Interpreting the effect of soil texture on transport and removal of nitrate-N in saline coastal tidal flats under steady-state flow condition
Tidal-flats play important roles in oceanic nitrogen (N) cycles. Particularly, N loss in the tidal-flats depends on soil texture and yet the dominant N removal mechanism in relation to soil texture is not clear. Therefore, the objective of this study was to investigate the effect of soil texture on...
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Published in | Continental shelf research Vol. 84; pp. 35 - 42 |
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Format | Journal Article |
Language | English |
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Elsevier Ltd
01.08.2014
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Abstract | Tidal-flats play important roles in oceanic nitrogen (N) cycles. Particularly, N loss in the tidal-flats depends on soil texture and yet the dominant N removal mechanism in relation to soil texture is not clear. Therefore, the objective of this study was to investigate the effect of soil texture on NO3−-N removal and transport in texturally contrasting tidal-flats of the western coast of Korea [Gangwha (GH, silt) and Saemangeum (SMG, loamy sand) sites]. To interpret the experimental results, we compared the time-course patterns of NO3−-N disappearance during incubation under intertidal and subtidal conditions and the patterns of breakthrough curves (BTCs) of NO3−-N with a conservative tracer (Br−) during miscible displacement experiment. Nitrate disappearance by denitrification was negligible for SMG soils, but was 1.6 and 2.3mgNkg−1 soil day−1 under intertidal and subtidal conditions for GH soils, respectively. The BTCs of NO3−-N and Br− were identical and followed Gaussian distributions in SMG tidal-flats, while those obtained for GH tidal-flats were broad and asymmetrical. Calculated Pêclet number of Br− in seawater matrix by fitting the CXTFIT model to the measured BTCs was 45.03 for SMG and 4.93 for GH tidal-flats, indicating dominance of advection over dispersion for the former, and vice versa for the latter. From a mass balance of NO3−-N, nearly all of the added NO3−-N (38.8mg) was recovered in the effluents with a slight unaccounted-for portion (2.8mg) in SMG system, indicating the possibility of an intense off-shore NO3−-N discharge (leaching) from the tidal-flats. In contrast, a considerably large amount (27.0mg) of added NO3−-N was not recovered in GH system but nearly one-third (13.5mg) was recovered in the effluents, suggesting that denitrification dominates over off-shore discharge in NO3−-N removal. Our results showed that the patterns of NO3−-N removal was different depending on soil texture of the tidal-flats and that a dominant mechanism of NO3−-N removal was denitrification in GH tidal-flats and was off-shore discharge in SMG tidal-flats. Therefore, NO3−-N removal characteristics of tidal-flats should be predetermined for site-specific management of waste water N loadings to coastal water systems.
•Nitrate transport and removal was different in texturally contrasting tidal-flats.•The Pêclet number reflected NO3− transport characteristics affected by soil texture.•Advection dominated over dispersion in coarser tidal-flats, or vice versa.•Off-shore NO3− discharge was intense due to advection in coarse tidal-flats.•Denitrification dominated over off-shore discharge in NO3− loss for fine tidal-flats. |
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AbstractList | Tidal-flats play important roles in oceanic nitrogen (N) cycles. Particularly, N loss in the tidal-flats depends on soil texture and yet the dominant N removal mechanism in relation to soil texture is not clear. Therefore, the objective of this study was to investigate the effect of soil texture on NO3−-N removal and transport in texturally contrasting tidal-flats of the western coast of Korea [Gangwha (GH, silt) and Saemangeum (SMG, loamy sand) sites]. To interpret the experimental results, we compared the time-course patterns of NO3−-N disappearance during incubation under intertidal and subtidal conditions and the patterns of breakthrough curves (BTCs) of NO3−-N with a conservative tracer (Br−) during miscible displacement experiment. Nitrate disappearance by denitrification was negligible for SMG soils, but was 1.6 and 2.3mgNkg−1 soil day−1 under intertidal and subtidal conditions for GH soils, respectively. The BTCs of NO3−-N and Br− were identical and followed Gaussian distributions in SMG tidal-flats, while those obtained for GH tidal-flats were broad and asymmetrical. Calculated Pêclet number of Br− in seawater matrix by fitting the CXTFIT model to the measured BTCs was 45.03 for SMG and 4.93 for GH tidal-flats, indicating dominance of advection over dispersion for the former, and vice versa for the latter. From a mass balance of NO3−-N, nearly all of the added NO3−-N (38.8mg) was recovered in the effluents with a slight unaccounted-for portion (2.8mg) in SMG system, indicating the possibility of an intense off-shore NO3−-N discharge (leaching) from the tidal-flats. In contrast, a considerably large amount (27.0mg) of added NO3−-N was not recovered in GH system but nearly one-third (13.5mg) was recovered in the effluents, suggesting that denitrification dominates over off-shore discharge in NO3−-N removal. Our results showed that the patterns of NO3−-N removal was different depending on soil texture of the tidal-flats and that a dominant mechanism of NO3−-N removal was denitrification in GH tidal-flats and was off-shore discharge in SMG tidal-flats. Therefore, NO3−-N removal characteristics of tidal-flats should be predetermined for site-specific management of waste water N loadings to coastal water systems.
•Nitrate transport and removal was different in texturally contrasting tidal-flats.•The Pêclet number reflected NO3− transport characteristics affected by soil texture.•Advection dominated over dispersion in coarser tidal-flats, or vice versa.•Off-shore NO3− discharge was intense due to advection in coarse tidal-flats.•Denitrification dominated over off-shore discharge in NO3− loss for fine tidal-flats. Tidal-flats play important roles in oceanic nitrogen (N) cycles. Particularly, N loss in the tidal-flats depends on soil texture and yet the dominant N removal mechanism in relation to soil texture is not clear. Therefore, the objective of this study was to investigate the effect of soil texture on NO3 --N removal and transport in texturally contrasting tidal-flats of the western coast of Korea [Gangwha (GH, silt) and Saemangeum (SMG, loamy sand) sites]. To interpret the experimental results, we compared the time-course patterns of NO3 --N disappearance during incubation under intertidal and subtidal conditions and the patterns of breakthrough curves (BTCs) of NO3 --N with a conservative tracer (Br-) during miscible displacement experiment. Nitrate disappearance by denitrification was negligible for SMG soils, but was 1.6 and 2.3mgNkg-1 soil day-1 under intertidal and subtidal conditions for GH soils, respectively. The BTCs of NO3 --N and Br- were identical and followed Gaussian distributions in SMG tidal-flats, while those obtained for GH tidal-flats were broad and asymmetrical. Calculated Peclet number of Br- in seawater matrix by fitting the CXTFIT model to the measured BTCs was 45.03 for SMG and 4.93 for GH tidal-flats, indicating dominance of advection over dispersion for the former, and vice versa for the latter. From a mass balance of NO3 --N, nearly all of the added NO3 --N (38.8mg) was recovered in the effluents with a slight unaccounted-for portion (2.8mg) in SMG system, indicating the possibility of an intense off-shore NO3 --N discharge (leaching) from the tidal-flats. In contrast, a considerably large amount (27.0mg) of added NO3 --N was not recovered in GH system but nearly one-third (13.5mg) was recovered in the effluents, suggesting that denitrification dominates over off-shore discharge in NO3 --N removal. Our results showed that the patterns of NO3 --N removal was different depending on soil texture of the tidal-flats and that a dominant mechanism of NO3 --N removal was denitrification in GH tidal-flats and was off-shore discharge in SMG tidal-flats. Therefore, NO3 --N removal characteristics of tidal-flats should be predetermined for site-specific management of waste water N loadings to coastal water systems. |
Author | Ro, Hee-Myong Hwang, Sang-Il Lee, Min-Jin |
Author_xml | – sequence: 1 givenname: Min-Jin orcidid: 0000-0001-8955-586X surname: Lee fullname: Lee, Min-Jin organization: Department of Agricultural Biotechnology and Research Institute of Agriculture and Life Sciences, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul 151-921, Korea – sequence: 2 givenname: Sang-Il surname: Hwang fullname: Hwang, Sang-Il organization: Environmental Policy Research Group, Korea Envionment Institute, 215 Jinheungno, Eunpyeong-gu, Seoul 122-706, Korea – sequence: 3 givenname: Hee-Myong orcidid: 0000-0001-5437-3484 surname: Ro fullname: Ro, Hee-Myong email: hmro@snu.ac.kr organization: Department of Agricultural Biotechnology and Research Institute of Agriculture and Life Sciences, Seoul National University, 1 Gwanak-ro, Gwanak-gu, Seoul 151-921, Korea |
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SubjectTerms | Breakthrough curve (BTC) Discharge Effluents Nitrate Offshore engineering Offshore structures Soil (material) Soil texture Solute transport Surface layer Texture Tidal-flat Transport |
Title | Interpreting the effect of soil texture on transport and removal of nitrate-N in saline coastal tidal flats under steady-state flow condition |
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