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  • Lingyi LEI, Feipeng WANG, Kunpeng ZANG, Xiaolong LÜ, Zhi ZHANG, Liyang YANG, Jingli MU
    Advances in Earth Science. 2024, 39(11): 1156-1168. https://doi.org/10.11867/j.issn.1001-8166.2024.088

    Evaluating the distribution and sea-air fluxes of dissolved methane (CH4) in mariculture areas is important for understanding how aquaculture contributes to regional CH4 emissions into the atmosphere. Seasonal field surveys conducted in 2023 were used to analyze the temporal and spatial variation of CH4 concentrations in surface water and CH4 air-sea flux in a typical aquaculture system in Sansha Bay, Fujian Province. The results showed that dissolved CH4 concentrations ranged from 9.91 to 609.22 nmol/L, with corresponding air-sea fluxes between 3.46 to 1 188.15 μmol/ (m2·d). Temporally, the CH4 air-sea fluxes were higher in summer and autumn compared to spring and winter. Spatially, CH4 concentrations and air-sea fluxes decreased consistently from the estuary to the bay mouth, with the highest values in the estuarine aquaculture area and the lowest in the bay mouth aquaculture area. Correlation analysis showed that aquacultural activities and terrestrial runoff inputs contributed to the spatiotemporal distribution of CH4 concentrations within the bay. In the macroalgae cultivation zones, CH4 production and emissions during farming periods were significantly lower than during non-farming periods. Additionally, the residual feed and feces generated by fish in cages may result in increased CH4 emissions. Notably, CH4 emissions peaked in summer, due to enhanced aquaculture activities and runoff inputs during the wet season. Future work should focus on investigating CH4 air-sea fluxes in mariculture areas to provide scientific support for CH4 control and emission reduction in aquaculture.

  • Xiaozhi ZHANG, Huaiyang ZHOU, Shengping QIAN
    Advances in Earth Science. 2021, 36(3): 288-306. https://doi.org/10.11867/j.issn.1001-8166.2021.035

    Andesite is an important rock type in subduction zone magmatic arcs. Its genesis is still one of focuses on the international geological research. According to the tectonic setting of the andesite, magmatic arc andesite can be classified as continental arc andesite and oceanic arc andesite, which show different features in chemical composition and spatial distribution. Since the late 1920s, numerous researches have enriched our understanding of the genesis of magmatic arc andesite, which gradually can be summarized as Basalt-input model and Andesite-input model. The Basalt-input model considers the primary magma of magmatic arc andesite is basaltic, emphasizing the intra-crustal processes such as fractional crystallization, assimilation and contamination, and magma mixing. The Andesite-input model suggests andesitic melts can be formed directly in the mantle source, emphasizing the sub-crustal processes such as the metasomatic reaction between slab-derived fluid/melt and mantle peridotite, and rising of sediment diapirs. Although some progress has been made in the study of the genesis of magmatic arc andesite, each model still needs to be improved. There are many research fields to be studied in the future, including experimental petrology research of mantle metasomatite, relationship between andesite and the formation and evolution of continental crust, application of theoretical calculation and modelling and so on.