
应用生态学报 ›› 2026, Vol. 37 ›› Issue (9): 2963-2976.doi: 10.13287/j.1001-9332.202609.040
马田1,2, 白雅雯1,2, 赵艺棋1,2, 孙晓董1,2, 杨艳红3, 刘佩秀4, 韩广轩1,2*
收稿日期:2026-05-08
接受日期:2026-07-17
出版日期:2026-09-18
发布日期:2026-10-12
通讯作者:
*E-mail: gxhan@yic.ac.cn
作者简介:马 田, 女, 1988年生, 研究员。主要从事陆海连续体土壤碳循环研究。E-mail: matian4022@126.com
基金资助:MA Tian1,2, BAI Yawen1,2, ZHAO Yiqi1,2, SUN Xiaodong1,2, YANG Yanhong3, LIU Peixiu4, HAN Guangxuan1,2*
Received:2026-05-08
Accepted:2026-07-17
Online:2026-09-18
Published:2026-10-12
摘要: 滨海湿地作为关键的“蓝碳”生态系统,其碳汇评估多聚焦于垂直埋藏,而常忽略横向碳交换这一关键路径。本文系统梳理了滨海湿地横向碳交换关键组分(溶解态无机碳、溶解态有机碳和颗粒态有机碳)的生物地球化学转化过程、关键测算方法及其驱动机制。与垂直碳埋藏速率相比,滨海湿地横向碳输出速率较高,且不同滨海湿地类型间无差异显著。其关键过程包括潮汐泵驱动的孔隙水交换和海底地下水排放(SGD)。潮汐过程驱动沉积物与上覆水体间周期性孔隙水交换,促进了沉积物溶解物质释放;而水力梯度、潮汐引起的海底压力变化、波浪作用及海水-地下水密度差异等多重地球物理过程共同控制海底地下水排放的发生与强度。在驱动机制上,潮汐泵效应、孔隙水交换和SGD是横向碳输出的核心动力,而极端天气事件(如台风、强降雨)则通过激发效应和水动力强化,在短时间内主导碳通量变化。横向输出至近海的碳通过碳酸盐系统缓冲、沉降进入深海沉积物等路径实现长期封存,但也受到人类活动和气候变化的强烈干扰。未来研究亟需开展横向碳输出物理-生物地球化学耦合过程的精细量化,开展多组分碳的协同观测与同位素溯源,构建多重环境压力下的碳收支动态预测模型,为全球蓝碳精准核算与海岸带适应性管理提供科学支撑。
马田, 白雅雯, 赵艺棋, 孙晓董, 杨艳红, 刘佩秀, 韩广轩. 滨海湿地横向碳交换关键过程与影响机制[J]. 应用生态学报, 2026, 37(9): 2963-2976.
MA Tian, BAI Yawen, ZHAO Yiqi, SUN Xiaodong, YANG Yanhong, LIU Peixiu, HAN Guangxuan. Key processes and influencing mechanisms of lateral carbon exchange in coastal wetlands.[J]. Chinese Journal of Applied Ecology, 2026, 37(9): 2963-2976.
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