Abstract
Against the backdrop of recent climate change issues, the intensity of dry periods is increasing in semi-arid environments due to high temperatures, evaporation and a shortage of precipitation in summer. The Tafna catchment, which is located in north-western Algeria and is characterised by a Mediterranean climate with a sub-dry tendency, has been subject to severe and prolonged dry periods. In order to understand the impact of prolonged dry periods on biogeochemical processes and nutrient exchange between surface water (SW) and hyporheic water (HW) within the (study) catchment, four sets of samples were taken upstream of the Tafna wadi during low-water (LW) periods over two years (2014–2015). Nitrate, nitrite, ammonium and chloride were measured in surface water (SW) and hyporheic water (HW) at depths of 30, 60 and 100 cm. The results showed a significant loss of nitrate and a considerable increase in ammonium in the hyporheic zone (HZ) during these severe conditions. This could be related to (i) high rates of denitrification and (ii) the process of dissimilatory nitrate reduction to ammonium (DNRA). This study indicated that a severe drought directly affects the nitrogen cycle that occurs in a hyporheic zone (HZ), and thus affects the functioning of this area relative to the wadi system as a whole.
Similar content being viewed by others
References
Baldwin DS, Mitchell AM (2000) The effects of drying and re-flooding on the sediment and soil nutrient dynamics of lowland river–floodplain systems: a synthesis. Regul River Res Manag Int J Devot River Res Manag 16(5):457–467
Baxter C, Hauer FR, Woessner WW (2003) Measuring groundwater–stream water exchange: new techniques for installing minipiezometers and estimating hydraulic conductivity. Trans Am Fish Soc 132(3):493–502
Bellmore RA, Compton JE, Brooks JR et al (2018) Nitrogen inputs drive nitrogen concentrations in US streams and rivers during summer low flow conditions. Sci Total Environ 639:1349–1359
Benabdelkader A, Taleb A, Probst JL, Belaidi N, Probst A (2018) Anthropogenic contribution and influencing factors on metal features in fluvial sediments from a semi-arid Mediterranean river basin (Tafna River, Algeria): a multi-indices approach. Sci Total Environ 626:899–914
Bencala KE (1993) A perspective on stream-catchment connections. J N Am Benthol Soc 12(1):44–47
Bou C (1974) Les méthodes de récolte dans les eaux souterraines interstitielles. Ann Spéléol 29(4):611–619
Bou C, Rouch R (1967) Un nouveau champ de recherches sur la faune aquatique souterraine. CR Acad Sci Paris 265(4):369–370
Butturini, A, Sabater, F (2002) Nitrogen concentrations in a small Mediterranean stream: 1. Nitrate 2. Ammonium. Hydrol Earth Syst Sci 6(3):539–550
Claret C, Boulton AJ (2009) Integrating hydraulic conductivity with biogeochemical gradients and microbial activity along river–groundwater exchange zones in a subtropical stream. Hydrogeol J 17(1):151
Constantz J, Thomas CL, Zellweger G (1994) Influence of diurnal variations in stream temperature on streamflow loss and groundwater recharge. Water Resour Res 30(12):3253–3264
Crimo CP, McDonnell JJ (1997) Linking the hydrological and biogeochemical controls of nitrogen transport in near-stream zones of temperate-forested catchments: a review. J Hydrol 199:88–120
Dahm CN, Trotter EH, Sedell JR (1987) Role of anaerobic zones and processes in stream ecosystem productivity. Chem Qual Water Hydrol Cycle 157–178
Dahm CN, Baker MA, Moore DI, Thibault JR (2003) Coupled biogeochemical and hydrological responses of streams and rivers to drought. Freshw Biol 48(7):1219–1231
Danielopol DL (1989) Groundwater fauna associated with riverine aquifers. J N Am Benthol Soc 8(1):18–35
Datry T, Foulquier A, Corti R et al (2018) A global analysis of terrestrial plant litter dynamics in non-perennial waterways. Nat Geosci 1
Davies BE (1974) Loss-on-ignition as an estimate of soil organic matter 1. Soil Sci Soc Am J 38(1):150–151
Descloux S, Datry T, Philippe M, Marmonier P (2010) Comparison of different techniques to assess surface and subsurface streambed colmation with fine sediments. Int Rev Hydrobiol 95(6):520–540
Fisher SG, Likens GE (1973) Energy flow in Bear Brook, New Hampshire: an integrative approach to stream ecosystem metabolism. Ecol Monogr 43(4):421–439
Fisher SG, Grimm NB, Martí E, Gómez R (1998) Hierarchy, spatial configuration, and nutrient cycling in a desert stream. Aust J Ecol 23(1):41–52
García-García V, Gómez R, Vidal-Abarca MR, Suárez ML (2013) Subsurface N retention in two Mediterranean wetland-streams affected by agricultural runoff. Wetlands 33(4):597–608
Giorgi F (2006) Climate change hot-spots. Geophys Res Lett 33(8):L08707
Giorgi F, Lionello P (2008) Climate change projections for the Mediterranean region. Glob Planet Chang 63(2–3):90–104
Gomez JD, Wilson JL, Cardenas MB (2012) Residence time distributions in sinuosity-driven hyporheic zones and their biogeochemical effects. Water Resour Res 48(9):W09533
Gomez-Velez JD, Krause S, Wilson JL (2014) Effect of low-permeability layers on spatial patterns of hyporheic exchange and groundwater upwelling. Water Resour Res 50(6):5196–5215
Gregory SV, Swanson FJ, McKee WA, Cummins KW (1991) An ecosystem perspective of riparian zones. Bioscience 41(8):540–551
Grimm NB, Fisher SG (1984) Exchange between interstitial and surface water: implications for stream metabolism and nutrient cycling. Hydrobiologia 111(3):219–228
Haddou K, Bendaoud A, Belaidi N, Taleb A (2018) A large-scale study of hyporheic nitrate dynamics in a semi-arid catchment, the Tafna River, Northwest Algeria. Environ Earth Sci 77(13):520
Holmes RM, Fisher SG, Grimm NB (1994) Parafluvial nitrogen dynamics in a desert stream ecosystem. J N Am Benthol Soc 13(4):468–478
Holmes RM, Jones JB, Fisher SG, Grimm NB (1996) Denitrification in a nitrogen-limited stream ecosystem. Biogeochemistry 33(2):125–146
Humphries P, Baldwin DS (2003) Drought and aquatic ecosystems: an introduction. Freshw Biol 48(7):1141–1146
Hynes HBN, Hynes HBN (1970) The ecology of running waters, vol 555. Liverpool University Press, Liverpool
Jones JB (2002) Groundwater controls on nutrient cycling in a Mojave desert stream. Freshw Biol 47(5):971–983
Jones JB Jr, Holmes RM (1996) Surface-subsurface interactions in stream ecosystems. Trends Ecol Evol 11(6):239–242
Käser DH, Binley A, Heathwaite AL, Krause S (2009) Spatio-temporal variations of hyporheic flow in a riffle-step-pool sequence. Hydrol Process Int J 23(15):2138–2149
Kelso BH, Smith RV, Laughlin RJ (1999) Effects of carbon substrates on nitrite accumulation in freshwater sediments. Appl Environ Microbiol 65(1):61–66
Kemp MJ, Dodds WK (2001) Centimeter-scale patterns in dissolved oxygen and nitrification rates in a prairie stream. J N Am Benthol Soc 20(3):347–357
Lange J, Haensler A (2012) Runoff generation following a prolonged dry period. J Hydrol 464:157–164
Larned ST, Datry T, Arscott DB, Tockner K (2010) Emerging concepts in temporary-river ecology. Freshw Biol 55(4):717–738
Lefebvre S, Marmonier P, Pinay G (2004) Stream regulation and nitrogen dynamics in sediment interstices: comparison of natural and straightened sectors of a third-order stream. River Res Appl 20(5):499–512
Marmonier P, Des Châtelliers MC (1991) Effects of spates on interstitial assemblages of the Rhône River, Importance of spatial heterogeneity. Hydrobiologia 210(3):243–251
McClain ME, Boyer EW, Dent CL et al (2003) Biogeochemical hot spots and hot moments at the interface of terrestrial and aquatic ecosystems. Ecosystems 6(4):301–312
Megnounif A, Terfous A, Ghenaim A, Poulet JB (2007) Key processes influencing erosion and sediment transport in a semi-arid Mediterranean area: the Upper Tafna catchment, Algeria/Processus clefs influençant l'érosion et le transport des sédiments dans une région semi-aride Méditerranéenne: le bassin versant de la Haute Tafna, Algérie. Hydrol Sci J J Sci Hydrol 52(6):1271–1284
Mora-Gómez J, Duarte S, Cássio F, Pascoal C, Romaní AM (2018) Microbial decomposition is highly sensitive to leaf litter emersion in a permanent temperate stream. Sci Total Environ 621:486–496
Poff NL, Ward JV (1989) Implications of streamflow variability and predictability for lotic community structure: a regional analysis of streamflow patterns. Can J Fish Aquat Sci 46(10):1805–1818
Resh VH, Brown AV, Covich AP et al (1988) The role of disturbance in stream ecology. J N Am Benthol Soc 7(4):433–455
Sabater S, Tockner K (2009) Effects of hydrologic alterations on the ecological quality of river ecosystems. Water scarcity in the Mediterranean. Springer, Berlin, pp 15–39
Skoulikidis NT, Sabater S, Datry T et al (2017) Non-perennial Mediterranean rivers in Europe: status, pressures, and challenges for research and management. Sci Total Environ 577:1–18
Stanley EH, Valett HM (1992) Interactions between drying and the hyporheic zone of a desert stream. Global climate change and freshwater ecosystems. Springer, New York, pp 234–249
Stewardson MJ, Datry T, Lamouroux N, Pella H, Thommeret N, Valette L, Grant SB (2016) Variation in reach-scale hydraulic conductivity of streambeds. Geomorphology 259:70–80
Storey RG, Howard KW, Williams DD (2003) Factors controlling riffle-scale hyporheic exchange flows and their seasonal changes in a gaining stream: a three-dimensional groundwater flow model. Water Resour Res 39(2):1034
Storey RG, Williams DD, Fulthorpe RR (2004) Nitrogen processing in the hyporheic zone of a pastoral stream. Biogeochemistry 69(3):285–313
Taleb A, Belaidi N, Sanchez-Pérez JM, Vervier P, Sauvage S, Gagneur J (2008) Retention of nitrogen within a semi-arid gravel bed stream located downstream to a heavy polluted reservoir (Tafna River, Algeria): role of the hyporheic zone. River Res Appl 24:183–196
Triska FJ, Duff JH, Avanzino RJ (1993) The role of water exchange between a stream channel and its hyporheic zone in nitrogen cycling at the terrestrial—aquatic interface. Nutrient dynamics and retention in land/water ecotones of Lowland, Temperate Lakes and Rivers. Springer, Dordrecht, pp 167–184
Triska FJ, Jackman AP, Duff JH, Avanzino RJ (1994) Ammonium sorption to channel and riparian sediments: a transient storage pool for dissolved inorganic nitrogen. Biogeochemistry 26(2):67–83
Vannote RL, Minshall GW, Cummins KW, Sedell JR, Cushing CE (1980) The river continuum concept. Can J Fish Aquat Sci 37(1):130–137
Wilhite DA (2000) Drought as a natural hazard: concepts and definitions. In: Drought: a global assessment. Routledge, London, pp 3–18
Williams DD (1993) Nutrient and flow vector dynamics at the hyporheic/groundwater interface and their effects on the interstitial fauna. Nutrient dynamics and retention in land/water ecotones of Lowland, Temperate Lakes and Rivers. Springer, Dordrecht, pp 185–198
Zettam A, Taleb A, Sauvage S, Boithias L, Belaidi N, Sánchez-Pérez JM (2017) Modelling hydrology and sediment transport in a semi-arid and anthropized catchment using the SWAT model: the case of the Tafna river (northwest Algeria). Water 9(3):216
Acknowledgments
The authors thank the laboratory staff at LECGEN for their help with laboratory analysis and the National Agency of Hydrologic Resources (ANRH) in Oran for providing data on the Tafna’s discharge. We are particularly grateful to Amina Rezougui and Amine Benabedlkader for their help with field sampling and to Amine Zettam for his help with producing the map.
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
About this article
Cite this article
Zenagui, I., Belaidi, N., Benkebil, Z. et al. Nutrient dynamics in a hyporheic zone in response to a severe and prolonged dry period in a semi-arid river (Tafna wadi). Environ Earth Sci 79, 35 (2020). https://doi.org/10.1007/s12665-019-8780-4
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s12665-019-8780-4