Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau, The Hong Kong University of Science and Technology, Hong Kong, China.
Key Laboratory of Coastal Environment and Resources of Zhejiang Province, School of Engineering, Westlake University, Hangzhou, China.
Water Res. 2024 Sep 15;262:122120. doi: 10.1016/j.watres.2024.122120. Epub 2024 Jul 18.
Saltmarshes along the Chinese coast are threatened by the invasion of Spartina alterniflora (S. alterniflora). This study was carried out in the Andong Shoal, Hangzhou Bay, China, with the aim of comprehending the intricate impacts of S. alterniflora invasion on greenhouse gases (GHG) production and emissions. To address this issue, we thoroughly examined the chemistry of dissolved organic matter (DOM) and the rate of surface water-porewater interaction. Porewater and surface water samples were collected from farm land, S. alterniflora invaded areas, and Scirpus mariqueter (S. mariqueter) dominated areas. The findings indicated that the invasion of S. alterniflora impeded the interaction between surface water and porewater, resulting in reduced porewater exchange rates within its affected region (0.015-0.440 cm d), in contrast to areas dominated by S. mariqueter (9.635-18.232 cm d). The invasion also increased dissolved organic carbon concentration in porewater and created a stable and closed soil environment that resulted in DOM with smaller molecule sizes and higher humification levels. The presence of high tryptophan-like fluorescent DOM caused an increase in the production of methane and carbon dioxide in S. alterniflora invaded area. However, both limited surface-porewater exchange and significant differences in GHG concentrations between porewater and surface water suggested that the aerenchyma tissues of S. alterniflora may play an important role in transporting GHG from soil to the atmosphere.
中国沿海盐沼受到互花米草(Spartina alterniflora)的入侵威胁。本研究在中国杭州湾的庵东滩进行,旨在深入了解互花米草入侵对温室气体(GHG)产生和排放的复杂影响。为解决这一问题,我们全面研究了溶解有机 matter(DOM)的化学性质和地表水-孔隙水相互作用的速率。采集了农田、互花米草入侵区和海三棱藨草(Scirpus mariqueter)区的孔隙水和地表水样品。结果表明,互花米草入侵阻碍了地表水与孔隙水的相互作用,导致其影响区的孔隙水交换率降低(0.015-0.440 cm d),而海三棱藨草区的交换率较高(9.635-18.232 cm d)。入侵还增加了孔隙水中溶解有机碳的浓度,并形成了稳定的封闭土壤环境,导致 DOM 具有更小的分子大小和更高的腐殖化水平。富含色氨酸样荧光 DOM 的存在导致互花米草入侵区甲烷和二氧化碳的产生增加。然而,表面-孔隙水交换受限以及孔隙水和地表水之间 GHG 浓度存在显著差异表明,互花米草的通气组织可能在将 GHG 从土壤输送到大气中发挥重要作用。