Water-Quality Assessment of the Indiana Dunes National Lakeshore, 1973-74

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Water-Quality Assessment of the Indiana Dunes National Lakeshore, 1973-74 NI 3 1,818 00029799 2 (200) _ WRi no. WATER-QUALITY ASSESSMENT OF THE INDIANA DUNES NATIONAL LAKESHORE, 1973-74 k-CA A L . C 0 N , 1975 * SEP 2 5 8 R Prepared for the National Park Service U.S. GEOLOGICAL SURVEY Water-Resources Investigations 14-75 BIBLIOGRAPHIC DATA 1. Report No. 2. 3. Recipient's Accession No. SHEET 4. Title and Subtitle 5. Report Date Water-Quality Assessment of the Indiana Dunes June 1975 National Lakeshore, 1973-74 6. 7. Author(s) 8. Performing Organization Rept. Leslie D. Arihood No*WRI 14-75 9. Performing Organization Name and Address 10. Project/Task/Work Unit No. U.S. Geological Survey 1819 North Meridian Street 11. Contract/Grant No. Indianapolis, Indiana 46202 , 12. Sponsoring Organization Name and Address 13. Type of Report & Period Covered U.S. Geological Survey 1819 North Meridian Street Final Indianapolis, Indiana 46202 14. 15. Supplementary Notes Prepared for the National Park Service 16. Abstracts Precipitation samples collected at the National Lakeshore had average inorganic ion concentrations ranging from 0 to 7.0 milligrams per litre. Streams generally had a specific conductance ranging from 300 to 600 micromhos, an alkaline pH, and a dissolved oxygen concentration near saturation. The bogs and marshland contained water with a specific conductance ranging from 40 to 150 micromhos, an acid pH, and dissolved oxygen ranging from 0.2 to 4.0 milligrams per litre. Ground water was usually a calcium magnesium bicarbonate type and moderately to very hard (71 to 390 milligrams per litre). 17. Key Words and Document Analysis. 17a. Descriptors *Monitoring, *water supply, water chemistry, nutrients, aquatic microbiology, insecticides, chemistry of precipitation, hydrogeology 17b. Identifiers/Open-Ended Terms *Water-quality assessment, National Park Service 17c. COSATI Field/Group 18. Availability Statement 19. Security Class (This 21. No. of Pages Report) No restriction on distribution UNCLASSIFIED 20. Security Class (This 22. Price Page UNCLASSIFIED . FORM NTIS-35 (REV. 10-73) ENDORSED BY ANSI AND UNESCO. THIS FORM MAY BE REPRODUCED USCOMM-DC 8265-P74 WATER-QUALITY ASSESSMENT OF THE INDIANA DUNES NATIONAL LAKESHORE, 1973-74 By Leslie D. Arihood U.S. GEOLOGICAL SURVEY Water-Resources Investigations 14-75 Prepared for the National Park Service 1975 UNITED STATES DEPARTMENT OF THE INTERIOR Stanley K. Hathaway, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director For additional information write to: U.S. Geological Survey 1819 N. Meridian Street Indianapolis, Indiana 46202 CONTENTS Page Abstract 1 Introduction 2 Purpose and scope 2 Acknowledgments 7 Geohydrology 8 General aspects 8 Unit 1 8 Unit 2 9 Unit 4 9 Bedrock 9 Stream hydrology 13 Water quality 14 Precipitation 14 Ground water 15 Lakes and ponds 18 Bogs and marshland 21 Streams 26 Summary 31 References cited 33 Basic data 35 ILLUSTRATIONS Page Figure 1. Map showing location of study area 3 2. Map showing location of the sampling sites 4 3. Geologic map and sections 10 4. Potentiometric-surface map of unit 4 12 5. Map showing water type and hardness of selected ground-water samples 17 6. Map showing location of inter-dunal ponds, ash ponds, and sampling sites near NIPSCO 20 7. Map showing water type of selected bog and marshland samples 22 8. Graph comparing temperature and specific conductance data of the Cowles Bog area 24 9. Map showing water type of selected stream samples 28 10. Graph showing bacteria concentrations at selected stream sites 30 TABLES Page Table A-1. Field analyses 36 A-2. Chemical analyses 45 A-3. Trace element analyses 51 A-4. Organic analyses 52 A-5. Bacteriological analyses 54 WATER-QUALITY ASSESSMENT OF THE INDIANA DUNES NATIONAL LAKESHORE, 1973-74 By Leslie D. Arihood ABSTRACT The Indiana Dunes National Lakeshore is underlain by unconsolidated lake and glacial deposits which have been divided into three units. Unit 1 is comprised mostly of sand and, in the western part of the National Lakeshore, is capable of yielding more than 500 gallons per minute (32 litres per second) to properly constructed wells. Unit 2, a silt till below unit 1, has little potential as a source of water for public supplies within the National Lakeshore area. Unit 4, a clay till under unit 2, is capable of yielding from 10 to 65 gallons per minute (0.6 to 4 litres per second) throughout the National Lakeshore. Precipitation samples collected at the National Lakeshore had average inorganic ion concentrations ranging from 0 to 7.0 milligrams per litre. Streams in the National Lakeshore generally had a specific conductance ranging from 300 to 600 micromhos, a pH ranging from 6.5 to 8.1, and a dissolved oxygen concentration near saturation (7.7 to 12.9 milligrams per litre). The hogs and marshlands generally contained water with a specific conductance ranging from 40 to 150 micromhos, a pH ranging from 5.0 to 6.5, and dissolved oxygen ranging from 0.2 to 4.0 milligrams per litre. Most surface waters tended to have calcium and bicarbonate as the dominant ion pair. Exceptions include some inter-dunal ponds and certain watercourses and areas of Pinhook Bog. Ground-water chemical quality varied with depth and location but not with time during a 6-month interval. Ground water was usually a calcium magnesium bicarbonate type and moderately to very hard (71 to 390 milligrams per litre). INTRODUCTION Purpose and Scope The area between the Indiana cities of Gary and Michigan City (fig. 1) is being rapidly developed into urban and suburban communities supported by nearby industrial complexes. Part of this area is being preserved by the National Park Service, which has begun acquiring land for the Indiana Dunes National Lakeshore. As part of developing the National Lakeshore, the Park Service requested the U.S. Geological Survey to make a water-quality assessment of the area. Sampling for this assessment began July 1973 and ended April 1974. The Park Service also requested a discussion of the area's geohydrology and potential ground-water supplies. The water-quality assessment includes an analysis of the chemical, organic, and bacteriological quality of ground and surface water and the chemical quality of precipitation. Water-quality sampling was done quarterly and included approximately 78 sampling points (fig. 2). -2- MICHIGAN INDIANA >H• 21 Michigan CD City 1\1,7 LaPorte Pinhook Bog 1 41°30 1 >-- . V-- i Z Z = = 0 0 C-.) CD f= U-1 U-1 EXPLANATION Indiana Dunes National Lakeshore 0 5 10 Miles 1 1 1 I I 10 15 Kilometres 0 M i I 1 '00 K [0-et'es Figure Location of study area 3 1 87 ° 10' EXPLANATION Chemical—measurement site • Temperature—measurement site 77 Biological—measurement site Fl owing artesian well '25 Non—flowing artesian wel l • Well used for domestic supply O Well used for public—water supply 4) Unused well * Continuous record, stage—measurement gaging station —Nat i onal Lakeshore boundary 41°40 ' -- ,-- tw.,\ es r- ,- ')\e' ,- J , • __ __ 2 L_ . _ _j .. Cowl es Bog 2777.4k z!:.1___>< 19v 23 ,,,____ -------3P v- v-- 29 (4?--- 24 N I PSCO 2027 22 -37, ii „:„..3r..... Bethlehem Sand d 1 Ic e 6/-:,R' West ------- 6 , ___J L__ Beach V Unit I Baily 30 Homestead 31 Porter Figure 2.-- Indiana Dunes - 4 - 87 ° 00' 59 6 V61 60 *V4-163 64 _J 58 , 55 • \-\e' 66 V'\ \ CZ\ V 48 V-54 • 57 65 Q;kk\-\ V 53 49 56 X 52 / .47 50 51 3 \(\ „ \\C • '733 • I 1 I" 38 kr9 Information 40 Center 34 35 Tremont 6 37 9 Furnessville 43 r— N 0- • _J I 142 44 86J50' 677, = 0 Ic:= Pi nhook Bog 68 737-69 4 41'37' — Chesterton 3 4 5 Miles 0 1 2 3 4 5 0 7 8 Kilometres National Lakeshore sampling sites -5- The following table can be used to convert report data from English to metric units: To obtain English unit Multiplied by metric unit inches 25.4 millimetres (mm) feet .3048 metres gallons per minute (gal/min) .06308 litres per second (l/s) cubic feet per second 3 (ft /s) .02832 cubic metres per 3 second (m /s) Although the conversion factors are shown to as many as five significant figures, the metric equivalents in the text are shown only to the number of significant figures consistent with the values for the English units. Acknowledgments The author is especially grateful to the personnel of the Indiana Dunes National Lakeshore for their assistance in the project field work. The information from J. R. Hill and E. J. Hartke, of the Indiana Geological Survey, on water levels and geology of the area was valuable in preparing the report. Appreciation is expressed to the Northern Indiana Public Service Company and the Indiana Dunes State Park management for permission to enter and sample water in their area. Prof. J. E. Newman's data on precipitation quality, and Mr. E. C. Moore's cooperation in field data collection were also helpful. GEOHYDROLOGY General Aspects The study area is underlain by three unconsolidated rock groups originating from glacial action and lake sedimentation. Bedrock underlying these deposits consist of shale and limestone. All these formations are sources of water; however, the quantity of water available and the quality vary among them. The unconsolidated rocks were divided into units 1, 2, and 4 by Rosenshein (1962a), consisting respectively of sand, silt till, and clay till. Unit 3 of Rosenshein's description does not extend under the National Lakeshore area. Figure 3 shows the surficial geology and geologic sections of the area. The following unit descriptions are mostly a summary of the geohydrologic properties reported by Rosenshein and Hunn (1968).
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