Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment

The transport of nitrogen (N) to groundwater and surface water in the form of nitrate (NO3-), as a by-product of the application of N-rich fertilisers, has been studied extensively. Yet, in the catchments adjacent to the Great Barrier Reef (GBR) in tropical north Queensland, Australia, NO3- transpor...

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Main Authors: Jim Stanley, Lucy Reading
Format: Article
Language:English
Published: Elsevier 2020-12-01
Series:Heliyon
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2405844020323501
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spelling doaj-475f51d4494e4ff896ebe5454819b4bb2021-01-05T09:21:43ZengElsevierHeliyon2405-84402020-12-01612e05507Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchmentJim Stanley0Lucy Reading1Corresponding author.; Queensland University of Technology, 2 George St, Brisbane City, 4000, QLD, AustraliaQueensland University of Technology, 2 George St, Brisbane City, 4000, QLD, AustraliaThe transport of nitrogen (N) to groundwater and surface water in the form of nitrate (NO3-), as a by-product of the application of N-rich fertilisers, has been studied extensively. Yet, in the catchments adjacent to the Great Barrier Reef (GBR) in tropical north Queensland, Australia, NO3- transport in groundwater is not regularly monitored. An assessment of groundwater chemistry in the Liverpool Creek catchment of Queensland's wet-tropics region was conducted by regular sampling and analysis of groundwater over 12 months, through wet and dry seasons. A distinct spatial variability in groundwater chemistry was observed; groundwater aquifers with very low dissolved oxygen (DO) and NO3- consistently displayed relatively higher concentrations of sulphate (SO42-), sulphur (S2-) and ferrous iron (Fe2+) and low concentrations of dissolved organic carbon (DOC) (<2 ppm). Combined with averaged measured redox potential (Eh) of <250 mV, this indicates certain regions of the catchment have conditions favourable for removal of NO3- via autotrophic denitrification (DN), while other groundwater aquifers retained NO3 – concentrations just above the acceptable trigger limits defined in regional water quality guidelines. Observations indicate that the naturally heterogeneous structure of the coastal alluvium contributes to the distinct variability in groundwater chemistry over small distances, with NO3- concentrations influenced by a combination of DN, lateral shallow drainage and potential adsorption to clay surfaces within the alluvial sediments.http://www.sciencedirect.com/science/article/pii/S2405844020323501GroundwaterNitrateSugarcaneTropicsSulphateDenitrification
collection DOAJ
language English
format Article
sources DOAJ
author Jim Stanley
Lucy Reading
spellingShingle Jim Stanley
Lucy Reading
Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
Heliyon
Groundwater
Nitrate
Sugarcane
Tropics
Sulphate
Denitrification
author_facet Jim Stanley
Lucy Reading
author_sort Jim Stanley
title Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
title_short Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
title_full Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
title_fullStr Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
title_full_unstemmed Nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
title_sort nitrate dynamics in groundwater under sugarcane in a wet-tropics catchment
publisher Elsevier
series Heliyon
issn 2405-8440
publishDate 2020-12-01
description The transport of nitrogen (N) to groundwater and surface water in the form of nitrate (NO3-), as a by-product of the application of N-rich fertilisers, has been studied extensively. Yet, in the catchments adjacent to the Great Barrier Reef (GBR) in tropical north Queensland, Australia, NO3- transport in groundwater is not regularly monitored. An assessment of groundwater chemistry in the Liverpool Creek catchment of Queensland's wet-tropics region was conducted by regular sampling and analysis of groundwater over 12 months, through wet and dry seasons. A distinct spatial variability in groundwater chemistry was observed; groundwater aquifers with very low dissolved oxygen (DO) and NO3- consistently displayed relatively higher concentrations of sulphate (SO42-), sulphur (S2-) and ferrous iron (Fe2+) and low concentrations of dissolved organic carbon (DOC) (<2 ppm). Combined with averaged measured redox potential (Eh) of <250 mV, this indicates certain regions of the catchment have conditions favourable for removal of NO3- via autotrophic denitrification (DN), while other groundwater aquifers retained NO3 – concentrations just above the acceptable trigger limits defined in regional water quality guidelines. Observations indicate that the naturally heterogeneous structure of the coastal alluvium contributes to the distinct variability in groundwater chemistry over small distances, with NO3- concentrations influenced by a combination of DN, lateral shallow drainage and potential adsorption to clay surfaces within the alluvial sediments.
topic Groundwater
Nitrate
Sugarcane
Tropics
Sulphate
Denitrification
url http://www.sciencedirect.com/science/article/pii/S2405844020323501
work_keys_str_mv AT jimstanley nitratedynamicsingroundwaterundersugarcaneinawettropicscatchment
AT lucyreading nitratedynamicsingroundwaterundersugarcaneinawettropicscatchment
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