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Ministerio de Universidades - Gobierno de España

Título: THE INFLUENCE OF MEDITERRANEAN RIPARIAN ZONES ON STREAM NITROGEN DYNAMICS: A CATCHMENT APPROACH
Autor: Lupon Navazo, Anna
Universidad: Universidad de Barcelona
Departamento: C- ECOLOGIA
Fecha de Lectura: 16/11/2015
Programa de doctorado: Ecologia Fonamental i Aplicada
Dirección:
- BERNAL BERENGUER, SUSANA (DIRECTOR)
- Sabater Comas, Francesc (CODIRECTOR)
Tribunal:
- Pinay, Gilles (PRESIDENTE)
- MARCÉ ROMERO, RAFAEL (SECRETARIO)
- Llorens García, Pilar (VOCAL)
Descriptores:
- HIDROBIOLOGIA
- AGUAS SUPERFICIALES
- BIOQUIMICA DE SUELOS
- LIMNOLOGIA
Marcador: https://www.educacion.gob.es/teseo/mostrarRef.do?ref=1192341Añadir a favoritos.
Resumen:
Riparian areas are recognized to be natural filters of nitrogen (N) because they can substantially diminish the N delivery from terrestrial to aquatic ecosystems. However, understanding the influence of riparian zones on regulating N export from catchments is still challenging, mainly because stream water chemistry integrates biogeochemical processes co-occurring within upland, riparian, and fluvial ecosystems. The present dissertation aims to explore the influence of Mediterranean riparian zones on regulating both stream hydrology and catchment N exports, by combining empirical and modelling approaches at different temporal and spatial scales. Findings obtained from plot experiments show that the studied Mediterranean riparian soils acted as hot spots of soil microbial N supply within the catchment because they exhibited considerably higher net N mineralization (NNM) and net nitrification (NN) rates than upland oak and beech soils. This difference was attributed to larger stocks of N-rich leaf litter and permanent moist conditions in the riparian soils. Furthermore, soil microbial processes in the riparian site showed a distinct climatic sensitivity than in upland sites, which ultimately led to different temporal patterns of soil N cycling. Soil moisture was the major driver of NNM and NN in upland forests, while both temperature and precipitation shaped soil N dynamics in the riparian zone. Therefore, both upland and riparian soils exhibited pulses of NNM and NN following spring rewetting events, though summer temperatures only stimulate microbial activity at the riparian site. Riparian microbial pulses contributed > 25% to annual rates of NNM and NN; and coincided with increases in stream N loads. These results suggest that Mediterranean riparian soils may become important sources of nitrate (NO3-) to streams under future warming scenarios. Additionally, findings obtained from catchment-scale studies show that our Mediterranean riparian zone exerted a strong control on stream hydrology during the vegetative period. Riparian evapotranspiration (ET) influenced the temporal pattern of stream discharge and riparian groundwater elevation across daily and seasonal scales. Further, the influence of riparian ET on stream hydrology increased from headwaters to the valley bottom, where stream hydrological retention was prominent. Nonetheless, such stream hydrological retention was not accompanied by a decrease in catchment N exports, likely because low flow conditions, relatively warm conditions, and large stocks of N-rich leaf litter within the streambed enhanced in-stream NO3- release in summer. Conversely, in-stream photoautotrophic NO3- uptake was the major controlling factor of stream N dynamics in spring, when high light inputs favored gross primary productivity (GPP) prior to riparian canopy closure. As it occurred for summer nitrification, the influence of GPP on stream N dynamics increased along the stream continuum. At the valley bottom, in-stream photoautotrophic activity drop midday stream N concentration by 13% and reduced catchment NO3- exports by 10%. Finally, during the dormant period, we found minimal evidences of either NO3- uptake or release in the riparian zone. Together, these findings suggest that the high bioreactivity of streams ecosystems can influence stream N dynamics at the catchment scale, and even screen the potential buffer capacity of riparian zones. Accordingly, our mass balance calculations showed that both riparian groundwater inputs and in-stream processes equally contributed to longitudinal changes in stream NO3- concentrations, and thus, both source of variation are necessary to understand stream N dynamics at relevant ecological scales. Overall, findings gathered in the present dissertation question the idea that Mediterranean riparian zones are efficient N buffers, and stress that an integrated view of upland, riparian, and stream ecosystems is essential for advancing our understanding of catchment hydrology and biogeochemistry.

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