Spatial-Temporal Resolution of Dissolved Ch4 Concentrations and Fluxes from Different Freshwater Types in an Agricultural Irrigation Watershed in Eastern China

32 Pages Posted: 12 Jul 2022

See all articles by Tianrui Zhang

Tianrui Zhang

affiliation not provided to SSRN

Shuang Wu

affiliation not provided to SSRN

Xiantao Fang

affiliation not provided to SSRN

Zhaoqiang Han

affiliation not provided to SSRN

Shuqing Li

affiliation not provided to SSRN

Jinyang Wang

affiliation not provided to SSRN

Shuwei Liu

affiliation not provided to SSRN

Jianwen Zou

affiliation not provided to SSRN

Abstract

Inland freshwater ecosystems are of increasing concerns on global methane (CH4) budget in the atmosphere. Agricultural irrigation watershed is a potential CH4 emission hotspot owing to the anthropogenic carbon and nutrient loading. However, large-scale spatial variations of CH4 concentrations and fluxes in agricultural catchments remain poorly understood, constraining an accurate regional estimate of CH4 budgets. Here, we examined the spatial-temporal resolution of dissolved CH4 concentrations and fluxes from different freshwater types (ditch, reservoir and river) in an agricultural irrigation watershed from Hongze catchment, under intensive agriculture and rural activities in Eastern China. Annual mean CH4 concentration and flux were 0.12 μmol L-1 and 0.58 mg m-2 d-1, respectively. Total CH4 flux from this agricultural irrigation watershed was estimated to be 0.002 Gg CH4 yr-1. Diffusive CH4 flux varied in samples taken from different freshwater types, the annual mean CH4 flux for ditch, reservoir and river was 0.31±0.06, 0.71±0.13 and 0.72±0.25mg m-2 d-1, respectively. Midstream (reservoir) and downstream (river) waters are hotspots, in which the CH4 production rates were two times greater than in non-hotspot locations. The dissolved CH4 concentrations and fluxes in three water types showed similar temporal variations, with the highest levels in summer and the lowest levels in winter. Water velocity and wind speed are important in explaining variable of dissolved CH4 concentration and flux. The responses of CH4 fluxes to water dissolved oxygen (DO), nitrate nitrogen (NO3--N) and sediment dissolved organic carbon (DOC) concentrations were significantly stronger in reservoir and river than in ditch, indicating that intensive human activities may affect the CH4 fluxes from different freshwater types. These results highlighted a need for more field measurements with wider spatial coverage and finer frequency, which would further improve the reliability of flux estimates for assessing the contribution of agricultural watersheds to the regional and global CH4 budgets.

Keywords: Agricultural irrigation watershed, Dissolved CH4 concentration, Diffusive CH4 flux, Different freshwater types

Suggested Citation

Zhang, Tianrui and Wu, Shuang and Fang, Xiantao and Han, Zhaoqiang and Li, Shuqing and Wang, Jinyang and Liu, Shuwei and Zou, Jianwen, Spatial-Temporal Resolution of Dissolved Ch4 Concentrations and Fluxes from Different Freshwater Types in an Agricultural Irrigation Watershed in Eastern China. Available at SSRN: https://ssrn.com/abstract=4160652 or http://dx.doi.org/10.2139/ssrn.4160652

Tianrui Zhang

affiliation not provided to SSRN ( email )

Shuang Wu (Contact Author)

affiliation not provided to SSRN ( email )

Xiantao Fang

affiliation not provided to SSRN ( email )

Zhaoqiang Han

affiliation not provided to SSRN ( email )

Shuqing Li

affiliation not provided to SSRN ( email )

Jinyang Wang

affiliation not provided to SSRN ( email )

Shuwei Liu

affiliation not provided to SSRN ( email )

Jianwen Zou

affiliation not provided to SSRN ( email )

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