Heat tracing to examine seasonal groundwater flow beneath a low-gradient stream in rural central Illinois, USA
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  • 作者:Hridaya Bastola ; Eric W. Peterson
  • 关键词:Groundwater/surface ; water relations ; Numerical modeling ; Thermal conditions ; VS2DH ; USA
  • 刊名:Hydrogeology Journal
  • 出版年:2016
  • 出版时间:February 2016
  • 年:2016
  • 卷:24
  • 期:1
  • 页码:181-194
  • 全文大小:3,073 KB
  • 参考文献:Bartolino JR, Niswonger RG (1999) Numerical simulation of vertical ground-water flux of the Rio Grande from ground-water temperature profiles, central New Mexico. US Geol Surv Water Resour Invest Rep 99-4212
    Bastola H (2010) Identifying season changes in streambed thermal profile in a third order agricultural stream using 2D thermal modeling. MSc Thesis, Illinois State University, USA
    Beach V, Peterson EW (2013) Variation of hyporheic temperature profiles in a low gradient third-order agricultural stream: a statistical approach. Open J Modern Hydrol 3:55–66. doi:10.​4236/​ojmh.​2013.​32008 CrossRef
    Briggs MA, Lautz LK, McKenzie JM, Gordon RP, Hare DK (2012) Using high-resolution distributed temperature sensing to quantify spatial and temporal variability in vertical hyporheic flux. Water Resour Res 48, W02527. doi:10.​1029/​2011WR011227 CrossRef
    Briggs MA, Lautz LK, Buckley SF, Lane JW (2014) Practical limitations on the use of diurnal temperature signals to quantify groundwater upwelling. J Hydrol 519(Part B):1739–1751. doi:10.​1016/​j.​jhydrol.​2014.​09.​030 CrossRef
    Caissie D, Kurylyk BL, St-Hilaire A, El-Jabi N, MacQuarrie KTB (2014) Streambed temperature dynamics and corresponding heat fluxes in small streams experiencing seasonal ice cover. J Hydrol 519(Part B):1441–1452. doi:10.​1016/​j.​jhydrol.​2014.​09.​034 CrossRef
    Cardenas MB (2007) Potential contribution of topography-driven regional groundwater flow to fractal stream chemistry: residence time distribution analysis of Toth flow. Geophys Res Lett 34: doi:10.​1029/​2006GL029126
    Cardenas MB, Wilson JL, Zlotnik VA (2004) Impact of heterogeneity, bed forms, and stream curvature on subchannel hyporheic exchange. Water Resour Res 40: doi: 10.​1029/​2004WR003008
    Conlon T, Lee K, Risley J (2003) Heat tracing in streams in the central Willamette Basin, Oregon. In: Stonestrom DA, Constantz J (eds) Heat as a tool for studying the movement of ground water in streams. US Geol Surv Circ 1260, pp 29–34
    Constantz J (1998) Interaction between stream temperature, streamflow, and groundwater exchanges in alpine streams. Water Resour Res 34:1609–1615CrossRef
    Constantz J (2008) Heat as a tracer to determine streambed water exchanges. Water Resour Res 44(4), W00D10. doi: 10.​1029/​2008WR006996
    Constantz J, Stonestrom DA (2003) Heat as a tracer of water movement near streams, chap 1. In: Stonestrom DA, Constantz J (eds) Heat as a tool for studying the movement of ground water near streams. US Geol Surv Circ 1260, pp 1–6
    Constantz J, Thomas CL (1996) The use of streambed temperature profiles to estimate the depth, duration, and rate of percolation beneath arroyos. Water Resour Res 32:3597–3602CrossRef
    Constantz J, Stonestrom D, Stewart AE, Niswonger R, Smith TR (2001) Analysis of streambed temperatures in ephemeral channels to determine streamflow frequency and duration. Water Resour Res 37:317–328CrossRef
    Constantz J, Stewart AE, Niswonger R, Sarma L (2002) Analysis of temperature profiles for investigating stream losses beneath ephemeral channels. Water Resour Res 38(12):1316. doi: 10.​1029/​2001WR001221
    Constantz J, Cox MH, Su GW (2003) Comparison of heat and bromide as ground water tracers near streams. Ground Water 41:647–656CrossRef
    Essaid HI, Zamora CM, McCarthy KA, Vogel JR, Wilson JT (2008) Using heat to characterize streambed water flux variability in four stream reaches. J Environ Qual 37:1010–1023. doi:10.​2134/​jeq2006.​0448 CrossRef
    Fanelli RM, Lautz LK (2008) Patterns of water, heat, and solute flux through streambeds around small dams. Ground Water 46:671–687. doi:10.​1111/​j.​1745-6584.​2008.​00461.​x CrossRef
    Genereux DP, Leahy S, Mitasova H, Kennedy CD, Corbett DR (2008) Spatial and temporal variability of streambed hydraulic conductivity in West Bear Creek, North Carolina, USA. J Hydrol 358:332–353. doi:10.​1016/​j.​jhydrol.​2008.​06.​017 CrossRef
    Gordon RP, Lautz LK, Briggs MA, McKenzie JM (2012) Automated calculation of vertical pore-water flux from field temperature time series using the VFLUX method and computer program. J Hydrol 420–421:142–158. doi:10.​1016/​j.​jhydrol.​2011.​11.​053 CrossRef
    Hatch CE, Fisher AT, Revenaugh JS, Constantz J, Ruehl C (2006) Quantifying surface water–groundwater interactions using time series analysis of streambed thermal records: method development. Water Resour Res 42, W10410. doi 10.​1029/​2005WR004787
    Hatch CE, Fisher AT, Ruehl CR, Stemler G (2010) Spatial and temporal variations in streambed hydraulic conductivity quantified with time-series thermal methods. J Hydrol 389:276–288. doi:10.​1016/​j.​jhydrol.​2010.​05.​046 CrossRef
    Healy RW, Ronan AD (1996) Documentation of computer program VS2DH for simulation of energy transport in variably saturated porous media: modification of the U.S. Geological Survey’s computer program VS2DT. United States Geological Survey, Denver, CO, p 36
    Hoffmann JP, Blasch KW, Ferre TP (2003) Combined use of heat and soil-water content to determine stream/ground-water exchanges, Rillito Creek, Tucson, Arizona. In: Stonestrom DA, Constantz J (eds) Heat as a tool for studying the movement of ground water in streams. US Geol Surv Circ 1260, pp 47–56
    Kenoyer GJ, Anderson MP (1989) Groundwater’s dynamic role in regulating acidity and chemistry in a precipitation-dominated lake. J Hydrol 109:287–306. doi:10.​1016/​0022-1694(89)90020-6 CrossRef
    Lapham WW (1989) Use of temperature profiles beneath streams to determine rates of vertical ground-water flow and vertical hydraulic conductivity. US Geological Survey, Reston, VA, 35 pp
    Masterson JP, Sorenson JR, Stone JR, Moran S, Hougham A (2007) Hydrogeology and simulated ground-water flow in the salt pond region of southern Rhode Island. Scientific Investigations Report 2006–527, US Geological Survey, Reston, VA, p 56
    NOAA (2010) Climatological Data, Illinois. 115(1):3
    Oware E (2010) The impact of storm on thermal transport in the hyporheic zone of a low-gradient third-order sand and gravel bedded stream. MSc Thesis, Illinois State University, USA
    Peterson EW, Benning C (2013) Factors influencing nitrate within a low-gradient agricultural stream. Environ Earth Sci 68:1233–1245. doi:10.​1007/​s12665-012-1821-x CrossRef
    Peterson EW, Sickbert TB (2003) Assessment of stream water bypass through a meander neck in a flood plain. Geol Soc Am Abstr Programs 35:376
    Peterson EW, Sickbert TB (2006) Stream water bypass through a meander neck, laterally extending the hyporheic zone. Hydrogeol J 14:1443–1451. doi:10.​1007/​s10040-006-0050-3 CrossRef
    Peterson EW, Sickbert TB, Moore SL (2008) High frequency stream bed mobility of a low-gradient agricultural stream with implications on the hyporheic zone. Hydrol Process 22:4239–4248. doi:10.​1002/​hyp.​7031 CrossRef
    Prudic D, Niswonger R, Wood J, Henkelman K (2003) Trout Creek: estimating flow duration and seepage losses along an intermittent stream tributary to the Humboldt River, Lander and Humboldt counties, Nevada. In: Stonestrom DA, Constantz J (eds) Heat as a tool for studying the movement of ground water near streams. US Geol Surv Circ 1260, pp 58–71
    Schmidt C, Conant B Jr, Bayer-Raich M, Schirmer M (2007) Evaluation and field-scale application of an analytical method to quantify groundwater discharge using mapped streambed temperatures. J Hydrol 347:292–307. doi:10.​1016/​j.​jhydrol.​2007.​08.​022 CrossRef
    Sickbert TB, Peterson EW (2014) The effect of surface water velocity on hyporheic interchange. J Water Resour Prot 6:327–336. doi:10.​4236/​jwarp.​2014.​64035 CrossRef
    Silliman SE, Booth DF (1993) Analysis of time-series measurements of sediment temperature for identification of gaining vs. losing portions of Juday Creek, Indiana. J Hydrol 146:131–148CrossRef
    Silliman SE, Ramirez J, McCabe RL (1995) Quantifying downflow through creek sediments using temperature time series: one-dimensional solution incorporating measured surface temperature. J Hydrol 167:99–119. doi:10.​1016/​0022-1694(94)02613-g CrossRef
    Simpson SC, Meixner T (2012) Modeling effects of floods on streambed hydraulic conductivity and groundwater–surface water interactions. Water Resour Res 48, W02515
    Stallman RW (1963) Computation of ground-water velocity from temperature data. US Geol Surv Water Suppl Pap 1544:36–46
    Stonestrom DA, Constantz J (2003) Heat as a tool for studying the movement of ground water near streams. US Geol Surv Circ 1260, 96 pp
    Su GW, Jasperse J, Seymour D, Constantz J (2004) Estimation of hydraulic conductivity in an alluvial system using temperatures. Ground Water 42:890–901CrossRef
    Suzuki S (1960) Percolation measurements based on heat flow through soil with special reference to paddy fields. J Geophys Res 65:2883–2885CrossRef
    Swanson TE, Cardenas MB (2010) Diel heat transport within the hyporheic zone of a pool–riffle–pool sequence of a losing stream and evaluation of models for fluid flux estimation using heat. Limnol Oceanogr 55:1741–1754. doi:10.​4319/​lo.​2010.​55.​4.​1741 CrossRef
    Swanson TE, Cardenas MB (2011) Ex-Stream: a MATLAB program for calculating fluid flux through sediment–water interfaces based on steady and transient temperature profiles. Comput Geosci 37:1664–1669CrossRef
    Tonina D, Buffington JM (2007) Hyporheic exchange in gravel bed rivers with pool–riffle morphology: laboratory experiments and three-dimensional modeling. Water Resourc Res 43, W01421
    Van der Hoven SJ, Fromm NJ, Peterson EW (2008) Quantifying nitrogen cycling beneath a meander of a low gradient, N-impacted, agricultural stream using tracers and numerical modelling. Hydrol Process 22:1206–1215. doi:10.​1002/​hyp.​6691 CrossRef
    Walton WC (1965) Ground water recharge and runoff in Illinois. In: Survey ISW (ed) Department of registration and education. State of Illinois, Urbana, IL, 55 pp
    Water and Atmospheric Resources Monitoring Program (2010) Illinois Climate Network. Illinois State Water Survey, Champaign, IL
    Weight D (2008) Hydrogeology field manual, 2nd edn. McGraw Hill Publisher Professional, New York
    Winter TC (1986) Effect of ground-water recharge on configuration of the water table beneath sand dunes and on seepage in lakes in the Sandhills of Nebraska, USA. J Hydrol 86:221–237. doi:10.​1016/​0022-1694(86)90166-6 CrossRef
  • 作者单位:Hridaya Bastola (1) (2)
    Eric W. Peterson (2)

    1. ARCADIS, 111 SW Columbia, Suite 670, Portland, OR, 97201, USA
    2. Department of Geography-Geology, Illinois State University, Campus Box 4400, Normal, IL, 61790, USA
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Hydrogeology
    Geology
    Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1435-0157
文摘
The thermal profile of a streambed is affected by a number of factors including: temperatures of stream water and groundwater, hydraulic conductivity, thermal conductivity, heat capacity of the streambed, and the geometry of hyporheic flow paths. Changes in these parameters over time cause changes in thermal profiles. In this study, temperature data were collected at depths of 30, 60, 90 and 150 cm at six streambed wells 5 m apart along the thalweg of Little Kickapoo Creek, in rural central Illinois, USA. This is a third-order low-gradient baseflow-fed stream. A positive temperature gradient with inflection at 90-cm depth was observed during the summer period. A negative temperature gradient with inflection at 30 cm was observed during the winter period, which suggests greater influence of stream-water temperatures in the substrate during the summer. Thermal models of the streambed were built using VS2DHI to simulate the thermal profiles observed in the field. Comparison of the parameters along with analysis of temperature envelopes and Peclet numbers suggested greater upwelling and stability in temperatures during the winter than during the summer. Upwelling was more pronounced in the downstream reach of the pool in the riffle and pool sequence. Keywords Groundwater/surface-water relations Numerical modeling Thermal conditions VS2DH USA

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