欢迎访问《生态学杂志》官方网站,今天是 分享到:

生态学杂志 ›› 2025, Vol. 44 ›› Issue (3): 892-902.doi: 10.13292/j.1000-4890.202503.002

• 研究报告 • 上一篇    下一篇

不同海拔茶园土壤有机碳库组分及其化学结构

许宏达,王纯*,葛茂泉,杨发峻,吴梓炜,林少颖,王维奇   

  1. (福建师范大学地理科学学院, 碳中和未来技术学院, 福州 350117; 福建师范大学地理研究所, 福州 350117)
  • 出版日期:2025-03-10 发布日期:2025-06-10

Soil organic carbon fractions and chemical structure in tea gardens at different altitudes.

XU Hongda, WANG Chun*, GE Maoquan, YANG Fajun, WU Ziwei, LIN Shaoying, WANG Weiqi   

  1. (School of Geographical Sciences, School of Carbon Neutrality Future Technology, Fujian Normal University, Fuzhou 350117, China; Institute of Geographical Science, Fujian Normal University, Fuzhou 350117, China).

  • Online:2025-03-10 Published:2025-06-10

摘要: 土壤有机碳含量及化学结构对于陆地生态系统固碳和全球碳平衡具有重要影响。以福建省福鼎市典型茶园不同海拔土壤为研究对象,采用傅里叶红外光谱法和土壤参数分析相结合,对土壤有机碳不同组分含量、化学结构、土壤碳库管理指数(CPMI)等进行测定与分析。结果表明:土壤微生物生物量碳(MBC)表现为高海拔显著高于中低海拔(P<0.05),土壤溶解性有机碳(DOC)含量表现为中海拔最高,上层土壤易氧化有机碳(EOC)含量和土壤有机碳(SOC)含量均表现为中高海拔显著高于低海拔(P<0.05);土壤烷氧碳相对强度整体最高,且上层土壤烷氧碳相对强度随海拔升高显著降低(P<0.05),烷基碳和芳香碳的相对强度不同海拔间差异不显著(P>0.05);土壤脂肪碳相对强度整体较低,随着海拔的升高呈现先升高后降低的趋势(P<0.05);随着海拔升高,上层土壤芳香碳/烷氧碳(ARC/ALC)比值提高;上层土壤CPMI表现为中高海拔高于低海拔;土壤SOC及其各组分与TN含量和含水量呈正相关,与容重呈负相关;土壤烷氧碳与TN含量、土壤碳库稳定性呈负相关;土壤含水量和TN是影响茶园不同海拔土壤有机碳库组分及其化学结构特征的关键影响因素,上层土壤有机碳稳定性随海拔升高而升高。在未来的茶园管理实践中,应该进一步提升低海拔上层土壤碳汇功能。


关键词: 海拔, 有机碳组分, 碳结构, 土壤碳库管理指数, 茶园

Abstract: Soil organic carbon content and chemical structure affect carbon sequestration of terrestrial ecosystems and global carbon balance. We collected soil samples from typical tea plantations at different altitudes in Fuding City, Fujian Province. Fourier transform infrared spectroscopy and soil parameter analysis were used to analyze the content of soil carbon fractions, chemical structure and soil carbon pool management index (CPMI). The results showed that soil microbial biomass carbon (MBC) was significantly higher at high altitude than that at middle and low altitude (P<0.05). The content of soil dissolved organic carbon (DOC) was the highest at middle altitude (P<0.05). The content of soil easily oxidized organic carbon (EOC) and soil organic carbon (SOC) in the upper soil layers were the lowest at low altitude. The relative strength of soil alkoxy carbon was the highest. The relative strength of upper soil alkoxy carbon decreased significantly with increasing altitudes (P<0.05), while the relative strength of soil alkyl carbon and aromatic carbon showed no significant differences among altitudes (P>0.05). The relative strength of soil fat carbon was generally low, and it increased first and then decreased with increasing altitudes (P<0.05). With the increases of altitudes, the ratio of aromatic carbon/alkoxy carbon (ARC/ALC) in upper soil increased. The CPMI of upper soil was higher at middle and high altitudes than that at low altitudes. Soil SOC and its fractions were positively correlated with soil TN content and water content, and negatively correlated with bulk density. Soil alkoxy carbon was negatively correlated with soil TN content and carbon pool stability. Soil water content and TN were the key factors affecting the composition and chemical structure of soil organic carbon in tea plantations at different altitudes. The stability of upper soil organic carbon increased with increasing altitudes. In the future management practice of tea plantations, carbon sink function of upper soil at low altitude should be further strengthened.


Key words: altitude, organic carbon fraction, carbon structure, soil carbon pool management index, tea garden