盐水耦合三价铁输入对闽江河口湿地CO2排放的影响
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X16;X171

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国家自然科学基金项目(42371108)和福建省公益类科研院所专项(2023R1002003)资助。


Effects of Saltwater-coupled Trivalent Iron Input on CO2 Emissions from Min River Estuary Wetlands
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The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan)

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    摘要:

    为了探究全球气候变化背景下海平面上升导致的盐水入侵,以及强降雨条件下河流输送大量Fe元素对河口湿地生态系统CO2排放的影响,选取闽江河口道庆洲短叶茳芏淡水湿地为研究对象,通过中宇宙模拟试验,结合气相色谱法,研究盐水耦合Fe(III) 输入对植物生长期内河口湿地CO2排放的影响。结果表明:①盐水输入、Fe(III) 输入以及盐水耦合Fe(III) 输入均能显著促进河口湿地生态系统CO2的排放通量(P<0.05),但三者之间差异不显著;②盐水输入、Fe(III) 输入以及盐水耦合Fe(III) 输入均显著降低了河口湿地CO2排放的温度敏感性(P<0.05);③土壤β葡萄糖苷酶(βG)和纤维素水解酶(CBH)的活性较低,β-N-乙酰氨基葡萄糖苷酶(NAG)和酸性磷酸酶(AP)的活性较高;盐水输入、Fe(III) 输入以及盐水耦合Fe(III) 输入均显著抑制土壤βG活性(P<0.05);④河口湿地CO2的排放通量与湿地土壤电导率呈显著正相关,与土壤温度、土壤βG和CBH活性均呈显著负相关(P<0.05)。总之,盐水输入、Fe(III) 输入以及盐水耦合Fe(III) 输入均促进了河口湿地植物生长期内的CO2排放,但各处理之间差异不显著,表明双因素之间存在相互作用,其对河口湿地生态系统CO2排放的影响并非单因素输入的简单叠加;同时,盐水耦合Fe(III) 输入加剧了高温条件下的环境胁迫,因而抑制了微生物活性,降低了闽江河口湿地生态系统CO2排放对温度的敏感性。

    Abstract:

    In order to investigate the effects of saltwater intrusion due to sea level rise in the context of global climate change and the transport of large amounts of Fe by rivers under heavy rainfall conditions on CO2emissions from estuary wetland ecosystems, the Daoqingzhou freshwater wetland of Cyperus malaccensis in the estuary of the Min River was selected as a study object, a mesocosm simulation experiment was conducted, combined with gas chromatography, to study the effect of saltwater-coupled Fe(III) input on CO2 emissions during the growing period of plants in the estuary wetland. The results showed that: 1) Saltwater input, Fe(III) input, and saltwater coupled with Fe(III) input significantly contributed to CO2 emissions fluxes in estuary wetland ecosystems (P<0.05), but there were no significant differences among the three treatments. 2) Saltwater input, Fe(III) input, and saltwater coupled with Fe(III) input significantly reduced the temperature sensitivity of soil CO2 emissions in estuary wetlands (P<0.05). 3) Soil β-glucosidase (βG) and cellulose hydrolase (CBH) activities were lower, and β-N-Acetylglucosaminidase (NAG) and acid phosphatase (AP) activities were higher; saltwater input, Fe(III) input, and saltwater coupled with Fe(III) input significantly inhibited soil βG activity (P<0.05). 4) The emission flux of CO2 from the estuary wetland was significantly positively correlated with soil conductivity, and significantly negatively correlated with soil temperature, soil βG and CBH activities (P<0.05). In conclusion, saltwater input, Fe(III) input and saltwater-coupled Fe(III) input all promoted CO2 emissions during the growing period of plants in estuary wetlands, but there were no significant differences among the three treatments, indicating that the effects of two factors input on CO2 emissions were not a simple superposition of single-factor input because of an interaction between the two factors in estuary wetland ecosystems. Meanwhile, the saltwater-coupled Fe(III) input aggravated the environmental stress under high-temperature condition, and thus inhibited microbial activity and reduced the sensitivity of CO2 emissions to temperature in the wetland ecosystem of the Min River estuary.

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吴琪梦,王纯,侯丽,王霖,吴春梅,廖亦阳,王佳娜,仝川.盐水耦合三价铁输入对闽江河口湿地CO2排放的影响[J].土壤,2026,58(2):336-345. WU Qimeng, WANG Chun, HOU Li, WANG Lin, WU Chunmei, LIAO Yiyang, WANG Jiana, TONG Chuan. Effects of Saltwater-coupled Trivalent Iron Input on CO2 Emissions from Min River Estuary Wetlands[J]. Soils,2026,58(2):336-345

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  • 收稿日期:2025-03-31
  • 最后修改日期:2025-06-24
  • 录用日期:2025-06-27
  • 在线发布日期: 2026-05-09
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