RIVER ROCK BASIN: HISTORICAL BACKGROUND, IEPA TARGETED WATERSHEDS, AND RESOURCE-RICH AREAS
by
Robert A. Sinclair Office of Surface Water Resources: Systems, Information & GIS
Illinois State Water Survey Hydrology Division Champaign, Illinois
A Division of the Illinois Department of Natural Resources
April 1996
CONTENTS Introduction Acknowledgments Historical Perspective of the Basin Basin Physiography and Geology Land Use Basin Soils Streams in the Basin Streamflow and Sediment Quality Streamflow Sediment Quality Surface Water Quality IEPA Stream Assessment Criteria IEPA Surface Water Quality Assessment Ground-Water Resources and Quality Ground-Water Resources Ground-Water Quality IEPA Targeted Watershed Approach Major Watershed Areas Criteria for Selecting Targeted Watersheds TWA Program Activities TWA for the Rock River Basin References Page 1 1 3 3 5 5 5 8 8 8 13 13 14 16 16 17 19 19 19 19 20 23
INTRODUCTION Conservation 2000, a program to improve natural ecosystems, visualizes resource-rich areas, and promotes ecosystem projects and development of procedures to integrate economic and recreational development with natural resource stewardship. The Rock River basin is one of the areas identified for such projects. This report briefly characterizes the water resources of the basin and provides other relevant information. The Rock River originates in the Horicon Marsh in Dodge County, Wisconsin, and flows in a generally southerly direction until it enters Illinois just south of Beloit. Then it flows in a southwesterly direction until it joins the Mississippi River at Rock Island. The river flows for about 163 miles in Illinois, and its total length from head to mouth is about 318 miles. The Illinois portion of the Rock River basin covers Boone, Winnebago, and Ogle Counties; major portions of McHenry, Stephenson, DeKalb, Lee, Henry, and Whiteside Counties; and minor portions of Jo Daviess, Kane, Carroll, Bureau, Mercer, and Rock Island Counties. The total area of the Rock River is 10,915 square miles, about 5,650 of which are in Illinois (Figure 1). The Rock River has three major tributaries: the Pecatonica, Kishwaukee, and Green Rivers, with drainage areas of 2,641, 1,257, and 1,131 square miles and river lengths of 92.8 (in Illinois), 64.2, and 91.2 miles, respectively (Healy, 1979). Smaller tributaries include Elkhorn Creek (247 square miles), Rock Creek (237 square miles), Kyte River (194 square miles), and Leaf River (117 square miles). The majority of the basin is in agricultural lands, primarily row crops. Major urban areas are Rockford (population 139,426), Moline-Rock Island (83,754), DeKalb (34,925), Sterling-Rock Falls (24,786), Freeport (25,840), Belvidere (15,958), and Dixon (15,144). Population figures are from the 1991 U.S. Census Population and Housing publication. Acknowledgments Various State Water Survey personnel helped in preparation of this report. Brett Ward prepared the color maps. John Blomberg supplied the water use information. H. Allen Wehrmann prepared the ground-water information section, and Misganaw Demissie prepared the benchmark sediment monitoring section. Krishan P. Singh reviewed the draft report and made many helpful comments. Sarah Hibbeler edited the manuscript, and Norma Lee Rhines typed the final report.
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Figure 1. Rock River resource-rich area
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HISTORICAL PERSPECTIVE OF THE BASIN Development in the basin began in the early 1900s when two large swamps in the Green River basin were drained and the river was dredged and straightened. By the 1930s, seven low-head dams, 9 to 15 feet high, were constructed in the Rock River and they served as sources of hydroelectric power. In 1938, only one dam was still being used for that purpose; the pools formed by the other dams are now being used mostly for recreation. The Rock River basin, as defined by the Illinois State Planning Commission or ISPC (1938), occupies the northwest portion of Illinois. It includes watersheds of the Rock, Green, Kishwaukee, and Pecatonica Rivers, and areas drained by the Galena, Apple, and Plum Rivers and other small tributaries entering directly into the Mississippi River, from the Wisconsin/Illinois border to the confluence of the Rock River with the Mississippi. The basin covers 6,481 square miles, or 4,147,840 acres, in Illinois as given in Table 1. This chapter is largely based on the ISPC (1938) report. Basin Physiography and Geology The northwest portion of the basin, including all of Jo Daviess County, is very hilly. With the exception of Jo Daviess County and the northwest corner of Carroll County, the entire basin is covered with deposits of glacial drift (Illinoisian drift) overlying Mississippi loess from a depth of about 5 feet in the hilly country to more than 50 feet in the valleys. Below these deposits in the valleys lie blue clay and sand and gravel beds to a depth of about 70 feet, identified as Pleistocene drift. Immediately underlying these deposits and paralleling the Mississippi River is a rock outcrop of Quaternary age, about 3 to 6 miles wide. The formation follows the Rock River upstream for about 20 miles from its confluence with the Mississippi and extends 3 to 6 miles on either side of the river. Immediately east of this rock formation, Silurian rock underlies all of Whiteside County, forming a narrow strip about 3 miles wide, which parallels the Quaternary along the west side of Carroll County and curves east to underlie the southeast corner of Jo Daviess County and the southwest corner of Stephenson County, paralleling the northern boundary of Carroll County. In the remainder of the basin, Ordovician rock of Galena and Plattville type underlies the drift. The eastern portion of the basin is a high tableland, covering Boone, McHenry, Kane, and DeKalb Counties. A rolling ridge of high land along the southern boundary separates the valley of the Green River from the area further south. Elevations vary from 540 feet in Rock Island County to 1,220 feet above mean sea level in Jo Daviess County. Coal deposits are found in the southeast portion of the basin. Lead and zinc are mined in the northwest. Limestone, sand, and gravel are well distributed throughout the basin. The bottomlands of the Rock River, the Pecatonica River, Richland Creek (a tributary to the Pecatonica), and the Kishwaukee River, and the Mississippi River bottomlands in Jo Daviess, Carroll, and Whiteside Counties, are subject to periodic flooding. These bottomlands cover approximately 130,000 acres.
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Table 1. Distribution of Basin Area by County (Illinois State Planning Commission, 1938)
County
Boone Bureau Carroll DeKalb Henry Jo Daviess Kane Lee McHenry Mercer Ogle Rock Island Stephenson Whiteside Winnebago Total
Total square miles in county 293 881 453 638 824 623 527 742 620 540 756 424 559 679 529 9,088
Total square miles in basin 293 280 453 406 540 623 133 627 329 17 756 257 559 679 529 6,481
Percent of county in basin 100.0 31.8 100.0 63.6 65.5 100.0 25.2 84.5 53.1 3.1 100.0 60.6 100.0 100.0 100.0
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Land Use Severe erosion (with frequent gullies in hillier sections) and moderate sheet erosion (with occasional gullies in the rolling areas) are prevalent in the Rock River basin. Almost one-sixth of Jo Daviess County, scattered areas of northwest Carroll County, and the northwest and northeast corners of Winnebago County were originally covered with timber (Telford, 1926). Bottomlands along the Rock River were intensively cultivated. Land use in the Rock River basin, in terms of areas in forests, agriculture, and urban and other uses, is given in Table 2 for each county (U.S. Bureau of Census, 1936). Basin Soils In the upper reaches of the basin, mainly in Boone County and eastern Winnebago County, the soil is a brownish-yellow clay with a noncalcareous subsoil. Along the north bank of the Rock River in Ogle County, the soil is similar to that described above. However, in southern Ogle County and in the north-central portion of Lee County, the soil is dark with a noncalcareous subsoil. Below this, on the north side of the Rock River in Whiteside County, is a dark soil with a noncalcareous subsoil. On the south side of the river, covering the southwest portion of Lee County and the southern half of Whiteside County, the soil is a sandy loam with areas of peat and muck. The soil in the Pecatonica River valley is a sandy loam. In the northeastern quarter of Stephenson County, it is dark, with a noncalcareous subsoil, and in the northwestern quarter of Winnebago County, it is a brownish-yellow clay, with a noncalcareous subsoil. In the Kishwaukee River basin, the soil is mainly a yellow clay, with a calcareous subsoil in McHenry County; a brownish-yellow clay with a noncalcareous subsoil in northern Boone County; and dark with a heavy calcareous subsoil in southern Boone County. Sandy loam prevails in the central part of the Green River basin. In southern Henry and Bureau Counties, the soil is dark, with a noncalcareous subsoil. Streams in the Basin The Rock River rises in southeastern Wisconsin, enters Illinois near Beloit, and empties into the Mississippi River immediately below the city of Rock Island. The total fall in the river bed level from the Illinois/Wisconsin border to the confluence with the Mississippi River is about 187 feet. It has seven in-channel dams along its length in Illinois. The principal tributaries are the Green, Kishwaukee, and Pecatonica Rivers.
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Table 2. Land Use in the Rock River Basin Acres of land within basin available for Urban, other County
Boone Bureau Carroll DeKalb Henry Jo Daviess Kane Lee McHenry Mercer Ogle Rock Island Stephenson Whiteside Winnebago Total Forests 5,311 10,804 24,912 3,614 9,327 60,038 2,189 9,287 3,584 840 27,757 21,500 12,020 16,653 17,877 225,713 Agriculture 138,949 137,605 206,507 224,888 266,014 206,469 63,942 317,534 145,151 7,766 368,268 95,594 284,608 342,937 228,084 3,034,316 uses 43,260 30,791 58,501 31,338 70,259 132,213 18,989 74,459 61,825 2,274 87,815 47,386 61,132 74,970 92,599 887,811 Total 187,520 179,200 289,920 259,840 345,600 398,720 85,120 401,280 210,560 10,880 483,840 164,480 357,760 434,560 338,560 4,147,840
% of county
area 100.0 31.8 100.0 63.6 65.5 100.0 25.2 84.5 53.1 3.1 100.0 60.6 100.0 100.0 100.0
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The Pecatonica River rises in Wisconsin, flows south into Stephenson County, adopts a bit of a southeasterly direction to Freeport, then gradually changes to a northeasterly direction through Winnebago County and discharges into the Rock River near Rockton in the northeast comer of the county. Its total drainage area is 2,641 square miles (Healy, 1979), about 860 of which are in Illinois. The river length in Illinois is about 92 miles. The river channel is very crooked and frequently doubles back on itself. The floodplain averages 1 mile or more in width. The Kishwaukee River rises in the tablelands of McHenry County. It flows in a westerly direction across central McHenry and Boone Counties, and empties into the Rock River in southeastern Winnebago County. Its major tributary is the South Branch Kishwaukee River, which drains a major part of DeKalb County and about one-fourth of Kane County. The Green River rises in Lee County and flows in a southwesterly direction through Lee, Bureau, and Henry Counties. It joins the Rock River in the west-central portion of Henry County. The river flows through gently rolling country for its entire length, about 91 miles, and drains an area of 1,131 square miles.
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STREAMFLOW AND SEDIMENT QUALITY Streamflow There are ten continuous streamgaging stations in the Rock River basin. Table 3 contains information on the streams such as USGS gaging station numbers, drainage area, mean and peak flows (and their dates of occurrence) observed for water years 1993 and 1994, number of years in the period of record, and associated long-term mean flow. The long-term mean flow values versus drainage areas at the ten gaging stations are plotted in Figure 2. The slope of the line fitted is about 45. Table 3 shows that mean flows for water year 1993 (October 1992 to September 1993) were on average about 2.25 times the long-term mean flows. However, in water year 1994, mean flows were on average only eight percent higher than the long-term mean flows. Mean flows can change significantly from one year to another. Though 1994 seems like a normal or average year, the observed peak flows are: 1) significantly higher than those observed in 1993 for the Kishwaukee River at Belvidere and near Perryville; 2) about the same order of magnitude for the South Branch Kishwaukee River, Rock River at Como, Elkhorn Creek, and Rock River near Joslin; and 3) significantly lower for the Pecatonica River, Rock River at Rockton, Green River, and Mill Creek. Mean flows in 1994 are only about 45 percent of those in 1993 on the average, and the flood peaks occurred during February 20-22, 1994, at all ten stations. (A rainstorm over frozen ground and snow cover yields much higher runoff than a similar storm in spring and summer.) Peak flows occurred on different days and months in 1993. Sediment Quality The Illinois State Planning Commission's Rock River basin report of July 1938 stated that the Rock River was heavily laden with silt in suspension, most of which washed down from the Pecatonica watershed as the result of erosion within that area. An unpublished Illinois Natural History Survey report of the same period stated that drainage ditches carrying silt in suspension also contributed to this type of pollution. Neutron activation analysis has been used to analyze sediment cores from the Rock River and from two branches and the North Fork of Kent Creek, to determine the concentrations of thirteen heavy metalstitanium (Ti), copper (Cu), vanadium (V), manganese (Mn), arsenic (As), antimony (Sb), selenium (Se), chromium (Cr), nickel (Ni), scandium (Sc), iron (Fe), zinc (Zn), and cobalt (Co)and two rare earths, samarium (Sm) and lanthanum (La) (Landsberger et al., 1990). The downstream sites of both the Rock River and the two branches of Kent Creek show elevated concentrations of several heavy metals including arsenic, antimony, and zinc. In addition, hundreds of parts per million of copper have been found in samples from the downstream site of the North Fork of Kent Creek. Toxicity tests of the sediments also indicate that the downstream sites are detrimental to life-forms. Analyses of
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Table 3 Drainage Area and Flow Information for the Rock River Basin Water year 1993 Mean, cfs Peak, cfs
2,452 12,200
USGS number 05435500
Stream/river Pecatonica River at Freeport Rock River at Rockton Kishwaukee River at Belvidee S. Br. Kishwaukee River at DeKalb S. Br. Kishwaukee River at Fairdale Kishwaukee River near Perryville Rock River at Como Elkhorn Creek near Penrose Rock River near Joslin Green River near Geneseo Mill Creek at Milan
DA * 1,326
Water year 1994 Mean, cfs Peak, cfs 1,135 4,900
Years 81
Long-term mean flow 932
05437500 05438500 05439000 05439500 05440000 05443500 05444000 05446500 05447500 05448000
6,363 538 77.7 387 1,099 8,753 146 9,549 1.003 62.4
9,484 992 151 752 1,955 12,990 272 14,560 1,579 173
22,900 7,870 1,310 8,190 11,400 42,700 4,230 46,500 9,600 7,680
4,841 311 55.1 273 729 6,504 140 6,972 640 37.7
16,900 11,900 1,260 8,790 17,100 37,800 4,010 39,700 7,370 3,100
55 55 69 55 55 60 55 55 59 55
4,105 369 64.9 277 756 5,434 102 6,332 641 46.2
* Drainage area in square miles
Figure 2. Long-term mean flow versus drainage area
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the data from the two branches of Kent Creek clearly indicate that heavy metal concentrations increase as the distance from the center of industrial activity (Rockford) decreases. Suspended sediment concentration data have been collected since 1981 at two monitoring sites within the Rock River basin as part of the Illinois State Water Survey's Benchmark Sediment Monitoring Program for Illinois streams (Allgire and Demissie, 1995). The two stations are located on the Pecatonica River at Freeport and on the Rock River at Rockton. The data for the two stations (Figure 3) indicate that suspended sediment concentrations at the Pecatonica River site are higher than those at the Rock River site, implying that erosion and sediment delivery in the Pecatonica River watershed are higher than in the remaining part of the Rock River watershed upstream of Rockton. There is also an indication that suspended sediment concentrations have been decreasing at both stations during the monitoring period. The causes for such a decreasing trend are not known, but it may be associated with trends in precipitation or land use practices. The Pecatonica River site monitors sediment delivery from the 1,326 square mile watershed upstream of the station. The Rock River sites monitor sediment delivery from a larger area, 6,363 square miles, that includes the Pecatonica River watershed.
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Figure 3. Instantaneous suspended sediment concentrations for sampling sites on the Pecatonica and Rock Rivers (Allgire and Demissie, 1995)
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SURFACE WATER QUALITY The Wisconsin Department of Natural Resources -Environmental Protection Division reported that many streams in the lower Rock River basin in Wisconsin received pollutionrelated wastes (State of Wisconsin, 1971). These wastes were primarily organic and consisted of treated sewage and industrial wastes. Toxic substances were being discharged to some lakes from several industries in the basin. The report recommended that the removal of nutrients or the diversion of sewage treatment plant effluents around recreational lakes be given serious consideration. Recently, the Illinois State Water Survey reported a decreasing trend in nitrate-nitrogen levels in the Rock River basin in Illinois (IDENR, 1994). This may be attributed to improved farming practices and reduced use of septic tanks by lakefront communities. The information given below is summarized from the Illinois Environmental Protection Agency, IEPA, Illinois Water Quality Report, 1992-1993, published in 1994. IEPA Stream Assessment Criteria The IEPA describes water quality conditions in terms of the degree to which waters attain designated use standards. For example (IEPA, 1994): Full Support: the water quality meets the needs of all designated uses protected by applicable water quality standards. Full/Threatened: water quality is presently adequate to maintain designated uses, but if a declining trend continues, only partial support may be attained in the future. Partial Support/Minor Impairment: water quality has been impaired, but only to a minor degree. There may be minor exceedences in applicable water quality standards or criteria for assessing the designated use attainment. Partial Support/Moderate Impairment: water quality conditions are impaired to a greater degree, inhibiting the waterbody from meeting all the needs for that designated use. Nonsupport: water quality is severely impaired and not capable of supporting the designated use to any degree.
Water quality conditions are considered for specific or individual uses, including aquatic life, swimming, water, drinking recreation, secondary contact, and fish consumption. In addition, an aggregate assessment of the overall use support is provided. Illinois' waters are classified for a variety of designated uses: 1) General use - provides protection for indigenous aquatic life, primary and secondary contact recreation, and agricultural and industrial uses; 2) Public and food processing water supplies - provides protection for potable water supplies and water use for food processing purposes; 3) Lake Michigan - provides protection for Illinois' portion of Lake Michigan waters through stringent water quality standards; and 4) Secondary contact and indigenous life use - this is the least 13
stringent designated use and applies to certain streams and canals in the Chicago area. Water quality standards for use 2 are somewhat stricter than those for use 1. IEPA Surface Water Quality Assessment A total of 1,443.4 stream miles in the Rock River basin were assessed for overall use support (IEPA, 1994). Evaluated and monitored stream miles (604.3 and 893.1, respectively) combine for a total of 1,443.4 miles. Overall aquatic life use was rated as full support on 881.1 stream miles (61.5 percent); full support but threatened use on 45.6 stream miles (3.2 percent); partial support with minor impairment on 449.0 stream miles (31.1 percent); and partial support with moderate impairment on 60.7 stream miles (4.2 percent). Fish consumption was assessed on 327.6 stream miles in the Rock River basin. All these miles were rated as full use support. Of these, 302.6 miles were assessed for swimming: 165.9 miles as full support, 29.0 miles as partial support and moderate impairment, and 107.7 miles as nonsupport. Swimming use does not apply to stream miles with disinfection exemptions. Surface water is not used as a source of drinking water in the Rock River basin. Causes and sources of less than full support for rivers, creeks, and tributaries in the Rock River basin are summarized below: Rock River. Phosphorus from municipal wastewater discharges and agricultural runoff is the main reason 63 percent of mainstream miles were rated partial support/minor impairment. The rest of the main stream fully supports aquatic life uses. Pecatonica River. As in the Rock River, phosphorus is the main reason 82 percent of mainstream miles were rated as partial support/minor impairment (the remaining 18 percent were rated as full support). Out of 21 tributaries to the Pecatonica River, 13 attained full aquatic life use along their entire length, 6 were rated as having partial support/minor impairment, and Yellow Creek and Richland Creek were rated as having full use support for 39 and 89 percent, respectively, of their total stream miles. Kishwaukee River. About 85.4 percent of stream miles in the Kishwaukee River subbasin fully support aquatic life use. About 50 percent of stream miles with partial support/minor impairment were found in Mokeler Creek, East Branch Killbuck Creek, Lawrence Creek, and South Branch Kishwaukee River. Reduction in use support is caused by municipal wastewater discharges, cropland runoff, and organic enrichment. Green River. Of the total 272.8 miles assessed, 43 percent were rated full support, 37 percent were rated partial support/minor impairment, and the remaining 20 percent were rated partial support/moderate impairment. Impairment is primarily attributed to nutrients and habitat alterations due to channelization and agricultural runoff.
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Kyte River. Eighty-seven percent of the Kyte River and all three of its tributaries (Steward Beach, Prairie, and South Beach Creeks) were rated as fully supporting aquatic life use. Elkhorn and Rock Creeks. Sixty-eight percent of the assessed reaches of these creeks were rated as fully supporting aquatic life use. Miscellaneous Tributaries. Fifteen other tributaries to the Rock River were assessed for aquatic life use support. Eleven provided full support and four had partial support/minor impairment.
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GROUND-WATER RESOURCES AND QUALITY Ground water is a plentiful resource throughout the Rock River basin. Large quantities are withdrawn from sand and gravel aquifers in the glacial drift, and from shallow dolomite and sandstone bedrock aquifers (Visocky et al., 1985). The bedrock aquifers are Silurian, Ordovician, and Cambrian in age. The sand and gravel and shallow dolomite aquifers are generally encountered at depths less than 500 feet; the depth to sandstone aquifers varies considerably, but generally exceeds 500 feet. Pumpage from glacial sand and gravel wells is concentrated along river systems in communities such as Freeport-, Rock Falls, and Rockford. Pumpage from shallow dolomite wells in the basin is largely for domestic supplies. Pumpage from sandstone wells is concentrated in the Belvidere, Rockford, Freeport, Sterling, Dixon, Rochelle, and Quad Cities areas (Sasman and Baker, 1966). Ground-Water Resources The Illinois State Water Survey, Illinois State Geological Survey, and the U.S. Geological Survey have been investigating the geology and ground-water resources of the Rock River valley for decades (USGS, 1986a, 1986b). Several definitive studies of geology and ground-water resources were completed by the State Surveys in the 1950s and early 1960s (Hanson, 1955; Foster, 1956; Hackett and Bergstrom, 1956; and Hackett, 1960). They found that significant sand and gravel deposits are associated with glacial outwash along the Rock Bedrock valley in Winnebago County and the Green River Lowlands in Lee and Whiteside Counties and that well yields in excess of 1,000 gallons per minute are possible in these deposits. Several additional studies of sand and gravel resources along the Rock River and within basin counties were completed in the late 1960s (Anderson, 1967; Hunter and Kempton, 1967) along with more general descriptions of geologic materials in northern and northwestern Illinois (Bradbury, 1965; Frye et al., 1969). The Rock River serves as the discharge zone for regional ground water throughout the basin, including discharge from sand and gravel deposits as well as underlying bedrock formations. Walton (1965) estimated ground-water discharge to the Rock River at Rockton, Oregon, and Como as 0.39, 0.36, and 0.39 cubic feet per second per square mile, respectively, for years of near normal precipitation. Avery (1994) estimated ground-water discharge from beneath the Byron Superfund site in Ogle County to the Rock River to be as high as 30,900 cubic feet per day. In the mid-1930s, about half of the 150 communities in the region received their supply of drinking water from wells and from the Mississippi River (ISPC, 1938). Nearly two-thirds of the ground-water supplies were derived from bedrock sources while the remaining one-third was derived from unconsolidated drift deposits. Ground-water withdrawals in northwestern Illinois (including a few counties outside of the Rock River basin) in 1963 were estimated by Sasman and Baker (1966) to be 78.9 million gallons per day (mgd). Of the total 1963 pumpage, 65 percent was pumped from sandstone wells, 8 percent from shallow dolomite wells, and 27 percent from glacial drift wells. Public water supplies accounted for 69 percent of the 1963 withdrawals, industrial supplies for 20 percent, and domestic use for 11 percent. 16
By 1993, public ground-water withdrawals within the four basin counties of Winnebago, Ogle, Lee, and Whiteside were estimated to be 45 mgd. Annual pumpage rates and the number of wells in each aquifer are summarized in Table 4 for Winnebago, Ogle, Lee, and Whiteside Counties.
Table 4. Total Annual Ground-Water Pumpage Annual pumpage, 1993 (million gallons per day) 11.7 1.1 32.0 44.8
Aquifer Sand and gravel Shallow bedrock Deep bedrock Total
Number of wells 57 112 107 276
Ground-Water Quality Ground water throughout the Rock River basin is of generally good quality for most needs. The water is considered hard in all three aquifer systems, approximately 400 milligrams per liter (mg/L). Iron concentrations are extremely variable in the sand and gravel aquifers and quite often exceed the recommended standard of 1.0 mg/L. Iron concentrations tend to decrease with depth and are generally below 1.0 mg/L in the shallow bedrock and below 0.3 mg/L in the deep bedrock aquifers. Nitrate, like iron, is quite variable throughout the shallow sand and gravel aquifers but is generally around 3 mg/L or less, well below the drinking water standard of 10 mg/L nitrate-nitrogen. Some localized areas of elevated nitrate concentrations are known, particularly in the upper reaches of the basin in Winnebago County. This is largely due to the use of septic systems and fertilizers in areas unable to assimilate the nitrate load (Wehrmann, 1983). Like iron, nitrate concentrations tend to decrease with depth. Chloride and sulfate concentrations also are well within acceptable limits, with median concentrations below 25 and 50 mg/L, respectively, for all aquifer systems. While ground water remains an excellent water source within the basin, recent investigations have revealed a number of contamination problems, particularly within the shallow aquifers in the upper Rock River basin in Ogle and Winnebago Counties. A rating scheme based upon the "threat to human health via groundwater" was devised to identify potential trouble areas (Gibb et al., 1984). Application of the rating scheme within Winnebago and Ogle Counties resulted in the delineation of "hot spots" within the Rockford metropolitan area and secondary risk areas at Pecatonica, Rockton, South Beloit, and Rochelle. Wehrmann (1983) examined nitrate contamination problems in the sand and gravel terrace deposits along the upper Rock River at Roscoe and subsequent contamination of that same aquifer by volatile organic compounds (VOCs), principally trichloroethylene.
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A regional examination of ground-water quality around Rockford found much of the ground water used by residents and industry in the area to be satisfactory with regard to VOCs and selected trace metals (Wehrmann et al., 1988). However, one area in southeast Rockford was found to be significantly contaminated with VOCs. More than 100 domestic wells and at least two municipal wells were estimated to contain VOCs in excess of federal drinking water standards. The area is currently listed as a Superfund site. Other contamination studies have been conducted by the USGS at Belvidere (Boone County) and Byron (Ogle County).
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IEPA TARGETED WATERSHED APPROACH The IEPA is committing available resources within Bureau of Water programs to target watersheds with a maximum potential of realizing environmental benefits (IEPA, 1993). These programs and watersheds have great impact on issues such as human health and ecosystem protection. The Targeted Watershed Approach, TWA, is meant to facilitate water quality management planning. The objectives of the approach are: 1) identification of watersheds with the most critical water quality problems and development of solutions; 2) characterization of watersheds with the greatest potential for improvement using the State's Biological Stream Characterization process; 3) protection of existing high quality water resources considered to be threatened; and 4) integration of point and nonpoint source program activities. Major Watershed Areas The seven major watershed areas (MWAs) covering the state are: MWA #1 - Rock River basin MW...