2019
DOI: 10.1016/j.jclepro.2019.02.002
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Emission and absorption of greenhouse gases generated from marine shrimp production (Litopeneaus vannamei) in high salinity

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Cited by 17 publications
(3 citation statements)
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“…The freshwater and brackish aquaculture ponds, with a global total surface area of around 1.1×10 5 km 2 (Verdegem and Bosma, 2009), are potential hotspots of CH4 emission because of their large loadings of organic matter from residual feeds and feces of cultured animals (IPCC, 2019;Yang et al, 2018Yang et al, , 2019Yuan et al, 2019). Although numerous studies have quantified CH4 fluxes from the aquaculture ponds (Chen et al, 2016;Ma et al, 2018;Soares and Henry-Silva, 2019;Wu et al, 2018;Yang et al, 2018Yang et al, , 2019Yuan et al, 2019), the biogeochemical processes involved (e.g., CH4 production, oxidation, and transport) in the aquaculture systems have thus far received little attention (Avnimelech and Ritvo, 2003). Biogenic CH4 is produced during the terminal step of organic matter degradation in anaerobic sediments (Lofton et al, 2015) and in oxic waters with rich planktonic microbes (Bogard et al, 2014;Khatun et al, 2019;Tang et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…The freshwater and brackish aquaculture ponds, with a global total surface area of around 1.1×10 5 km 2 (Verdegem and Bosma, 2009), are potential hotspots of CH4 emission because of their large loadings of organic matter from residual feeds and feces of cultured animals (IPCC, 2019;Yang et al, 2018Yang et al, , 2019Yuan et al, 2019). Although numerous studies have quantified CH4 fluxes from the aquaculture ponds (Chen et al, 2016;Ma et al, 2018;Soares and Henry-Silva, 2019;Wu et al, 2018;Yang et al, 2018Yang et al, , 2019Yuan et al, 2019), the biogeochemical processes involved (e.g., CH4 production, oxidation, and transport) in the aquaculture systems have thus far received little attention (Avnimelech and Ritvo, 2003). Biogenic CH4 is produced during the terminal step of organic matter degradation in anaerobic sediments (Lofton et al, 2015) and in oxic waters with rich planktonic microbes (Bogard et al, 2014;Khatun et al, 2019;Tang et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…79 CO 2 concentration in water is driven by the consumption and production of autotrophic organisms and by the production of heterotrophic organisms, as well as by salinity, temperature and water alkalinity. 51,80,81 However, lack of correlation between DO, and CO 2 and CH 4 flux, suggests no biological control over the flux of these two gases. DO concentration in water in low precipitation months (dry season) is very low, but in September it is above 5.0 mg L -1 (Table 2).…”
Section: Discussionmentioning
confidence: 99%
“…A recirculation aquaculture system (RAS) can stabilize water quality so that it remains suitable and can be reused for aquaculture. In addition, the recirculation system can control plankton and algae blooming so that the water remains in good condition (Díaz‐Jiménez et al, 2018; Matich et al, 2020; Soares & Henry‐Silva, 2019; Yang et al, 2020). The same was reported by Badiola et al (2012), Martín‐Calderón et al (2015), Xu and Boyd (2016), and Zarain‐Herzberg et al (2010) that the use of recirculation can reduce organic waste and other nutrients so that water quality is in good condition and suitable for use in aquaculture.…”
Section: Introductionmentioning
confidence: 99%