Relative influence of watershed and geomorphic features on nutrient and carbon fluxes in a pristine and moderately urbanized stream

被引:5
|
作者
Tremblay, Charles Charrier [1 ]
Botrel, Morgan [1 ]
Lapierre, Jean-Francois [1 ]
Franssen, Jan [2 ]
Maranger, Roxane [1 ]
机构
[1] Univ Montreal, GRIL, Dept Sci Biol, Montreal, PQ, Canada
[2] Univ Montreal, GRIL, Dept Geog, Montreal, PQ, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Streams; Nutrients; Carbon; Retention; Geomorphic structures; Urbanization; Land use and land cover; DISSOLVED ORGANIC-CARBON; NITROGEN FLUXES; NITRATE REMOVAL; SURFACE WATERS; LAND-USE; ECOSYSTEMS; RETENTION; DENITRIFICATION; RESTORATION; PHOSPHORUS;
D O I
10.1016/j.scitotenv.2019.136411
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Streams are important sites of elemental transformations due to the relatively high contact rates between flowing water and biogeochemically reactive sediments. Increased urbanization typically results in higher nutrient and carbon (C) inputs to streams from their watersheds and increased flow rates due to modification in channel form, reducing within stream net retention and increasing downstream exports. However, less is known on how moderate urbanization might influence the joint processing of C, nitrogen (N), and phosphorus (P) in streams or the relative influence of changes in watershed and stream features on their fluxes. In this study, we performed mass-balances of different C, N, and P species in multiple reaches with contrasting land use land cover and geomorphic features (pools, riffles, runs) to determine the effects of geomorphology versus human influence on elemental fluxes in a pristine and a semi-urban stream. N was the most responsive of all elements, where nitrate concentrations were 3.5-fold higher in the pen-urban stream. Dissolved organic carbon was only slightly higher in the pen-urban site whereas total P not significantly different between streams. In terms of fluxes, nitrate behaved differently between the streams with net retention occurring in the majority of the reaches of the pristine site, whereas net export was observed in all of the reaches of the semi-urban one. We found a decrease in nitrate concentrations with an increase in excess deuterium of the water (d-excess), an indicator of how overall water retention capacity of the watershed favored N loss. Within the stream, the presence of pools, and reduced channel slope, which also increase water retention time, again favored N loss. Overall, nitrate was the most sensitive nutrient to slight urbanization, where higher export to stream was influenced by land use, but where geomorphic features were more important in driving retention capacity. (C) 2020 Elsevier B.V. All rights reserved.
引用
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页数:10
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