Ricardo González-PinzónUniversity of New Mexico | UNM · Department of Civil, Construction & Environmental Engineering
Ricardo González-Pinzón
Ph.D. in Water Resources Engineering
Professor of Water Resources Engineering
About
65
Publications
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Introduction
I couple experimental (field and laboratory) observations with mathematical and statistical analyses to 1) investigate sub-hour-to-multidecade variability of mass and energy fluxes, scaling patterns, and the coupling between natural and human systems, and 2) propose actionable science aimed at improving the sustainable use of ecosystem services, particularly those concerning the supply and demand of food, energy, and water resources.
Additional affiliations
September 2009 - May 2013
July 2013 - July 2019
February 2006 - June 2008
Publications
Publications (65)
Wildfires are increasing globally in frequency, severity, and extent, but their impact on fluvial networks, and the resources they provide, remains unclear. We combine remote sensing of burn perimeter and severity, in-situ water quality monitoring, and longitudinal modeling to create the first large-scale, long-term estimates of stream+river length...
Climate change is causing pronounced shifts during winter in the US, including shortening the snow season, reducing snowpack, and altering the timing and volume of snowmelt-related runoff. These changes in winter precipitation patterns affect in-stream freeze-thaw cycles, including ice and snow cover, and can trigger direct and indirect effects on...
Despite advances in wastewater treatment plant (WWTP) efficiencies, multiple contaminants of concern, such as
microplastics, pharmaceuticals, and per- and poly-fluoroalkyl substances (PFAS) remain largely untreated near
discharge points and can be highly concentrated before they are fully mixed within the receiving river. Environmental
agencies enf...
Wildfire disturbance propagation along fluvial networks remains poorly understood. We use incident, atmospheric, and water-quality data from the largest wildfire in New Mexico’s history to quantify how this gigafire affected surface runoff processes and mobilized wildfire disturbances into fluvial networks after burning 1382 km². Surface runoff pos...
Land cover changes alter hydrologic (e.g., infiltration-runoff), biochemical (e.g., nutrient loads), and ecological processes (e.g., stream metabolism). We quantified differences in aquatic ecosystem respiration in two contrasting stream reaches from a forested watershed in Colorado (1st-order reach) and an agricultural watershed in Iowa (3rd-order...
Most freshwater aquatic studies rely on Eulerian monitoring, i.e., water quality and quantity are monitored using grab samples or semi-continuous sensors deployed at fixed cross-sections. While Eulerian monitoring is practical, it provides a limited understanding of spatial and temporal heterogeneity. We designed and built The Navigator, a Lagrangi...
Many studies in ecohydrology focusing on hydrologic transport argue that longer residence times across a stream ecosystem should consistently result in higher biological uptake of carbon, nutrients, and oxygen. This consideration does not incorporate the potential for biologically mediated reactions to be limited by stoichiometric imbalances. Based...
Anthropogenic and natural disasters (e.g., wildfires, oil spills, mine spills, sewage treatment facilities) cause water quality disturbances in fluvial networks. These disturbances are highly unpredictable in space-time, with the potential to propagate through multiple stream orders and impact human and environmental health over days to years. Due...
We are developing a data-driven and machine learning-facilitated transformation of how we craft one-dimensional models for solute transport in rivers. After testing state-of-the-art 1-D models with hundreds of tracer tests performed worldwide, research has consistently shown that our current solute transport theory in river corridors misbehaves cat...
Many studies in ecohydrology focusing on hydrologic transport argue that longer residence times across a stream ecosystem should consistently result in higher biological uptake of carbon, nutrients, and oxygen. This consideration does not incorporate the potential for biologically mediated reactions to be limited by stoichiometric imbalances. Based...
Hyporheic exchange influences hydrologic transport and water quality through transient storage, which extends solute transit time, and leads to mixing of surface water and groundwater. Despite its importance, estimating the extent and spatiotemporal variability of the hyporheic zone remains challenging due to limitations in assessing the subsurface...
Despite their frequent use, there are few simple and readily accessible tools to help guide the logistical planning of tracer injections in streams and rivers. We combined the widely used advection-dispersion-reaction equation, peak concentration estimates based on a meta-analysis of hundreds of tracer injections carried out in streams and rivers,...
Though community-based scientific approaches are becoming more common, many scientific efforts are conducted by small groups of researchers that together develop a concept, analyze data, and interpret results that ultimately translate into a publication. Here, we present a community effort that breaks these traditional boundaries of the publication...
We evaluated groundwater quality, pollution, and its effects on human health in the eastern part of the Lake Urmia basin, the largest lake in the Middle East. Although groundwater quality is suitable for drinking and irrigation purposes, an index-based approach quantifying heavy metal pollution revealed that most sampling sites exhibited moderate t...
In this study, we explored opportunities to optimize food-energy-water (FEW) resources by closing nutrient loops in aridland rivers. We evaluated source and sink behavior of nitrogen as nitrate (NO3-N) in three connected channels associated with an irrigation network, i.e., man-made delivery and drain canals, and the main stem of the Rio Grande riv...
Sensor‐based, semicontinuous observations of water quality parameters have become critical to understanding how changes in land use, management, and rainfall‐runoff processes impact water quality at diurnal to multidecadal scales. While some commercially available water quality sensors function adequately under a range of turbidity conditions, othe...
Fluvial networks integrate, transform, and transport constituents from terrestrial and aquatic ecosystems. To date, most research on water quality dynamics has focused on process understanding at individual streams, and, as a result, there is a lack of studies analyzing how physical and biogeochemical drivers scale across fluvial networks. We perfo...
In streams, gross primary production (GPP) and ecosystem respiration (ER) (i.e., stream metabolism) control the transport and fate of nutrients and organic carbon and vice versa. The importance of short-term and local factors in driving these processes is well known in the literature. However, little information exists regarding the extent of tempo...
The Resazurin (Raz) – Resorufin (Rru) tracer system is widely used in hydrological studies. In most field experiments a lack of mass balance closure is reported and, to date, it is still unclear what drives incomplete recovery. We designed controlled laboratory experiments varying the initial concentrations of Raz, the test durations, and the type...
Resazurin (Raz) is a phenoxazine dye that can be reduced irreversibly to the daughter compound resorufin (Rru) by aerobic respiration. Previous hydrologic studies using the Raz‐Rru reactive tracer system to quantify water‐sediment interactions and metabolic activity have reported that dilution‐corrected masses of Raz and Rru recovered are smaller t...
High concentrations of fecal indicator bacteria (FIB) can result in exceedance of surface water quality standards, particularly in urban areas which receive stormwater runoff. Although FIB are considered to be an indicator of mammalian waste, there is increasing evidence of regrowth in sediments of warm streams. However, the role that sediment-wate...
We introduce "The Integrator," a novel technique to quantify transport and reaction metrics commonly used to characterize flow systems. This development consists of two products: (1) The Integrator sampling device and (2) its supporting mathematical framework, which is compatible with semi-continuous sensor data. The use of The Integrator device si...
The resazurin-resorufin tracer system has been used to quantify surface water-sediment interactions and microbial metabolic activity in stream ecosystems for one decade. This review describes the evolution of the tracer technique and summarizes how it has been used by the hydrologic and stream ecology communities. We highlight major hydrologic appl...
Stream restoration goals include reducing erosion and increasing hyporheic exchange to promote biogeochemical processing and improve water quality. Little is known, however, about fine particle dynamics in response to stream restoration. Fine particles (<100 μm) are exchanged with transient storage areas near and within streambeds and banks. Fine p...
The exchange of groundwater and surface water (GW-SW), including dissolved constituents and energy, represents a critical yet challenging characterization problem for hydrogeologists and stream ecologists. Here, we describe the use of a suite of high spatial-resolution remote-sensing techniques, collected using a small unmanned aircraft system (sUA...
The reactive transport of uranium (U) and vanadium (V) from abandoned mine wastes collected from the Blue Gap/Tachee Claim 28 mine site, AZ was investigated by integrating flow-through column experiments with reactive transport modelling, and electron microscopy. The mine wastes were sequentially reacted in flow-through columns at pH 7.9 (10 mM HCO...
Fine particles (1-100 µm), including particulate organic carbon (POC) and fine sediment, influence stream ecological functioning because they may contain or have a high affinity to sorb nitrogen and phosphorus. These particles are immobilized within stream storage areas, especially hyporheic sediments and benthic biofilms. However, fine particles a...
Shallow benthic biolayers at the top of the streambed are believed to be places of enhanced biogeochemical turnover within the hyporheic zone. They can be investigated by reactive stream tracer tests with tracer recordings in the streambed and in the stream channel. Common in-stream measurements of such reactive tracers cannot localize where the pr...
Reactive tracer tests with the compound resazurin are often conducted in streams to determine hyporheic exchange parameters and investigate stream metabolism. Metabolic reactivity is closely linked to the hyporheic zone, and it was the aim of this study to assess the contributions of benthic biolayers, layers of increased reactivity at the top of i...
Closing nutrient loops in terrestrial and aquatic ecosystems is integral to achieve resource security in the food-energy-water (FEW) nexus. We performed multiyear (2005-08), monthly sampling of instream dissolved inorganic nutrient concentrations (NH4-N, NO3-N, soluble reactive phosphorus-SRP) along a ~300-km arid-land river (Rio Grande, NM, USA) a...
Chemical reactions occur throughout natural waters however the reaction rates often are enhanced just below the sediment-water interface compared with surface water or deeper groundwater. Hydrologic exchange across the sediment surface brings reactive solutes and fine particulates from surface waters into contact with the abundant reaction sites as...
Hall et al. (2013) presented a synthesis on 969 nutrient tracer experiments
conducted primarily in headwater streams (generally < fourth-order
streams), with discharges < 200 L s−1 for ~90 % of
the experiments, and used a scaling method to test the hypothesis that
nutrient demand is constant with increasing stream size (i.e., along a river
continuu...
Hall et al. (2013) presented a synthesis on 969 nutrient tracer experiments conducted primarily in headwater streams (generally < 4th order streams), with discharges < 200 L/s for ~90% of the experiments, and used a power-law scaling method to test the hypothesis that nutrient demand is constant with increasing stream size (i.e., along a river cont...
We investigated changes in respiration across night and daytime in a headwater stream. For this, we conducted consecutive nighttime and daytime experiments injecting the bioreactive tracer resazurin in two reaches with different riparian canopy densities (different levels of photosynthetically active radiation) to compare respiration rate coefficie...
Groundwater–surface-water (GW-SW) interactions in streams are difficult to quantify because of heterogeneity in hydraulic and reactive processes across a range of spatial and temporal scales. The challenge of quantifying these interactions has led to the development of several techniques, from centimeter-scale probes to whole-system tracers, includ...
Resazurin (Raz) and its reaction product resorufin (Rru) have increasingly
been used as reactive tracers to quantify metabolic activity and hyporheic
exchange in streams. Previous work has indicated that these compounds undergo
sorption in stream sediments. We present laboratory experiments on Raz and
Rru transport, sorption, and transformation, co...
Stream functioning includes simultaneous interaction among solute transport, nutrient processing, and metabolism. Metabolism is measured with methods that have limited spatial representativeness and are highly uncertain. These problems restrict development of methods for up-scaling biological processes that mediate nutrient processing. We used the...
Resazurin (Raz) and its reaction product resorufin (Rru) have increasingly been used as reactive tracers to quantify metabolic activity and hyporheic exchange in streams. Previous works have indicated that these compounds undergo sorption in stream sediments. We present a series of laboratory column and batch experiments on Raz and Rru transport, s...
[1] We provide an efficient method to estimate processing rates through simple algebraic relationships derived from the transient storage model equations. The method is based on the transport equations, but eliminates the need to calibrate highly uncertain (and intermediate) parameters. We demonstrate that under some common stream transport conditi...
We provide an efficient method to estimate processing rates through simple algebraic relationships derived from the transient storage model equations. The method is based on the transport equations, but eliminates the need to calibrate highly uncertain (and intermediate) parameters. We demonstrate that under some common stream transport conditions...
We investigated scaling of conservative solute transport using temporal
moment analysis of 98 tracer experiments (384 breakthrough curves)
conducted in 44 streams located on five continents. The experiments span
7 orders of magnitude in discharge (10^-3 to 10^3
m3/s), span 5 orders of magnitude in longitudinal scale
(10^1 to 10^5 m), and sample dif...
Small dams enhance the development of patchy microenvironments along stream
corridors by trapping sediment and creating complex streambed morphologies. This
patchiness drives intricate hyporheic flux patterns that govern the exchange of O2 and redox-
sensitive solutes between the water column and the stream bed. We used multiple tracer
technique...
The fate of biologically available nitrogen (N) and carbon (C) in stream
ecosystems is controlled by the coupling of physical transport and
biogeochemical reaction kinetics. However, determining the relative role
of physical and biogeochemical controls at different temporal and
spatial scales is difficult. The hyporheic zone (HZ), where
groundwater...
The use of smart tracers to study hydrologic systems is becoming more
widespread. Smart tracers are compounds that irreversibly react in the
presence of a process or condition under investigation. Resazurin (Raz)
is a smart tracer that undergoes an irreversible reduction to resorufin
(Rru) in the presence of cellular metabolic activity. We quantifi...
Stream metabolism is a key component of nutrient and organic matter
cycling. To date, determining rates of metabolism is accomplished with
techniques that are not spatially representative, mainly because of the
limited sample volume of the methods. The lack of a robust technique to
estimate stream metabolism has restricted the development of method...
The fate of biologically-available nitrogen (N) and carbon (C) in stream
ecosystems is controlled by the coupling of physical transport and
biogeochemical reaction kinetics. However, determining the relative role
of physical and biogeochemical controls at different temporal and
spatial scales is difficult. Hyporheic and riparian zones, where ground...
After three decades of active research in hydrology and stream ecology,
the relationship between stream solute transport, metabolism and
nutrient dynamics is still unresolved. These knowledge gaps obscure the
function of stream ecosystems and how they interact with other landscape
processes. To date, measuring rates of stream metabolism is accompli...
Punctuated head differentials along stream water surface profiles, in
conjunction with heterogeneous sediment and complex bedforms, enhance
hyporheic exchange, although the magnitude of this exchange is not
uniform across the streambed. Patchy biogeochemical micro-environments
develop within these complex systems, and are strongly controlled by
res...
Hydrologic retention in stream ecosystems favors the reactions of solutes and nutrients in metabolically active transient storage (MATS) zones. These zones are hot spots where metabolic activity is expected to contribute significantly to ecosystem respiration. We compare the results of a series of coinjections of resazurin (Raz) as a redox sensitiv...
Transient storage zones increase the contact time of main-channel water with biogeochemically reactive sediments, and thus, increased transient storage is often presumed to increase stream nutrient retention. However, empirical relationships between transient storage and ecosystem processes found in the literature are surprisingly weak or even cont...
The first step in developing travel time and water quality models in streams is to correctly model solute transport mechanisms.
In this paper a comparison between two solute transport models is performed. The parameters of the Transient Storage model
(TS) and the Aggregated Dead Zone model (ADZ) are estimated using data of thirty seven tracer exper...
One of the common problems that water planners have to deal with is the development of flood hazard maps from point precipitation data. This article presents the development of a methodology for the production of this type of maps, using a linked strategy between the HEC-GeoHMS-HEC-HMS hydrological modeling system and the HEC-GeoRAS-HEC-RAS river a...