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Mineralogy of suspended sediment in three karst springs

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Abstract

Springs in karstic carbonate rocks frequently carry a sediment load as well as a dissolved load. Analysis of morphology and mineralogy of suspended sediment from three contrasting karst springs reveals a suite of clastic particles that reflect both source areas and processes that take place within the aquifer. Nolte Spring in Lancaster County, Pennsylvania, USA, discharges sediment of apparently precipitated calcite, indicating that at some point in the aquifer or vadose zone, water exceeds saturation with respect to calcite. Sediment morphologies and chemical conditions in the aquifer point to two different scenarios for this precipitation. The other two springs, Arch Spring in Blair County, Pennsylvania and Bushkill Spring in Northampton County, Pennsylvania, show no evidence of calcite precipitation. Arch Spring discharges mainly layer silicates, while Bushkill Spring discharges mainly silica.

Résumé

Les sources situées en contexte carbonaté karstique charrient fréquemment, outre les matières dissoutes, une charge solide. La morphologie et la minéralogie des sédiments en suspension issus de trois sources karstiques de caractéristiques distinctes ont été analysées : une série de particules clastiques, reflétant à la fois les secteurs des sources et les processus internes de l’aquifère, en ressort. Les sédiments issus de Nolte Spring (Comté de Lancaster, Pennsylvanie, Etats-Unis) sont constitués de calcite apparemment précipitée: ceci indique que l’eau atteint la sursaturation vis-à-vis de la calcite à un certain point de l’aquifère ou de la zone non-saturée. La morphologie des sédiments et les conditions chimiques au sein de l’aquifère mènent à deux scénarii différents pour expliquer cette précipitation. Les deux autres sources, Arch Spring (Comté de Blair, Pennsylvanie) et Bushkill Spring (Comté de Northampton, Pennsylvanie), ne présentent aucun indice de précipitation de calcite. Arch Spring exporte essentiellement des phyllosilicates, alors que la silice est majoritaire à Bushkill Spring.

Resumen

Los manantiales en rocas carbonatadas karstficadas tienen frecuentemente una carga de sedimentos y de sólidos disueltos. Los análisis de la morfología y mineralogía de los sedimentos suspendidos de tres manantiales kársticos contrastados revela un conjunto de partículas clásticas que reflejan ambas áreas fuente y los procesos que tienen lugar dentro del acuífero. Nolte Spring en el Condado de Lancaster, Pennsylvania, USA, descarga sedimento de calcita aparentemente precipitada indicando que en cierto punto del acuífero o en la zona vadosa, el agua supera la saturación con respecto a la calcita. La morfología de los sedimentos y las condiciones químicas en el acuífero apuntan a dos escenarios diferentes para esta precipitación. Los otras dos manantiales, Arch Spring en el Condado de Blair, Pennsylvania y Bushkill Spring en el Condado de Norhtampton, Pennsylvania, no muestran evidencia de precitación de calcita. Arch Spring descarga principalmente filosilicatos mientras que Bushkill Spring descarga fundamentalmente Sílice.

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References

  • Amraoui F, Razack M, Bouchaou L (2003) Turbidity dynamics in karstic systems: example of Ribaa and Bittit springs in the Middle Atlas (Morocco). Hydrol Sci J 48:971–984

    Article  Google Scholar 

  • Bosch RF, White WB (2004) Lithofacies and transport of clastic sediments in karstic aquifers. In: Sasowsky ID, Mylroie JE (eds) Studies in cave sediments. Kluwer/Plenum, New York, pp 1–22

    Google Scholar 

  • Dogwiler T, Wicks CM (2004) Sediment entrainment and transport in fluviokarst systems. J Hydrol 295:163–172

    Article  Google Scholar 

  • Drysdale R, Pierotti L, Piccini L, Baldacci F (2001) Suspended sediments in karst spring waters near Massa (Tuscany), Italy. Environ Geol 40:1037–1050

    Article  Google Scholar 

  • Fitzpatrick EA (1993) Soil microscopy and micromorphology. Wiley, Chichester, England

    Google Scholar 

  • González LA, Carpenter SJ, Lohmann KC (1992) Inorganic calcite morphology: roles of fluid chemistry and fluid flow. J Sediment Petrol 62:382–399

    Google Scholar 

  • Herman EK, Toran L, White, WB (2005) Hurricane precipitation events reveal threshold behavior in water level and sediment concentration at Arch Spring, PA, USA. Geological Society of American National Meeting, Salt Lake City, Utah, 16–19 Oct 2005

  • Lynch FL, Mahler BJ, Hauwert NN (2004) Provenance of suspended sediment discharged from a karst aquifer determined by clay mineralogy. In: Sasowsky ID, Mylroie JE (eds) Studies in cave sediments. Kluwer/Plenum, New York, pp 83–93

    Google Scholar 

  • Mahler BJ, Lynch FL (1999) Muddy waters: temporal variation in sediment discharging from a karst spring. J Hydrol 214:165–178

    Article  Google Scholar 

  • Mahler BJ, Personné JC, Lods GF, Drogue C (2000) Transport of free and particulate-associated bacteria in karst. J Hydrol 238:179–193

    Article  Google Scholar 

  • Mahler BJ, Personné JC, Lynch FL, Van Mere PC (2004) Sediment and sediment-associated contaminant transport through karst. In: Sasowsky ID, Mylroie JE (eds) Studies in cave sediments. Kluwer/Plenum, New York, pp 23–46

    Google Scholar 

  • Massei N, Wang HQ, Dupont JP, Rodet J, Laignel B (2003) Assessment of direct transfer and resuspension of particles during turbid flows at a karstic spring. J Hydrol 275:109–121

    Article  Google Scholar 

  • Peterson EW, Wicks CM (2003) Characterization of the physical and hydraulic properties of the sediment in karst aquifers of the Springfield Plateau, central Missouri, USA. Hydrogeol J 11:357–367

    Google Scholar 

  • Rillstone B, Toran L (2004) Variability of karst spring sediments within and between storm waters. Geological Society of American Northeast-Southeast Regional Meeting, Tysons Corner, VA, 25–27 March 2004

  • Rones M (1969) A lithostratigraphic, petrographic and chemical investigations of the lower Middle Ordovician carbonate rocks in central Pennsylvania. Pennsylvania Geologic Survey General Geology Report 53, Pennsylvania Geologic Survey, Harrisburg, PA, p 224

  • Scholle PA, Ulmer-Scholle DS (2003) A color guide to the petrography of carbonate rocks: grains, textures, porosity, diagenesis. Am Assoc Petrol Geol Mem 77

  • Shuster ET, White WB (1971) Seasonal fluctuations in the chemistry of limestone springs: a possible means for characterizing carbonate aquifers. J Hydrol 14:93–128

    Article  Google Scholar 

  • Tancredi JM (2004) Variation in sediment and geochemistry as evidence of changes in flowpaths to a karst spring in southeastern Pennsylvania. MSc Thesis, Temple University, Philadelphia, PA

    Google Scholar 

  • Toran L, Tancredi J, Herman EK, White WB (2006) Conductivity and sediment variation during storms as evidence of pathways in karst springs. Geol Soc Am Spec Pap 404(14):169–176

    Google Scholar 

  • Vesper DJ, White WB (2003) Metal transport to karst springs during storm flow: an example from Fort Campbell, Kentucky/Tennessee, USA. J Hydrol 276:20–36

    Article  Google Scholar 

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Acknowledgements

This work was supported by the National Science Foundation under Awards No. 125601 and 125551. The authors thank Robert Buckwalter and the West Earl Township Water Authority for access to Nolte Spring, landowners David and Linda Morrow for access to Arch Spring, and Dr. Mary Roth of Lafayette College for obtaining access to Bushkill Spring.

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Authors and Affiliations

  1. Department of Geosciences and Materials Research Institute, The Pennsylvania State University, 801 Deike Building, University Park, PA, 16802, USA

    Ellen K. Herman & William B. White

  2. Department of Geology, Temple University, Philadelphia, PA, 19122, USA

    Jennifer H. Tancredi & Laura Toran

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  1. Ellen K. Herman
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  2. Jennifer H. Tancredi
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  3. Laura Toran
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  4. William B. White
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Correspondence to Ellen K. Herman.

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Herman, E.K., Tancredi, J.H., Toran, L. et al. Mineralogy of suspended sediment in three karst springs. Hydrogeol J 15, 255–266 (2007). https://doi.org/10.1007/s10040-006-0108-2

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