Environmental tracers and indicators bringing together groundwater, surface water and groundwater-dependent ecosystems: importance of scale in choosing relevant tools

被引:45
作者
Bertrand, G. [1 ]
Siergieiev, D. [2 ]
Ala-Aho, P. [3 ]
Rossi, P. M. [3 ]
机构
[1] Univ Sao Paulo, Inst Geociencias, CEPAS Groundwater Res Ctr, BR-01498 Sao Paulo, Brazil
[2] Lulea Univ Technol, S-97187 Lulea, Sweden
[3] Univ Oulu, Dept Proc & Environm Engn, Water Resources & Environm Engn Lab, Oulu 90014, Finland
关键词
Groundwater-dependent ecosystems; Environmental tracers; Hyporheic zone; GW-SW interaction; Indicators; SALMON SPAWNING GRAVELS; HYPORHEIC ZONE; ELECTRICAL-CONDUCTIVITY; BANK FILTRATION; NATURAL TRACER; TIME-SERIES; STREAM; TEMPERATURE; FLOW; MANAGEMENT;
D O I
10.1007/s12665-013-3005-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Groundwater-surface water (GW-SW) interactions cover a broad range of hydrogeological and biological processes and are controlled by natural and anthropogenic factors at various spatio-temporal scales, from watershed to hyporheic/hypolentic zone. Understanding these processes is vital in the protection of groundwater-dependent ecosystems increasingly required in water resources legislation across the world. The use of environmental tracers and indicators that are relevant simultaneously for groundwater, surface water and biocenoses-biotope interactions constitutes a powerful tool to succeed in the management task. However, tracer type must be chosen according to the scale of interest and tracer use thus requires a good conceptual understanding of the processes to be evaluated. This paper reviews various GW-SW interaction processes and their drivers and, based on available knowledge, systemises application of conservative tracers and semi-conservative and reactive environmental indicators at different spatial scales. Biocenoses-biotopes relationships are viewed as a possible transition tool between scales. Relation between principal application of the environmental tracers and indicators, examples and guidelines are further proposed for examining GW-SW interactions from a hydrogeological and biological point of view by demonstrating the usability of the tracers/indicators and providing recommendations for the scientific community and decision makers.
引用
收藏
页码:813 / 827
页数:15
相关论文
共 105 条
[21]  
Constantz J., 2003, Heat as a tool for studying the movement of ground water near streams, P1, DOI [10.3133/cir1260, DOI 10.3133/CIR1260]
[22]   Quantifying groundwater discharge to Cockburn River, southeastern Australia, using dissolved gas tracers 222Rn and SF6 [J].
Cook, P. G. ;
Lamontagne, S. ;
Berhane, D. ;
Clark, J. F. .
WATER RESOURCES RESEARCH, 2006, 42 (10)
[23]   Estimating groundwater discharge to rivers from river chemistry surveys [J].
Cook, Peter G. .
HYDROLOGICAL PROCESSES, 2013, 27 (25) :3694-3707
[24]   Predicting export of dissolved organic carbon from forested catchments in glaciated landscapes with shallow soils [J].
Creed, I. F. ;
Beall, F. D. ;
Clair, T. A. ;
Dillon, P. J. ;
Hesslein, R. H. .
GLOBAL BIOGEOCHEMICAL CYCLES, 2008, 22 (04)
[25]   Incorporating ecological perspectives in European groundwater management policy [J].
Danielopol, DL ;
Gibert, J ;
Griebler, C ;
Gunatilaka, A ;
Hahn, HJ ;
Messana, G ;
Notenboom, J ;
Sket, B .
ENVIRONMENTAL CONSERVATION, 2004, 31 (03) :185-189
[26]   Incorporating the hyporheic zone within the river discontinuum: Longitudinal patterns of subsurface copepod assemblages in an Alpine stream [J].
Di Lorenzo, Tiziana ;
Stoch, Fabio ;
Galassi, Diana M. P. .
LIMNOLOGICA, 2013, 43 (04) :288-296
[27]   A functional methodology for determining the groundwater regime needed to maintain the health of groundwater-dependent vegetation [J].
Eamus, D ;
Froend, R ;
Loomes, R ;
Hose, G ;
Murray, B .
AUSTRALIAN JOURNAL OF BOTANY, 2006, 54 (02) :97-114
[28]   Comparison of tracer methods to quantify hydrodynamic exchange within the hyporheic zone [J].
Engelhardt, I. ;
Piepenbrink, M. ;
Trauth, N. ;
Stadler, S. ;
Kludt, C. ;
Schulz, M. ;
Schueth, C. ;
Ternes, T. A. .
JOURNAL OF HYDROLOGY, 2011, 400 (1-2) :255-266
[29]   Whole-stream metabolism in two montane streams: Contribution of the hyporheic zone [J].
Fellows, CS ;
Valett, HM ;
Dahm, CN .
LIMNOLOGY AND OCEANOGRAPHY, 2001, 46 (03) :523-531
[30]   Attenuation of mining-derived pollutants in the hyporheic zone: A review [J].
Gandy, C. J. ;
Smith, J. W. N. ;
Jarvis, A. P. .
SCIENCE OF THE TOTAL ENVIRONMENT, 2007, 373 (2-3) :435-446