Abstract
Abstract. The storage and release of water in soils is critical for sustaining plant transpiration and groundwater recharge. However, how much subsurface mixing of water occurs, and how much of the water is available for plants or otherwise percolates to streams and the groundwater is not yet understood. Based on stable isotope (2H and 18O) data, some studies have found that water infiltrating into soils can bypass older pore water. However, the mechanisms leading to the separation of water routed to the streams and water held tightly in smaller pores are still unclear. Here, we address the current limitations of the understanding of subsurface mixing and their consequences regarding the application of stable isotopes in ecohydrological studies. We present an extensive data set, for which we sampled the isotopic composition of mobile and bulk soil water in parallel with groundwater at a fortnightly temporal resolution and stream water and rainfall at a much higher resolution in a Mediterranean long-term research catchment, in Vallcebre, Spain. The data reveal that the mobile and tightly bound water of a silty loam soil in a Scots pine forest do not mix well; however, they constitute two disjunct subsurface water pools with little exchange, despite intense rainfall events leading to high soil wetness. We show that the isotopic compartmentalization results from the rewetting of small soil pores by isotopically depleted winter/spring rain. Thus, stable isotopes, and, in turn, water residence times, do not only vary across soil depth, but also across soil pores. Our findings have important implications for stable isotope applications in ecohydrological studies assessing the water uptake by plants or the process realism of hydrological models, as the observed processes are currently rarely implemented in the simulation of water partitioning into evapotranspiration and recharge in the critical zone.
Highlights
Rainfall infiltrating into soils often does not replace already stored water in the soil pores as described by translatory flow (Hewlett and Hibbert, 1967; Fig. S1 in the Supplement of this paper), and it can bypass large amounts of water held in pores prior to infiltration (Beven and Germann, 1982)
We found that the mobile water was more enriched in heavy isotopes than the bulk soil water for each sampling campaign
The mechanism by which different isotopic compositions for the mobile and tightly bound soil water develop at the plot scale have not previously been presented
Summary
Rainfall infiltrating into soils often does not replace already stored water in the soil pores as described by translatory flow (Hewlett and Hibbert, 1967; Fig. S1 in the Supplement of this paper), and it can bypass large amounts of water held in pores prior to infiltration (Beven and Germann, 1982). M. Sprenger et al.: Mechanisms of consistently disjunct soil water pools over (pore) space and time between mobile and bulk soil water, as it is the water in the pore space fraction that is not accessible by suction lysimeter. Sprenger et al.: Mechanisms of consistently disjunct soil water pools over (pore) space and time between mobile and bulk soil water, as it is the water in the pore space fraction that is not accessible by suction lysimeter It was hypothesized by Brooks et al (2010) that rainwater refilling the dry soil at the end of a dry season would lead to a distinct signal between mobile and tightly bound water. Understanding the stable isotopic composition and its variation in space and time is essential in the application of stable isotopes of water for paleoclimatological tree ring analyses (Gessler et al, 2014), plant water uptake assessments (Dubbert and Werner, 2019), partitioning between soil evaporation and transpiration (Wang et al, 2010), testing atmosphere–land surface models (Haese et al, 2013), understanding runoff processes (Klaus and McDonnell, 2013), and water residence time estimates (Sprenger et al, 2019)
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