地理学报 ›› 2016, Vol. 71 ›› Issue (11): 1926-1938.doi: 10.11821/dlxb201611005
宋贤威1,2(), 高扬2,3(
), 温学发2, 郭大立2, 于贵瑞2, 何念鹏2, 张进忠1
收稿日期:
2016-06-24
修回日期:
2016-10-08
出版日期:
2016-11-25
发布日期:
2016-11-25
作者简介:
作者简介:宋贤威(1993-), 男, 硕士, 主要从事环境地球化学研究。E-mail:
基金资助:
Xianwei SONG1,2(), Yang GAO2,3(
), Xuefa WEN2, Dali GUO2, Guirui YU2, Nianpeng HE2, Jinzhong ZHANG1
Received:
2016-06-24
Revised:
2016-10-08
Published:
2016-11-25
Online:
2016-11-25
摘要:
喀斯特地区的岩石风化固碳被认为是全球遗漏碳汇之一,中国喀斯特地区的分布面积达344万km2,目前对其岩溶碳汇缺乏精确、系统的评估,对碳汇产生的机制仍存在争议。本文通过对喀斯特地区碳汇研究的回顾,详细介绍了适用于喀斯特地区固碳速率的估算方法,并对喀斯特地区的岩石风化碳汇进行再评估,然后将地球关键带科学概念引入喀斯特生态系统,阐述喀斯特关键带碳汇研究对生态系统服务和功能的意义。研究结果表明,中国喀斯特地区每年因岩溶作用产生的碳汇为4.74 Tg C yr-1,未来中国需要加强岩石—土壤—水体—生物—大气复杂交互系统的基础数据收集,以明确各界面碳通量,对喀斯特关键带碳汇进行多尺度、多方法、全方位联合评估,在改善喀斯特生态系统功能、科学管理区域和国家碳收支及全球变化研究等方面为政府和学者提供参考。
宋贤威, 高扬, 温学发, 郭大立, 于贵瑞, 何念鹏, 张进忠. 中国喀斯特关键带岩石风化碳汇评估及其生态服务功能[J]. 地理学报, 2016, 71(11): 1926-1938.
Xianwei SONG, Yang GAO, Xuefa WEN, Dali GUO, Guirui YU, Nianpeng HE, Jinzhong ZHANG. Rock-weathering-related carbon sinks and associated ecosystem service functions in the karst critical zone in China[J]. Acta Geographica Sinica, 2016, 71(11): 1926-1938.
表2
中国喀斯特地区固碳速率估算汇总
估算方法 | 估算区域(裸岩=90.7万km2,全国=344万km2) | 固碳速率 (Tg C yr-1) | 全球固碳速率 (Pg C yr-1) | 资料来源 |
---|---|---|---|---|
水化学径流法 | 裸岩 | 12 | — | [11] |
水化学径流法 | 裸岩 | 4.8 | — | [54] |
溶蚀试片法 | 裸岩 | 3.2 | — | [54] |
DBL理论(潜在速率) | 全国 | 64.2 | 0.41 | [42] |
水化学径流法 | 全国 | 17.9 | 0.11 | [42] |
溶蚀试片法 | 全国 | 17.5 | 0.11 | [42] |
溶蚀试片法 | 全国 | 3.21 | — | [9] |
水化学径流法 | 全国 | 4.84 | — | [9] |
累加法(按省份) | 全国 | 5.07 | — | [9] |
GIS-溶蚀试片法 | 全国 | 3.88 | — | [9] |
GEM-CO2模型 | 全国 | 14.1 | — | [63] |
水化学径流法(分区) | 全国 | 10.09 | — | [62] |
水化学径流法(分区) | 全国 | 4.74 | — | 本研究 |
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