Spatio-temporal Characteristics of Soil Organic Carbon and Its Components in Typical tea Gardens in Hunan Province, China

doi:10.16258/j.cnki.1674-5906.2025.09.006

Ecology and Environmental Sciences ›› 2025, Vol. 34 ›› Issue (9): 1386-1397.DOI: 10.16258/j.cnki.1674-5906.2025.09.006

• Papers on Carbon Cycling and Carbon Emission Reduction • Previous Articles Next Articles

Spatio-temporal Characteristics of Soil Organic Carbon and Its Components in Typical tea Gardens in Hunan Province, China

LIU Qing¹^,²^,³(), GONG Yushun⁴, WANG Wei¹^,^*(), FANG Xiantao²^,³, WU Jinshui²^,³, SHEN Jianlin²^,³^,^*()

1. Resources and Environment College of Tibet Agriculture and Animal Husbandry College, Linzhi 860000, P. R. China
2. Institute of Subtropical Agricultural Ecology, Chinese Academy of Sciences/Key Laboratory of Subtropical Agricultural Ecological Process, Changsha 410125 P. R. China
3. Subtropical Agricultural Ecology Institute, Chinese Academy of Sciences/Changsha Agricultural Environment Observation and Research Station, Changsha 410125 P. R. China
4. Key Laboratory of Tea Science of Ministry of Education/Hunan Agricultural University, Changsha 410128, P. R. China

Received:2025-01-09 Online:2025-09-18 Published:2025-09-05

湖南典型茶园土壤有机碳及其组分时空特征

刘卿¹^,²^,³(), 龚雨顺⁴, 王伟¹^,^*(), 方贤滔²^,³, 吴金水²^,³, 沈健林²^,³^,^*()

1.西藏农牧学院资源与环境学院，西藏林芝 860000
2.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，湖南长沙 410125
3.中国科学院亚热带农业生态研究所/长沙农业环境观测研究站，湖南长沙 410125
4.湖南农业大学/茶学教育部重点实验室，湖南长沙 410128

通讯作者: *沈健林。E-mail: jlshen@isa.ac.cn；王伟。Email: xzwangwei@xza.edu.cn
作者简介:刘卿（1999年生），女，硕士研究生，研究方向为土壤碳循环。E-mail: 2111972814@qq.com
基金资助:
国家自然科学基金国际项目(42161144002);国家自然科学基金国际项目(U23A2009);中国科学院青年创新促进会优秀会员项目(Y2021102)

Abstract

Abstract:

Soil organic carbon pool is the largest carbon pool in terrestrial ecosystems. The quantity and quality of the soil organic carbon (SOC) pool determines the soil fertility status; thus, it is an important indicator for assessing soil quality. Tea plantations are one of the most important land use types in China, and the study of the composition and spatio-temporal variations of soil organic carbon pools in tea plantations is of great significance for accurately assessing regional carbon sinks. In this study, 12 typical tea-planting areas in Hunan Province, located in the subtropical zone, were selected as research subjects. Soil samples were collected from tea gardens with different planting years (0‒5 years, 10‒15 years, and over 20 years) in each area. The effects of planting year, soil depth, and tea ridge/row distribution on the content and composition characteristics of soil organic carbon in tea gardens were studied to provide a scientific basis for carbon sink assessment and fertility improvement in tea garden soils. The results showed that in typical tea gardens in Hunan Province, soil organic carbon contents in the 0‒20 cm and 20‒40 cm soil layers were 11‒48.88 g·kg⁻¹ and 1.79‒33.08 g·kg⁻¹, respectively. Soil organic carbon content showed an increasing trend with increasing planting years. The average soil organic carbon contents were 11.12 g·kg⁻¹, 12.89 g·kg⁻¹, and 17.91 g·kg⁻¹ in the 0‒40 cm soil layer with 0‒5 years, 10‒15 years, and over 20 years of planting, respectively. Soil organic carbon content of the tea ridges was significantly lower than that of the tea rows. The average soil organic carbon content in the 0-40 cm soil layer of tea rows were1.37 times that of the tea ridges. The dissolved organic carbon, microbial biomass carbon, particulate organic carbon, and mineral-associated organic carbon content in tea garden soil accounted for 1.21%, 1.31%, 25.71%, and 41.59% of soil organic carbon, respectively. The spatial and temporal variations of soil organic carbon components in tea plantations showed that with the increase in planting years, the content of soil organic carbon components increased, but the proportion of mineral-associated carbon in soil organic carbon decreased in tea gardens for more than 20 years, and the content of soil organic carbon components in tea rows was significantly higher than that in tea ridges. Random forest analysis showed that attitude was the most critical factor affecting the SOC content in tea gardens in Hunan Province. We estimated that the soil organic carbon storage reached 18.6×10⁶ t in the 0‒40 cm soil layer of tea gardens in Hunan Province. In summary, with increase soil depth, the content of soil organic carbon and its components in tea gardens decreased. The increase in planting years was beneficial to the accumulation of soil organic carbon and its components in tea gardens, which had the potential to act as carbon sinks.

Key words: tea-planting years, soil depth, tea garden, soil organic carbon, components of organic carbon

摘要： 土壤有机碳库是陆地生态系统中最大的碳库，其数量和质量决定土壤肥力状况，是评估土壤质量的重要指标。茶园是中国重要的土地利用类型，研究其土壤有机碳库组成与时空变化特征对精准评估区域碳汇具有重要意义。以位于亚热带区的湖南省12个典型植茶区为研究对象，采集不同种植年限（0-5、10-15、20年以上）茶园土壤，研究种植年限、土层深度、茶垄/茶行分布对茶园土壤有机碳质量分数及组成特征，以期为茶园土壤碳汇评估和茶园培肥提供科学依据。结果表明，湖南典型茶园在0-20 cm和20-40 cm土层土壤有机碳（SOC）质量分数分别为11-48.88 g·kg⁻¹和1.79-33.08 g·kg⁻¹，随种植年限的增加，土壤有机碳呈上升趋势，在0-5年茶园、10-15年茶园和20年以上茶园0-40 cm土层土壤有机碳平均质量分数分别为11.12、12.89、17.91 g·kg⁻¹。茶垄土壤有机碳质量分数显著低于茶行，茶行0-40 cm土层土壤有机碳平均质量分数是茶垄的1.37倍。茶园土壤可溶性有机碳、微生物量碳、颗粒有机碳和矿物结合态质量分数分别占到土壤有机碳的1.21%、1.31%、25.71%和41.59%，各土壤有机碳组分的时空变化特征为随着种植年限的延长，土壤有机碳组分质量分数增加，但矿物结合态有机碳占土壤有机碳比例到20年以上茶园开始降低，茶行土壤有机碳组分质量分数显著高于茶垄。随机森林分析显示影响区域茶园土壤有机碳及其组分质量分数的因子中最关键的因子是海拔，估算得到湖南省茶园表层0-40 cm土壤有机碳储量达18.6×10⁶ t。综上，随土层深度的增加，茶园土壤有机碳及其组分质量分数减少，植茶年限的增加有利于茶园土壤有机碳及其组分质量分数的累积，茶园具有一定的碳汇功能。

关键词: 植茶年限, 土层深度, 茶园, 土壤有机碳, 有机碳组分

CLC Number:

S153.6
X144

LIU Qing, GONG Yushun, WANG Wei, FANG Xiantao, WU Jinshui, SHEN Jianlin. Spatio-temporal Characteristics of Soil Organic Carbon and Its Components in Typical tea Gardens in Hunan Province, China[J]. Ecology and Environmental Sciences, 2025, 34(9): 1386-1397.

刘卿, 龚雨顺, 王伟, 方贤滔, 吴金水, 沈健林. 湖南典型茶园土壤有机碳及其组分时空特征[J]. 生态环境学报, 2025, 34(9): 1386-1397.

Figures/Tables 10

References 53

[1]	AWALE R, EMESON A M, MACHADO S, 2017. Soil organic carbon pools as early indicators for soil organic matter stock changes under different tillage practices in inland pacific northwest[J]. Frontiers in Ecology and Evolution, 5: 00096.
[2]	CAMBARDELLA C A, ELLIOTT E T, 1992. Particulate soil organic-matter changes across a grassland cultivation sequence[J]. Soil Science Society of America Journal, 56(3): 777-783.
[3]	CARVALHAIS N, FORKEL M, KHOMIK M, et al., 2014. Global covariation of carbon turnover times with climate in terrestrial ecosystems[J]. Nature, 514(7521): 213-217.
[4]	ESTEBAN G, JOBBÁGY, JACKSON R B, 2001. The distribution of soil nutrients with depth: Global patterns and the imprint of plants[J]. Biogeochemistry, 53(1): 51-77.
[5]	GHOSH B N, MEENA V S, SINGH R J, et al., 2019. Effects of fertilization on soil aggregation, carbon distribution and carbon management index of maize-wheat rotation in the north-western Indian Himalayas[J]. Ecological Indicators, 105: 415-424.
[6]	HIGASHI T, MU Y H, KOMATSUZAKI M, et al., 2014. Tillage and cover crop species affect soil organic carbon in Andosol, Kanto, Japan[J]. Soil and Tillage Research, 138: 64-72.
[7]	MAHECHA M D, REICHSTEIN M, CARVALHAIS N, et al., 2010. Global convergence in the temperature sensitivity of respiration at ecosystem level[J]. Science, 329(5993): 838-840. DOI PMID
[8]	MISHRA G, GIRI K, JANGIR A, et al., 2020. Projected trends of soil organic carbon stocks in Meghalaya state of Northeast Himalayas, India. Implications for a policy perspective[J]. Science of the Total Environment, 698: 134266.
[9]	PANG D B, CUI M, LIU Y G, et al., 2019. Responses of soil labile organic carbon fractions and stocks to different vegetation restoration strategies in degraded karst ecosystems of southwest China[J]. Ecological Engineering, 138: 391-402.
[10]	PUTZ S, GROENEVELD J, HENLE K, et al., 2014. Long-term carbon loss in fragmented Neotropical forests[J]. Nature Communications, 5: 5037. DOI PMID
[11]	TAVARES M L R, NAHAS E, 2014. Humic fractions of forest, pasture and maize crop soils resulting from microbial activity[J]. Brazilian Journal of Microbiology, 45(3): 963-969. PMID
[12]	WANG S Q, LI T X, ZHENG Z C, 2016. Effect of tea plantation age on the distribution of soil organic carbon and nutrient within micro-aggregates in the hilly region of western Sichuan, China[J]. Ecological Engineering, 90: 113-119.
[13]	WANG S Q, LI T X, ZHENG Z C, et al., 2019. Soil organic carbon and nutrients associated with aggregate fractions in a chrono sequence of tea plantations[J]. Ecological Indicators, 101: 444-452.
[14]	WIESMEIER M, SPÖRLEIN P, GEUß U, et al., 2012. Soil organic carbon stocks in southeast Germany (Bavaria) as affected by land use, soil type and sampling depth[J]. Global Change Biology, 18(7): 2233-2245.
[15]	WU J S, JOERGENSEN R G, POMMERENING B, et al., 1990. Measurement of soil microbial biomass C by fumigation-extraction: an automated procedure[J]. Acta Agrestia Sinica, 22(8): 1167-1169.
[16]	XU R K, ZHAO A Z, LI Q M, et al., 2003. Acidity regime of the Red Soils in a subtropical region of southern China under field conditions[J]. Geoderma, 115(1-2): 75-84.
[17]	白潇, 张世熔, 钟钦梅, 等, 2018. 中国东部区域土壤活性有机碳分布特征及其影响因素[J]. 生态环境学报, 27(9): 1625-1631. DOI
	BAI X, ZHANG S R, ZHONG Q M, et al., 2018. Distribution and influencing factors of soil labile organic carbon among the east area of China[J]. Ecology and Environmental Sciences, 27(9): 1625-1631.
[18]	鲍士旦, 2000. 土壤农化分析[M]. 北京: 中国农业出版社.
	BAO S D, 2000. Soil agrochemical analysis[M]. Beijing: China Agriculture Press.
[19]	常博然, 陈茹岚, 王彪, 等, 2024. 藏东南折拉山不同林分类型土壤有机碳及其组分分布特征[J]. 生态环境学报, 33(10): 1495-1505. DOI
	CHANG B R, CHEN R L, WANG B, et al., 2024. Characteristics of soil organic carbon and its component distribution in different forest stand types on mount zola in southeastern Tibet[J]. Ecology and Environmental Sciences, 33(10): 1495-1505.
[20]	陈仕栋, 2011. 湖南省土壤有机碳密度､储量的空间分布格局及其影响因子分析[D]. 长沙: 中南林业科技大学.
	CHEN S D, 2011. Spatial distribution pattern and influencing factors of soil organic carbon density and storage in Hunan Province[D]. Changsha: Central South University of Forestry and Technology.
[21]	陈新邦, 唐光木, 张云舒, 等, 2023. 不同类型外源碳添加对灰漠土土壤碳储量的影响[J]. 水土保持学报, 37(3): 330-335.
	CHEN X B, TANG G M, ZHANG Y S, et al., 2023. Effects of different types of exogenous carbon addition on soil carbon storage in grey desert soil[J]. Journal of Soil and Water Conservation, 37(3): 330-335.
[22]	杜磊, 2023. 川西低山丘陵区不同品种植茶土壤有机碳库稳定机制研究[D]. 雅安: 四川农业大学.
	DU L, 2023. Research on the stabilization mechanism of soil organic carbon pool of different tea varieties in the low hilly area of western Sichuan[D]. Ya’an: Sichuan Agricultural University.
[23]	杜雪, 王海燕, 邹佳何, 等, 2022. 长白山北坡云冷杉阔叶混交林土壤有机碳分布特征及其影响因素[J]. 生态环境学报, 31(4): 663-669. DOI
	DU X, WANG H Y, ZOU J H, et al., 2022. Distribution characteristics and influencing factors of soil organic carbon in spruce-fir broad-leaved mixed forest on north slope of Changbai Mountains[J]. Ecology and Environmental Sciences, 31(4): 663-669.
[24]	范利超, 韩文炎, 李鑫, 等, 2015. 茶园与相邻林地土壤有机碳及基础呼吸的垂直分布特征[J]. 农业环境科学学报, 34(6): 1149-1157.
	FAN L C, HAN W Y, LI X, et al., 2015. Vertical distribution of soil organic carbon and soil basal respiration in tea soil and adjacent woodland soil[J]. Journal of Agro-Environment Science, 34(6): 1149-1157.
[25]	高福丽, 夏建国, 2009. 不同种植年限茶园土壤有机无机复合状况及有机碳分布特征[J]. 水土保持学报, 23(1): 50-53, 72.
	GAO F L, XIA J G, 2009. Soil Organic-mineral complex status and distribution of organic carbon in tea gardens of different planting-year[J]. Journal of Soil and Water Conservation, 23(1): 50-53, 72.
[26]	韩文炎, 阮建云, 林智, 等, 2002. 茶园土壤主要营养障碍因子及系列茶树专用肥的研制[J]. 茶叶科学, 22(1): 70-74.
	HAN W Y, YUAN J Y, LIN Z, et al., 2002. The major nutritional limiting factors in tea soils and development of tea specialty fertilizer series[J]. Journal of Tea Science, 22(1): 70-74.
[27]	何平, 刘健, 余坤勇, 等, 2016. 南方竹林地土壤有机碳空间异质性研究[J]. 土壤通报, 47(2): 278-286.
	HE P, LIU J, YU K Y, et al., 2016. Research on spatial heterogeneity of soil organic carbon in the southern bamboo Forest[J]. Chinese Journal of Soil Science, 47(2): 278-286.
[28]	李世玉, 2010. 中国茶园生态系统碳平衡研究[D]. 杭州: 浙江大学.
	LI S Y, 2010. Carbon balance of tea plantation ecosystem in China[D]. Hangzhou: Zhejiang University.
[29]	李玮, 2015. 茶园土壤有机碳动态及其矿化特征研究[D]. 雅安: 四川农业大学.
	LI W, 2015. Research on the dynamics and mineralization characteristics of soil organic carbon in tea gardens[D]. Ya’an: Sichuan Agricultural University.
[30]	李亚, 张黎明, 陈瀚阅, 等, 2019. 基于Landsat遥感影像和1꞉50000土壤数据库的福州市耕地有机碳动态变化研究[J]. 中国生态农业学报(中英文), 27(4): 581-590.
	LI Y, ZHANG L M, CHEN H Y, et al., 2019. Research on the dynamic changes of cultivated land organic carbon in fuzhou city based on landsat remote sensing images and a 1꞉50000 soil database[J]. Chinese Journal of Eco-Agriculture (Chinese & English), 27(4): 581-590.
[31]	刘杰云, 邱虎森, 汤宏, 等, 2019. 生物质炭对双季稻水稻土微生物生物量碳、氮及可溶性有机碳氮的影响[J]. 环境科学, 40(8): 3799-3807.
	LIU J Y, QIU H S, TANG H, et al., 2019. Effects of biochar amendment on soil microbial biomass carbon, nitrogen and dissolved organic carbon, nitrogen in paddy soils[J]. Research of Environmental Sciences, 40(8): 3799-3807.
[32]	刘敏英, 2012. 植茶年限对土壤团聚体组成及其有机碳组分影响[D]. 雅安: 四川农业大学.
	LIU M Y, 2012. Effects of tea planting years on soil aggregate composition and organic carbon fractions[D]. Ya’an: Sichuan Agricultural University.
[33]	马红亮, 陈灿灿, 尹云锋, 等, 2024. 森林土壤不同粒径颗粒的碳矿化研究[J]. 土壤学报, 61(5): 1247-1259.
	MA H L, CHEN C C, YIN Y F, et al., 2024. Experimental study on carbon mineralization of different sizes particle in forest soils[J]. Acta Pedologica Sinica, 61(5): 1247-1259.
[34]	马维伟, 刘强, 李广, 等, 2024. 甘肃尕海湿地不同植被退化阶段土壤颗粒有机碳含量及动态[J/OL]. 土壤学报, 1-13 [2024-12-11]. http://kns.cnki.net/kcms/detail/32.1119.P.20240710.1259.006.html.
	MA W W, LIU Q, LI G, et al., 2024. Temporal dynamics and content of soil particulate organic of gahai wetland in gansu province during vegetation degradation succession[J/OL]. Acta Pedologica Sinica, 1-13 [2024-12-11]. http://kns.cnki.net/kcms/detail/32.1119.P.20240710.1259.006.html.
[35]	梅宇, 梁晓, 2024. 2023年我国茶叶产销及进出口形势分析[J]. 中国茶叶, 46(4): 18-26.
	MEI Y, LIANG X, 2024. Analysis of China’s Tea Production, Sales, Import and Export Situation in 2023[J]. China Tea Marketing Association, 46(4): 18-26.
[36]	申玲芝, 2024. 福建省安溪县茶园生态系统碳储量及碳汇潜力评估[D]. 福州: 福建农林大学.
	SHEN L Z, 2024. Carbon storage and carbon sink potential assessment of tea garden ecosystem in Anxi County, Fujian Province[D]. Fuzhou: Fujian Agriculture and Forestry University.
[37]	沈艳, 傅瓦利, 蓝家程, 等, 2012. 岩溶山地不同土地利用方式土壤颗粒有机碳和矿物结合态有机碳的分布特征[J]. 水土保持研究, 19(6): 1-6.
	SHEN Y, FU W L, LAN J C, et al., 2012. Distribution characteristics of soil particulate organic carbon and mineral-associated organic carbon of different land use in karst mountain[J]. Journal of Soil and Water Conservation, 19(6): 1-6.
[38]	汤宏, 沈健林, 刘杰云, 等, 2017. 稻秸的不同组分对水稻土微生物量碳氮及可溶性有机碳氮的影响[J]. 水土保持学报, 31(4): 264-271.
	TANG H, SHEN J L, LIU J Y, et al., 2017. Effects of different ingredients of rice straw incorporation on soil microbial biomass carbon, nitrogen and dissolved organic carbon, nitrogen in rice paddy soil[J]. Journal of Soil and Water Conservation, 31(4): 264-271.
[39]	王峰, 陈玉真, 尤志明, 等, 2015. 菌渣施用对茶园土壤有机碳含量及腐殖质组成的影响[J]. 福建农业学报, 30(2): 198-203.
	WANG F, CHEN Y Z, YOU Z M, et al., 2015. Effect of applying spent mushroom culture residues to tea garden on soil organic carbon content and humus composition[J]. Fujian Journal of Agricultural Sciences, 30(2): 198-203.
[40]	王晟强, 杜磊, 叶绍明, 2020. 桂南茶园土壤团聚体有机碳和养分对植茶年限的响应[J]. 应用生态学报, 31(3): 837-844. DOI
	WANG S Q, DU L, YE S M, et al., 2020. Responses of soil aggregate-associated organic carbon and nutrients to tea cultivation age in southern Guangxi, China[J]. Chinese Journal of Applied Ecology, 31(3): 837-844. DOI
[41]	王诗旖, 姚惠婷, 黄欣, 等, 2024. 茶园土壤有机碳库组分､影响因素及其稳定性研究进展[J]. 环境科学研究, 37(5): 1104-1115.
	WANG S Y, YAO H T, HUANG X, et al., 2024. Research progress on soil organic carbon pools components, influencing factors and stability of tea plantation[J]. Research of Environmental Sciences, 37(5): 1104-1115.
[42]	王义祥, 叶菁, 王成己, 等, 2014. 不同经营年限对柑橘果园土壤有机碳及其组分的影响[J]. 生态环境学报, 23(10): 1574-1580.
	WANG Y X, YE J, WANG C J, et al., 2014. Effect of different cultivation years on soil organic carbon pools in citrus orchards[J]. Ecology and Environmental Sciences, 23(10): 1574-1580.
[43]	吴彬, 徐晶晶, 成艳红, 等, 2021. 石灰施用对酸性土壤矿物结合有机碳形成的影响[J]. 中国农学通报, 37(21): 98-105. DOI
	WU B, XU J J, CHENG H Y, et al., 2021. Effects of lime application on the formation of mineral - associated organic carbon in acidic soils[J]. Chinese Agricultural Science Bulletin, 37(21): 98-105.
[44]	吴铭, 郑子成, 李廷轩, 等, 2014. 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, 23(7): 1041-1047.
	WU M, ZHENG Z C, LI T X, et al., 2014. Distribution characteristics of soil micro - aggregates and organic carbon under different tea - planting durations[J]. Resources and Environment in the Yangtze Basin, 23(7): 1041-1047.
[45]	冼海英, 肖波, 姚小萌, 等, 2024. 黄土高原生物结皮覆盖下表层土壤有机碳组分对模拟气候暖湿化的响应[J]. 应用生态学报, 36(1): 132-140.
	XIAN H Y, XIAO B, YAO X M, et al., 2024. Responses of organic carbon fractions in biocrust-covered surface soil to simulated warming and wetting on the Loess Plateau, Northwest China[J]. Chinese Journal of Applied Ecology, 36(1): 132-140.
[46]	辛宜静, 刘方, 陈祖拥, 等, 2024. 贵州区域茶园土壤有机碳空间分布的异质性及其主导因素[J]. 长江流域资源与环境, 33(7): 1589-1598.
	XIN Y J, LIU F, CHEN Z Y, et al., 2024. Spatial distribution and influencing factors of soil organic carbon in tea plantations in Guizhou province[J]. Resources and Environment in the Yangtze Basin, 33(7): 1589-1598.
[47]	谢珊, 2024. 不同种植年限茶树生长对土壤碳氮组分及微生物多样性的影响[D]. 贵阳: 贵州大学.
	XIE S, 2024. Effects of tea tree growth with different planting durations on soil carbon and nitrogen components and microbial diversity[D]. Guizhou: Guizhou University.
[48]	白龙龙, 盛雅琪, 徐丽丽, 等, 2024. “双碳”背景下我国稻田生态系统土壤固碳潜力分析[J]. 中国工程科学, 26(6): 246-256. DOI
	BAI L L, SHNEG Y Q, XU L L, et al., 2024. Carbon sequestration potential of paddy soil in China under the carbon peaking and carbon neutrality goals[J]. Strategic Study of CAE, 26(6): 246-256. DOI
[49]	余健, 房莉, 卞正富, 等, 2014. 土壤碳库构成研究进展[J]. 生态学报, 34(17): 4829-4838.
	YU J, FANG L, BIAN Z F, et al., 2014. A review of the composition of soil carbon pool[J]. Acta Ecologica Sinica, 34(17): 4829-4838.
[50]	于君宝, 刘景双, 王金达, 等, 2004. 不同开垦年限黑土有机碳变化规律[J]. 水土保持学报, 18(1): 27-30.
	YU J B, LIU J S, WANG J D, et al., 2004. Organic carbon variation law of black soil during different tillage period[J]. Journal of Soil and Water Conservation, 18(1): 27-30.
[51]	章晓芳, 郑生猛, 夏银行, 等, 2020. 红壤丘陵区土壤有机碳组分对土地利用方式的响应特征[J]. 环境科学, 41(3): 1466-1473.
	ZHANG X F, ZHENG S M, XIA Y H, et al., 2020. Responses of soil organic carbon fractions to land use types in hilly red soil[J]. Research of Environmental Sciences, 41(3): 1466-1473.
[52]	张彦军, 郁耀闯, 牛俊杰, 等, 2020. 秦岭太白山北坡土壤有机碳储量的海拔梯度格局[J]. 生态学报, 40(2): 629-639.
	ZHANG Y J, YU Y C, NIU J J, et al., 2020. The altitudinal gradient pattern of soil organic carbon storage on the north slope of Taibai Mountain in the Qinling Mountains[J]. Acta Ecologica Sinica, 40(2): 629-639.
[53]	赵秀婷, 辉朝茂, 朱书红, 等, 2022. 土壤有机质含量及其红外光谱特征对甜龙竹不同种植年限的响应[J]. 江西农业大学学报, 44(6): 1448-1456.
	ZHAO X T, HUI Z M, ZHU S H, et al., 2022. Response of soil organic matter content and its infrared spectral characteristics to different planting durations of Dendrocalamus brindisi[J]. Acta Agriculture Universitatis Jiangxiensis, 44(6): 1448-1456.

地区		经纬度	成土母质	土壤类型	地形地貌	海拔/m	年均降雨量/mm	年均温度/℃
湘北	石门县	29.67697°N，111.13568°E	板页岩风化物	黄壤	山地	800.0	1390.3	18.4
湘北	安化县	28.06293°N，110.94252°E	板页岩风化物	红壤	山地	800.0	1622.0	16.2
湘中	宁乡市	28.15858°N，112.17545°E	第四纪红土	红壤	丘陵	500.0	1472.9	17.6
	长沙县	28.16967°N，112.17417°E	花岗岩风化物	红壤	丘陵	300.0	1577.0	17.2
	新化县	27.93049°N，111.62245°E	板页岩风化物	红壤	山地	780.0	1455.9	17.0
湘南	常宁市	26.18958°N，112.29028°E	第四纪红土	红壤	山地	720.0	1440.0	18.1
	零陵区	26.17587°N，111.47099°E	第四纪红土	红壤	丘陵	169.4	1595.0	18.1
	汝城县	25.79194°N，112.90789°E	花岗岩风化物	红壤	丘陵	330.0	1545.7	16.5
湘西	沅陵县	28.66148°N，110.66289°E	板页岩风化物	黄壤	山地	600.0	1440.0	17.0
	古丈县	28.64958°N，109.97962°E	板页岩风化物	黄壤	山地	640.0	1475.9	16.0
	吉首市	28.21581°N，109.82114°E	花岗岩风化物	黄壤	丘陵	321.4	1440.5	16.4
	保靖县	28.73624°N，109.63897°E	石灰岩风化物	黄壤	丘陵	450.0	1470.0	16.1

地区		经纬度	成土母质	土壤类型	地形地貌	海拔/m	年均降雨量/mm	年均温度/℃
湘北	石门县	29.67697°N，111.13568°E	板页岩风化物	黄壤	山地	800.0	1390.3	18.4
湘北	安化县	28.06293°N，110.94252°E	板页岩风化物	红壤	山地	800.0	1622.0	16.2
湘中	宁乡市	28.15858°N，112.17545°E	第四纪红土	红壤	丘陵	500.0	1472.9	17.6
	长沙县	28.16967°N，112.17417°E	花岗岩风化物	红壤	丘陵	300.0	1577.0	17.2
	新化县	27.93049°N，111.62245°E	板页岩风化物	红壤	山地	780.0	1455.9	17.0
湘南	常宁市	26.18958°N，112.29028°E	第四纪红土	红壤	山地	720.0	1440.0	18.1
	零陵区	26.17587°N，111.47099°E	第四纪红土	红壤	丘陵	169.4	1595.0	18.1
	汝城县	25.79194°N，112.90789°E	花岗岩风化物	红壤	丘陵	330.0	1545.7	16.5
湘西	沅陵县	28.66148°N，110.66289°E	板页岩风化物	黄壤	山地	600.0	1440.0	17.0
	古丈县	28.64958°N，109.97962°E	板页岩风化物	黄壤	山地	640.0	1475.9	16.0
	吉首市	28.21581°N，109.82114°E	花岗岩风化物	黄壤	丘陵	321.4	1440.5	16.4
	保靖县	28.73624°N，109.63897°E	石灰岩风化物	黄壤	丘陵	450.0	1470.0	16.1

地区	pH	全氮质量分数/ (g·kg⁻¹)	全磷质量分数/ (g·kg⁻¹)	全钾质量分数/ (g·kg⁻¹)	土壤有机碳质量分数/ (g·kg⁻¹)	可溶性有机碳质量分数/ (g·kg⁻¹)	微生物量碳质量分数/ (g·kg⁻¹)	颗粒有机碳质量分数/ (g·kg⁻¹)	矿物结合态有机碳质量分数/ (g·kg⁻¹)
石门县	4.71±0.09bcd	2.02±0.37ab	1.24±0.26a	15.14±0.52bc	17.60±3.67ab	0.20±0.02abcd	0.25±0.06bc	7.42±1.37ab	6.29±1.00bc
安化县	4.81±0.19bcd	1.19±0.1cd	0.56±0.07b	13.50±0.37cde	12.43±1.10b	0.15±0.03cd	0.15±0.02cd	1.97±0.23de	4.11±0.35c
宁乡市	4.61±0.14cd	1.08±0.37d	0.46±0.14b	15.48±1.61bc	12.17±1.50b	0.16±0.05bcd	0.10±0.03d	1.13±0.50e	4.76±1.15c
长沙县	4.73±0.13bcd	0.81±0.14d	0.41±0.05b	17.45±1.34bc	9.81±1.34b	0.19±0.04abcd	0.19±0.04bcd	2.22±0.52de	4.98±0.60bc
新化县	4.93±0.11bcd	1.57±0.15bcd	0.38±0.06b	12.64±2.25cde	17.62±2.23ab	0.20±0.03abcd	0.20±0.03bcd	4.30±0.90cd	6.76±0.78bc
常宁市	4.52±0.09d	1.94±0.06abc	1.27±0.06a	16.66±2.00bc	23.63±0.86a	0.26±0.03abc	0.11±0.02d	3.23±0.18cde	15.57±0.68a
零陵区	5.82±0.21a	1.06±0.07d	0.40±0.05b	8.62±0.37de	13.20±0.82b	0.28±0.03a	0.28±0.03bc	4.69±0.55bcd	5.42±0.28bc
汝城县	4.73±0.08bcd	1.30±0.04bcd	0.62±0.05b	7.44±0.42e	14.37±0.58b	0.30±0.01a	0.12±0.02d	5.09±0.75abcd	6.56±0.49bc
沅陵县	5.30±0.28ab	0.95±0.12d	0.32±0.03b	12.49±0.56cde	11.30±1.41b	0.10±0.01d	0.16±0.03bcd	2.40±0.69de	5.89±0.59bc
古丈县	4.41±0.07d	2.41±0.17a	1.07±0.19a	14.48±0.56bcd	24.70±2.65a	0.27±0.02ab	0.49±0.02a	7.72±0.89a	7.96±0.66bc
吉首市	5.23±0.10abc	1.16±0.09cd	0.40±0.06b	20.18±0.67ab	12.25±0.90b	0.13±0.01d	0.15±0.02cd	2.78±0.43cde	5.39±0.36bc
保靖县	5.57±0.21a	1.49±0.12bcd	0.40±0.05b	23.66±3.04a	13.52±1.02b	0.11±0.01d	0.29±0.03b	5.57±0.53abc	4.93±0.57bc

地区	pH	全氮质量分数/ (g·kg⁻¹)	全磷质量分数/ (g·kg⁻¹)	全钾质量分数/ (g·kg⁻¹)	土壤有机碳质量分数/ (g·kg⁻¹)	可溶性有机碳质量分数/ (g·kg⁻¹)	微生物量碳质量分数/ (g·kg⁻¹)	颗粒有机碳质量分数/ (g·kg⁻¹)	矿物结合态有机碳质量分数/ (g·kg⁻¹)
石门县	4.71±0.09bcd	2.02±0.37ab	1.24±0.26a	15.14±0.52bc	17.60±3.67ab	0.20±0.02abcd	0.25±0.06bc	7.42±1.37ab	6.29±1.00bc
安化县	4.81±0.19bcd	1.19±0.1cd	0.56±0.07b	13.50±0.37cde	12.43±1.10b	0.15±0.03cd	0.15±0.02cd	1.97±0.23de	4.11±0.35c
宁乡市	4.61±0.14cd	1.08±0.37d	0.46±0.14b	15.48±1.61bc	12.17±1.50b	0.16±0.05bcd	0.10±0.03d	1.13±0.50e	4.76±1.15c
长沙县	4.73±0.13bcd	0.81±0.14d	0.41±0.05b	17.45±1.34bc	9.81±1.34b	0.19±0.04abcd	0.19±0.04bcd	2.22±0.52de	4.98±0.60bc
新化县	4.93±0.11bcd	1.57±0.15bcd	0.38±0.06b	12.64±2.25cde	17.62±2.23ab	0.20±0.03abcd	0.20±0.03bcd	4.30±0.90cd	6.76±0.78bc
常宁市	4.52±0.09d	1.94±0.06abc	1.27±0.06a	16.66±2.00bc	23.63±0.86a	0.26±0.03abc	0.11±0.02d	3.23±0.18cde	15.57±0.68a
零陵区	5.82±0.21a	1.06±0.07d	0.40±0.05b	8.62±0.37de	13.20±0.82b	0.28±0.03a	0.28±0.03bc	4.69±0.55bcd	5.42±0.28bc
汝城县	4.73±0.08bcd	1.30±0.04bcd	0.62±0.05b	7.44±0.42e	14.37±0.58b	0.30±0.01a	0.12±0.02d	5.09±0.75abcd	6.56±0.49bc
沅陵县	5.30±0.28ab	0.95±0.12d	0.32±0.03b	12.49±0.56cde	11.30±1.41b	0.10±0.01d	0.16±0.03bcd	2.40±0.69de	5.89±0.59bc
古丈县	4.41±0.07d	2.41±0.17a	1.07±0.19a	14.48±0.56bcd	24.70±2.65a	0.27±0.02ab	0.49±0.02a	7.72±0.89a	7.96±0.66bc
吉首市	5.23±0.10abc	1.16±0.09cd	0.40±0.06b	20.18±0.67ab	12.25±0.90b	0.13±0.01d	0.15±0.02cd	2.78±0.43cde	5.39±0.36bc
保靖县	5.57±0.21a	1.49±0.12bcd	0.40±0.05b	23.66±3.04a	13.52±1.02b	0.11±0.01d	0.29±0.03b	5.57±0.53abc	4.93±0.57bc

指标	SOC	DOC	MBC	POC	MAOC
SOC	1
DOC	0.83^**	1
MBC	0.87^**	0.96^**	1
POC	0.58	0.53	0.63^*	1
MAOC	0.94^**	0.87^**	0.87^**	0.68^*	1

Spatio-temporal Characteristics of Soil Organic Carbon and Its Components in Typical tea Gardens in Hunan Province, China

湖南典型茶园土壤有机碳及其组分时空特征

RichHTML

PDF

Knowledge

Abstract

Cite this article

share this article

Figures/Tables 10

References 53

Related Articles 15

Recommended Articles

Metrics

Comments

[1]	SHEN Jialong, WU Lihong, LI Linshuang, ZHOU Yuanfang, YANG Xiaomin. Effects of Land Uses on Soil Organic Carbon Fractions and Their Carbon Sequestration in a Typical Karst Small Mountain Watershed [J]. Ecology and Environmental Sciences, 2025, 34(3): 358-367.
[2]	SHI Hanzhi, XIONG Zhenqian, CAO Yiran, WU Zhichao, WEN Dian, LI Furong, LI Dongqin, WANG Xu. Effect of Straw Returning to Field on Organic Carbon Fixation in Red Soil and Black Soil [J]. Ecology and Environmental Sciences, 2024, 33(9): 1372-1383.
[3]	LI Jianfu, HUANG Zhilin, HE Chengzhong, JIANG Xin, SONG Lin, LIU Jiaxin, CHEN Liding. Spatial Distribution and Key Factors Affecting Soil Organic Carbon Within the Karst Fault Basin in Eastern Yunnan, China [J]. Ecology and Environmental Sciences, 2024, 33(9): 1339-1352.
[4]	LIN Dandan, BI Huaxing, ZHAO Danyang, GUAN Ning, HAN Jindan, GUO Yanjie. Soil Organic Carbon Fractions and Carbon Pool Characteristics of Robinia pseudoacacia Forests with Different Densities in the Loess Region of Western Shanxi Province [J]. Ecology and Environmental Sciences, 2024, 33(3): 379-388.
[5]	LUO Qing, HE Qing, WU Huiqiu, KOU Liyue, FANG Xu, ZHANG Xinyu, LI Yuan, CHAI Yuting, ZHANG Ruisheng, DAI Wenju. Characteristics of Soil Organic Carbon Fractions in Liao River Estuary Wetland and Their Influencing Factors [J]. Ecology and Environmental Sciences, 2024, 33(3): 333-340.
[6]	CHANG Boran, CHEN Rulan, WANG Biao, LAN Tian, DENG Lin, XUE Huiying. Characteristics of Soil Organic Carbon and Its Component Distribution in Different Forest Stand Types on Mount Zola in Southeastern Tibet [J]. Ecology and Environmental Sciences, 2024, 33(10): 1495-1505.
[7]	LI Chuanfu, ZHU Taochuan, MING Yufei, YANG Yuxuan, GAO Shu, DONG Zhi, LI Yongqiang, JIAO Shuying. Effect of Organic Fertilizer and Desulphurized Gypsum on Soil Aggregates and Organic Carbon and Its Fractions Contents in the Saline-alkali Soil of the Yellow River Delta [J]. Ecology and Environmental Sciences, 2023, 32(5): 878-888.
[8]	ZHANG Lin, QI Shi, ZHOU Piao, WU Bingchen, ZHANG Dai, ZHANG Yan. Study on Influencing Factors of Soil Organic Carbon Content in Mixed Broad-leaved and Coniferous Forests Land in Beijing Mountainous Areas [J]. Ecology and Environmental Sciences, 2023, 32(3): 450-458.
[9]	QIN Jiaqi, XIAO Zhirou, MING Angang, ZHU Hao, TENG Jinqian, LIANG Zeli, TAO Yi, QIN Lin. Effect of Monoculture and Mixed Plantation with Coniferous and Broadleaved Tree Species on Soil Microbial Carbon Cycle Functional Gene Abundance [J]. Ecology and Environmental Sciences, 2023, 32(10): 1719-1731.
[10]	XIAO Guoju, LI Xiujing, GUO Zhanqiang, HU Yanbin, WANG Jing. Effects of Soil Organic Carbon on Maize Growth and Water Use at the Eastern Foot of Helan Mountain in Ningxia [J]. Ecology and Environmental Sciences, 2022, 31(9): 1754-1764.
[11]	QIAN Lianwen, YU Tiantian, LIANG Xujun, WANG Yixiang, CHEN Yongshan. Stability of Biochar after Application for 5 Years in the Amendment of Acidified Tea Garden Soil [J]. Ecology and Environmental Sciences, 2022, 31(7): 1442-1447.
[12]	GONG Lingxuan, WANG Lili, ZHAO Jianning, LIU Hongmei, YANG Dianlin, ZHANG Guilong. Effects of Different Cover Crop Patterns on Soil Physicochemical Properties and Organic Carbon Mineralization in Tea Gardens [J]. Ecology and Environmental Sciences, 2022, 31(6): 1141-1150.
[13]	MA Huiying, LI Xinzhu, MA Xinyu, GONG Lu. Characteristics and Driving Factors of Soil Organic Carbon Fractions under Different Vegetation Types of the mid-Northern Piedmont of the Tianshan Mountains, Xinjiang [J]. Ecology and Environmental Sciences, 2022, 31(6): 1124-1131.
[14]	DU Xue, WANG Haiyan, ZOU Jiahe, MENG Hai, ZHAO Han, CUI Xue, DONG Qiqi. Distribution Characteristics and Influencing Factors of Soil Organic Carbon in Spruce-fir broad-leaved Mixed Forest on North Slope of Changbai Mountains [J]. Ecology and Environmental Sciences, 2022, 31(4): 663-669.
[15]	HU Jingda, ZHOU Haiju, HUANG Yongzhen, YAO Xianyu, YE Shaoming, YU Sufang. A Study on Plant Species Diversity and Soil Carbon and Nitrogen in Different Cunninghamia lanceolata Stand Types [J]. Ecology and Environmental Sciences, 2022, 31(3): 451-459.