Luo Zhuan-Xi, Qiu Zhao-Zheng, Wang Zhen-Hong, Yan Chang-Zhou
Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China.
Huan Jing Ke Xue. 2013 Mar;34(3):900-6.
The purpose of this study was to characterize the decomposition process of different plant litters and its controlling factors, and to quantify the different contribution rates to sediments organic matter throughout the decomposition of different plant litters. Results showed that the decomposition rates of plant litters buried at medium tidal level were 0.655 a(-1) for mangrove and 1.723 a(-1) for Spartina, which were greater than those with 0.651 a(-1) for mangrove and 1.586 a(-1) for Spartina at high tidal level. The reduction of carbon concentration in plant litters at high tidal level was lower than that at medium tidal level, while the increment of nitrogen and sulfur concentrations in plant litters at high tidal level was greater than those at medium tidal. And the isotope abundance of carbon (delta13C) in plant litters at medium tidal level reduced much more significantly than that at high tidal level. The contribution rates of plant litters carbon to sediments organic matter differed among tidal levels, plant species and decomposition duration. Specifically, the decomposition of mangrove litters contributed 5.96% to the sediment organic matter at medium tidal level, which was greater than that (3.03%) at high tidal level. Similarly, the decomposition of Spartina litters contributed 14.81% to the sediment organic matter at medium tidal level, which was also greater than that (13.97%) at high tidal level. The contribution of the decomposition of Spartina litters organic matter (average with 14.39%) was greater than that of mangrove litters (4.50%). The decomposition of plant litters requires a long process. The contribution of plant litters to sediments organic matter throughout one year decomposition was lower than that in complete decomposition, in particular, mangrove litters. Our study showed that the quantitative differences in plant litters-derived sediment organic matter would improve the proper estimation of the contribution of litters to wetland organic matter.
本研究旨在表征不同植物凋落物的分解过程及其控制因素,并量化不同植物凋落物在整个分解过程中对沉积物有机质的不同贡献率。结果表明,中潮位掩埋的植物凋落物分解速率,红树林为0.655 a⁻¹,互花米草为1.723 a⁻¹,高于高潮位的0.651 a⁻¹和1.586 a⁻¹。高潮位植物凋落物中碳浓度的降低低于中潮位,而高潮位植物凋落物中氮和硫浓度的增加大于中潮位。中潮位植物凋落物中碳的同位素丰度(δ¹³C)比高潮位降低得更显著。植物凋落物碳对沉积物有机质的贡献率在潮位、植物种类和分解持续时间之间存在差异。具体而言,红树林凋落物在中潮位对沉积物有机质的贡献率为5.96%,高于高潮位的3.03%。同样,互花米草凋落物在中潮位对沉积物有机质的贡献率为14.81%,也高于高潮位的13.97%。互花米草凋落物有机质分解的贡献率(平均为14.39%)大于红树林凋落物(4.50%)。植物凋落物的分解需要一个漫长的过程。植物凋落物在一年分解过程中对沉积物有机质的贡献率低于完全分解时,特别是红树林凋落物。我们的研究表明,植物凋落物来源的沉积物有机质的定量差异将有助于更准确地估计凋落物对湿地有机质的贡献。