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干湿季水稻的温室气体排放与能量交换:涡度相关法。

Greenhouse gas emissions and energy exchange in wet and dry season rice: eddy covariance-based approach.

机构信息

Division of Crop Production, National Rice Research Institute, Cuttack, Odisha, 753006, India.

Department of Botany, Ravenshaw University, Cuttack, Odisha, 753003, India.

出版信息

Environ Monit Assess. 2018 Jun 25;190(7):423. doi: 10.1007/s10661-018-6805-1.

Abstract

Lowland tropical rice-rice system has a unique micrometrological characteristic that affects both energy component and net ecosystem energy. Periodic and seasonal variations of methane (CH), carbon dioxide (CO), and energy exchange from irrigated lowland rice-rice ecosystem were studied using open-path eddy covariance (EC) system during the dry (DS) and wet (WS) seasons in 2015. Concurrently, the manual chamber method was employed in nitrous oxide (NO) measurement efflux. Cumulative net ecosystem carbon exchange (NEE) was observed highest (- 232.55 g C m) during the WS and lowest (- 14.81 g C m) during wet fallow (WF). Similarly, the cumulative net ecosystem methane exchange (NEME) was found highest (13,456.5 mg CH m) during the WS and lowest (2014.3 mg CH m) during the WF. Surface energy fluxes, i.e., sensible (Hs) and latent heat (LE) fluxes, showed a similar trend. With the advancement of time, the ratio of ecosystem respiration (Re) and gross primary production (GPP) increased. The cumulative global warming potential (GWP) for the two cropping seasons including two fallows was 13,224.1 kg CO equivalent ha. The GWP and NEME showed a similar trend as soil enzymes and labile carbon pools in both seasons (except GWP at the harvesting stage in the wet season). The mean NEE exhibited a more negative value with decrease in labile pools from panicle initiation to harvesting stage in the WS. Soil labile C and soil enzymes can be used as an indicator of NEE, NEME, and GWP in lowland rice ecology. Graphical abstract Schematic presentation of GHG emission and energy exchange in lowland rice.

摘要

低地热带水稻-水稻系统具有独特的微观气象特征,影响能量组成和净生态系统能量。本研究使用开路涡度相关(EC)系统,在 2015 年旱季(DS)和雨季(WS)期间,研究了灌溉低地水稻-水稻生态系统中甲烷(CH)、二氧化碳(CO)和能量交换的周期性和季节性变化。同时,采用手动室法测量氧化亚氮(NO)排放通量。在 WS 期间,累积净生态系统碳交换(NEE)最高(-232.55 g C m),在 WF 期间最低(-14.81 g C m)。同样,在 WS 期间,累积净生态系统甲烷交换(NEME)最高(13456.5 mg CH m),在 WF 期间最低(2014.3 mg CH m)。地表能量通量,即显热(Hs)和潜热(LE)通量,表现出相似的趋势。随着时间的推移,生态系统呼吸(Re)和总初级生产力(GPP)的比值增加。两个种植季(包括两个休耕期)的累积全球增温潜势(GWP)为 13224.1 kg CO 当量公顷。GWP 和 NEME 与两个季节的土壤酶和可利用碳库呈相似趋势(雨季收获阶段的 GWP 除外)。在 WS 期间,从颖花启动到收获阶段,可利用碳库减少,导致平均 NEE 呈现更负的值。土壤可利用 C 和土壤酶可作为低地水稻生态系统中 NEE、NEME 和 GWP 的指标。

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