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Nitrous oxide and methane emissions from the restored mangrove ecosystem of the Cienaga Grande de Santa Marta, Colombia

机译:恢复的哥伦比亚圣玛尔塔圣玛尔塔红树林生态系统中的一氧化二氮和甲烷排放

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Most studies on emission of the greenhouse gases nitrous oxide (N_2O) and methane (CH_4) have been carried out in temperate areas so there is generally a lack of data from subtropical and tropical climates. A large part of the subtropical and tropical coastal wetlands consists of mangrove ecosystems, which have potential to act as sources of N_2O and CH_4. We measured N_2O and CH_4 emissions during 11 months in the brackish lagoon system Cienaga Grande de Santa Marta (CGSM) on the Caribbean coast of Colombia. The area has been seriously influenced by human disturbance which resulted in approximately 60% mangrove mortality but the ecosystem is now being rehabilitated. In addition to N_2O and CH_4 emissions at four sampling sites, we also measured temperature, salinity, pH, dissolved oxygen (DO), redox potential, nitrite (NO_2~-), nitrate (NO_3~-), ammonium (NH_4~+) and organic material in the water and/or the sediment. We found the mangrove sediments of CGSM to be a source of N_2O and CH_4 but there was large variability of the emissions on both temporal and spatial scale with N_2O and CH_4 fluxes in the range 35 -1180 μg m~(-2) h~(-1) and 0-31570 μg m~(-2) h~(-1), respectively. Correlations between N_2O fluxes and the water variables showed that salinity significantly contributed towards decreased emission of N_2O (r = -0.38). By contrast, water concentrations of NO_3~- were correlated with increased emission of N_2O (r = 0.54). Emission of CH_4 was negatively correlated with DO in the water (r = -0.34) and there was a positive correlation between organic matter and CH_4 emission (r = 0.75). It was found that untreated wastewater discharged into the Magdalena River and in turn, the lagoon system may have resulted in a substantially higher emission of both N_2O and CH_4 as the wastewater contributes substrate to the processes in the form of N and organic matter. With better treatment of wastewater, it is possible that emission of both gases would be lower, especially at the sites closest to Magdalena River.
机译:大多数关于温室气体排放的研究都在温带地区进行,因此一般缺乏来自亚热带和热带气候的数据。亚热带和热带沿海湿地的很大一部分由红树林生态系统组成,它们有可能成为N_2O和CH_4的来源。我们在哥伦比亚加勒比海沿岸咸咸泻湖系统圣玛尔塔圣玛尔塔(CGSM)的11个月内测量了N_2O和CH_4的排放。该地区已受到人为干扰的严重影响,导致约60%的红树林死亡,但目前正在恢复生态系统。除了在四个采样点排放N_2O和CH_4之外,我们还测量了温度,盐度,pH,溶解氧(DO),氧化还原电势,亚硝酸盐(NO_2〜-),硝酸盐(NO_3〜-),铵(NH_4〜+)以及水和/或沉积物中的有机物质。我们发现CGSM的红树林沉积物是N_2O和CH_4的来源,但N_2O和CH_4的通量在35 -1180μgm〜(-2)h〜( -1)和0-31570μgm〜(-2)h〜(-1)。 N_2O通量与水变量之间的相关性表明,盐度显着有助于减少N_2O的排放(r = -0.38)。相比之下,NO_3〜-的水浓度与N_2O排放增加相关(r = 0.54)。 CH_4的排放与水中的DO呈负相关(r = -0.34),有机物与CH_4的排放呈正相关(r = 0.75)。结果发现,未经处理的废水排放到马格达莱纳河中,进而导致泻湖系统排放的N_2O和CH_4大大增加,因为废水以N和有机物的形式参与了处理过程。通过更好地处理废水,两种气体的排放量可能会降低,尤其是在靠近马格达莱纳河的地区。

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