Chinese with English abstract)[王新闯, 齐光, 于大炮, 周莉, 代力民 (2011). 吉林省森林生态系统的碳储量、碳密度及其分布. 应用生态学报, 22, 2013-2020.]
17	Wei YW, Yu DP, Wang QJ, Zhou L, Zhou WM, Fang XM, Gu XP, Dai LM (2013). Soil organic carbon density and its influencing factors of major forest types in the forest region of Northeast China.Chinese Journal of Applied Ecology, 24, 3333-3340. (in Chinese with English abstract)[魏亚伟, 于大炮, 王清君, 周莉, 周旺明, 方向民, 谷晓萍, 代力民 (2013). 东北林区主要森林类型土壤有机碳密度及其影响因素. 应用生态学报, 24, 3333-3340.]
18	Xie XL, Sun B, Zhou HZ, Li ZP (2004). Soil carbon stocks and their influencing factors under native vegetations in China.Acta Pedologica Sinica, 41, 687-699. (in Chinese with English abstract)[解宪丽, 孙波, 周慧珍, 李忠佩 (2004). 不同植被下中国土壤有机碳的储量与影响因子. 土壤学报, 41, 687-699.]
19	Xu YZ, Jiang MX (2015). Forest carbon pool characteristics and advances in the researches of carbon storage and related factors. Acta Ecologica Sinica, 35, 926-933. (in Chinese with English abstract)[徐耀粘, 江明喜 (2015). 森林碳库特征及驱动因子分析研究进展. 生态学报, 35, 926-933.]
20	Yu DS, Shi XZ, Sun WX, Wang HJ, Liu QH, Zhao YC (2005). Estimation of China soil organic carbon storage and density based on 1:1 000 000 soil database.Chinese Journal of Applied Ecology, 16, 2279-2283. (in Chinese with English abstract)[于东升, 史学正, 孙维侠, 王洪杰, 刘庆花, 赵永存 (2005). 基于1:100万土壤数据库的中国土壤有机碳密度及储量研究. 应用生态学报, 16, 2279-2283.]
21	Zhang Y, Shi XZ, Zhao YC, Yu DS, Wang HJ, Sun WX (2008). Estimates and affecting factors of soil organic carbon storages in Yunnan-Guizhou-Guangxi region of China.Environmental Science, 29, 2314-2319. (in Chinese with English abstract)[张勇, 史学正, 赵永存, 于东升, 王洪杰, 孙维侠 (2008). 滇黔桂地区土壤有机碳储量与影响因素研究. 环境科学, 29, 2314-2319.]
22	Zhou YR, Yu ZL, Zhao SD (2000). Carbon storage and budget of major Chinese forest types.Acta Phytoecolgica Sinica, 24, 518-522. (in Chinese with English abstract)[周玉荣, 于振良, 赵士洞 (2000). 我国主要森林生态系统碳贮量和碳平衡. 植物生态学报, 24, 518-522.]

林型(代码) Forest type (Code)	主要树种 Main tree species
松树林 Pine forest (A)	马尾松 Pinus massoniana
杉木林 China fir forest (B)	杉木 Cunninghamia lanceolata
桉树林 Eucalyptus forest (C)	尾叶桉 Eucalyptus urophylla、大桉 Eucalyptus grandis、巨尾桉 Eucalyptus grandis × urophylla
栎类林 Quercus forest (D)	青冈 Cyclobalanopsis glauca、麻栎 Quercus acutissima、白栎 Quercus fabri、大叶栎 Quercus griffithii
硬阔林 Hardwood forest (E)	格木 Erythrophleum fordii、蚬木 Excentrodendron hsienmu、金丝李 Garcinia paucinervis
软阔林 Softwood forest (F)	枫香树 Liquidambar formosana、喜树 Camptotheca acuminata、木荷 Schima superba、米老排 Mytilaria laosensis、栲树 Castanopsis taiwaniana
石山林 Forest in limestone (G)	青冈 Cyclobalanopsis glauca、肥牛树 Cephalomappa sinensis、香椿 Toona sinensis、任豆 Zenia insignis、金丝李 Garcinia paucinervis
竹林 Bamboo forest (H)	毛竹 Phyllostachys edulis、麻竹 Dendrocalamus latiflorus
八角林 Anise forest (I)	八角 Illicium verum
油茶林 Oil-tea forest (J)	油茶 Camellia oleifera

林型(代码) Forest type (Code)	主要树种 Main tree species
松树林 Pine forest (A)	马尾松 Pinus massoniana
杉木林 China fir forest (B)	杉木 Cunninghamia lanceolata
桉树林 Eucalyptus forest (C)	尾叶桉 Eucalyptus urophylla、大桉 Eucalyptus grandis、巨尾桉 Eucalyptus grandis × urophylla
栎类林 Quercus forest (D)	青冈 Cyclobalanopsis glauca、麻栎 Quercus acutissima、白栎 Quercus fabri、大叶栎 Quercus griffithii
硬阔林 Hardwood forest (E)	格木 Erythrophleum fordii、蚬木 Excentrodendron hsienmu、金丝李 Garcinia paucinervis
软阔林 Softwood forest (F)	枫香树 Liquidambar formosana、喜树 Camptotheca acuminata、木荷 Schima superba、米老排 Mytilaria laosensis、栲树 Castanopsis taiwaniana
石山林 Forest in limestone (G)	青冈 Cyclobalanopsis glauca、肥牛树 Cephalomappa sinensis、香椿 Toona sinensis、任豆 Zenia insignis、金丝李 Garcinia paucinervis
竹林 Bamboo forest (H)	毛竹 Phyllostachys edulis、麻竹 Dendrocalamus latiflorus
八角林 Anise forest (I)	八角 Illicium verum
油茶林 Oil-tea forest (J)	油茶 Camellia oleifera

林型 Forest type	幼龄林 Young forest (I)	中龄林 Middle-aged forest (II)	近熟林 Near-mature forest (III)	成熟林 Mature forest (IV)	过熟林 Over-mature forest (V)
松树林 Pine forest	96.66^bc	78.05^c	115.28^ab	136.52^a	116.10^ab
杉木林 China fir forest	149.24^b	117.50^b	206.62^a	205.13^a	204.73^a
桉树林 Eucalyptus forest	106.06^bc	141.56^ab	164.94^a	111.05^bc	87.19^c
栎类林 Quercus forest	72.26^ab	90.84^ab	84.39^ab	47.91^b	107.99^a
硬阔林 Hardwood forest	250.17^a	236.22^ab	120.55^b	325.94^a	335.27^a
软阔林 Softwood forest	124.29^c	117.33^bc	150.00^bc	294.54^a	178.55^b
石山林 Forest in limestone	56.98^a	67.76^a	51.75^a	71.09^a	81.21^a
竹林 Bamboo forest	138.09^a	187.65^a	—	128.19^a	—
八角林 Anise forest	87.23^b	147.85^a	—	123.96^ab	—
油茶林 Oil-tea forest	85.17^a	103.85^a	—	78.37^a	—

林型 Forest type	幼龄林 Young forest (I)	中龄林 Middle-aged forest (II)	近熟林 Near-mature forest (III)	成熟林 Mature forest (IV)	过熟林 Over-mature forest (V)
松树林 Pine forest	96.66^bc	78.05^c	115.28^ab	136.52^a	116.10^ab
杉木林 China fir forest	149.24^b	117.50^b	206.62^a	205.13^a	204.73^a
桉树林 Eucalyptus forest	106.06^bc	141.56^ab	164.94^a	111.05^bc	87.19^c
栎类林 Quercus forest	72.26^ab	90.84^ab	84.39^ab	47.91^b	107.99^a
硬阔林 Hardwood forest	250.17^a	236.22^ab	120.55^b	325.94^a	335.27^a
软阔林 Softwood forest	124.29^c	117.33^bc	150.00^bc	294.54^a	178.55^b
石山林 Forest in limestone	56.98^a	67.76^a	51.75^a	71.09^a	81.21^a
竹林 Bamboo forest	138.09^a	187.65^a	—	128.19^a	—
八角林 Anise forest	87.23^b	147.85^a	—	123.96^ab	—
油茶林 Oil-tea forest	85.17^a	103.85^a	—	78.37^a	—

环境因子 Environment factor	SOC密度 SOC density	年平均气温 Annual mean air temperature	年降水量 Annual precipitation	海拔 Altitude	经度 Longitude	纬度 Latitude	土层深度 Soil depth	pH值 pH value
年平均气温 Annual mean air temperature	-0.301^**
年降水量 Annual precipitation	0.093	-0.034
海拔 Altitude	0.170^**	-0.201^**	-0.245^**
经度 Longitude	0.285^**	-0.452^**	0.340^**	-0.420^**
纬度 Latitude	0.316^**	-0.817^**	-0.195^**	0.426^**	0.142^**
土层深度 Soil depth	0.484^**	0.054	0.292^**	-0.137^*	0.340^**	-0.123^*
pH值 pH value	-0.038	-0.033	-0.050	-0.044	0.015	0.036	-0.148^**
表层土壤SOC含量 SOC content of surface soil	0.373^**	-0.354^**	-0.069	0.207^**	0.078	0.370^**	-0.293^**	0.311^**

广西主要森林土壤有机碳空间分布及其影响因素

Spatial pattern of soil organic carbon of the main forest soils and its influencing factors in Guangxi, China

全文

PDF (PC)

可视化

被引次数

摘要/Abstract

引用本文

使用本文

图/表 12

参考文献 22

相关文章 15

编辑推荐

Metrics

本文评价

环境因子 Environment factor	第一主成分 Principal component 1	第二主成分 Principal component 2	第三主成分 Principal component 3
年平均气温 Annual mean air temperature	-0.927	0.070	-0.167
年降水量 Annual precipitation	-0.035	0.228	0.624
海拔 Altitude	0.402	0.116	-0.780
经度 Longitude	0.393	0.160	0.804
纬度 Latitude	0.910	-0.071	-0.201
土层深度 Soil depth	-0.001	0.893	0.259
pH值 pH value	0.189	-0.896	-0.023
表层土壤SOC含量 SOC content of surface soil	0.517	-0.402	-0.032
方差贡献率 Variance contribution	28.845	23.300	22.270
累计贡献率 Accumulative contribution (%)	28.845	52.146	74.416

[1]	秦文宽, 张秋芳, 敖古凯麟, 朱彪. 土壤有机碳动态对增温的响应及机制研究进展[J]. 植物生态学报, 2024, 48(4): 403-415.
[2]	陈颖洁, 房凯, 秦书琪, 郭彦军, 杨元合. 内蒙古温带草地土壤有机碳组分含量和分解速率的空间格局及其影响因素[J]. 植物生态学报, 2023, 47(9): 1245-1255.
[3]	张英, 张常洪, 汪其同, 朱晓敏, 尹华军. 氮沉降下西南山地针叶林根际和非根际土壤固碳贡献差异[J]. 植物生态学报, 2023, 47(9): 1234-1244.
[4]	冯继广, 张秋芳, 袁霞, 朱彪. 氮磷添加对土壤有机碳的影响: 进展与展望[J]. 植物生态学报, 2022, 46(8): 855-870.
[5]	甘子莹, 王浩, 丁驰, 雷梅, 杨晓刚, 蔡敬琰, 丘清燕, 胡亚林. 亚热带森林不同植物及器官来源的可溶性有机质输入对土壤激发效应的影响及其作用机理[J]. 植物生态学报, 2022, 46(7): 797-810.
[6]	白悦, 刘晨, 黄月, 董亚楠, 王露. 科尔沁沙质草地植物群落高度空间异质性对不同放牧方式的响应[J]. 植物生态学报, 2022, 46(4): 394-404.
[7]	郑周涛, 张扬建. 1982-2018年青藏高原水分利用效率变化及归因分析[J]. 植物生态学报, 2022, 46(12): 1486-1496.
[8]	孙建, 王毅, 刘国华. 青藏高原高寒草地地上植物碳积累速率对生态系统多功能性的影响机制[J]. 植物生态学报, 2021, 45(5): 496-506.
[9]	董利军, 李金花, 陈珊, 张瑞, 孙建, 马妙君. 若尔盖湿地高寒草甸退化过程中土壤有机碳含量变化及成因分析[J]. 植物生态学报, 2021, 45(5): 507-515.
[10]	王奕丹, 李亮, 刘琪璟, 马泽清. 亚热带6个典型树种吸收细根寿命与形态属性格局[J]. 植物生态学报, 2021, 45(4): 383-393.
[11]	胡宗达, 刘世荣, 罗明霞, 胡璟, 刘兴良, 李亚非, 余昊, 欧定华. 川西亚高山不同演替阶段天然次生林土壤碳氮含量及酶活性特征[J]. 植物生态学报, 2020, 44(9): 973-985.
[12]	罗斯生, 罗碧珍, 魏书精, 胡海清, 李小川, 吴泽鹏, 王振师, 周宇飞, 钟映霞. 中度强度森林火灾对马尾松次生林土壤有机碳密度的影响[J]. 植物生态学报, 2020, 44(10): 1073-1086.
[13]	李娜, 张一鹤, 韩晓增, 尤孟阳, 郝翔翔. 长期不同植被覆盖对黑土团聚体内有机碳组分的影响[J]. 植物生态学报, 2019, 43(7): 624-634.
[14]	杨焕莹, 宋建达, 周焘, 金光泽, 姜峰, 刘志理. 林分、土壤及空间因子对谷地云冷杉林叶面积指数空间异质性的影响[J]. 植物生态学报, 2019, 43(4): 342-351.
[15]	鲍勇, 高颖, 曾晓敏, 袁萍, 司友涛, 陈岳民, 陈滢伊. 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.