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821:		Title:	Management strategies for flood protection in the Lower Illinois River, Phase I: Development of the Lower Illinois River-Pool 26 UNET model
		Volume/Number:	2001
		Issuing Agency:
		Description:	One of the main concerns was the ability to specify proper stage hydrographs at the downstream boundary of the Lower Illinois River for hydraulic design and analysis. We found that a unique stage-discharge rating relationship does not exist at the lower boundary of the Lower Illinois River at Grafton because of backwater effects from the Upper Mississippi River. Management options and results for managed storage and emergency activities need to be analyzed under more comprehensive design of flooding conditions. To improve the capability of UNET for modeling backwater effects for the Lower Illinois River, an extended model including Pool 26 of the Upper Mississippi River was developed. The downstream stations of the model are at the tail of Lock and Dam 25 and the Mel Price Lock and Dam pool, where stage readings are available. The model was calibrated with a 1979 flood and verified with a 1983 flood. Discharge and stage frequency analysis have also been performed for stations at Troy on Cuivre River, Lock and Dam 25 tail, Lock and Dam 26 pool, and Mel Price Lock and Dam on the Mississippi River.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-10
		ISL ID:	000000000840 Original UID: 999999994323 FIRST WORD: Management

822:		Title:	Historical sedimentation at the mouths of five deltas on Peoria Lake.
		Volume/Number:	2001
		Issuing Agency:
		Description:	This report summarizes the results of surveying conducted at the mouths of five deltas on Peoria Lake in 1999. The five deltas are at the mouths of Richland Creek, Partridge Creek, Blue Creek, Dickison Run, and Farm Creek. All surveying was done to include the planform of the deltas that existed in 1999. The 1999 planform of four of the five deltas except Dickison Run is different than the locations in 1902-1904. In order to estimate the volumes of deposited sediment between 1902-1904 and 1999, a grid was developed encompassing the aerial extent of the 1999 delta. Subsequently, computations determined the net volumetric accumulation of sediment within each grid for each delta: 2,683 acre-feet (Partridge Creek), 1,495 acre-feet (Blue Creek), 1,428 acre-feet (Richland Creek), 1,252 acre-feet (Farm Creek), and 338 acre-feet (Dickison Run). Relative values of the sediment accumulation could be quite misleading since most of these creeks have been altered over the last 100 years, the 1999 outlets are not at the same locations as those that existed in 1902-1904, and a significant amount of sand-and-gravel mining took place at several locations such as at Farm Creek. Still these values provide a significant contribution toward the understanding of the relative magnitudes of sediments being deposited at the mouths of these five deltas.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-08
		ISL ID:	000000000841 Original UID: 999999994324 FIRST WORD: Historical

823:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to file Annual Report.
		Date Created:	09 26 2006
		Agency ID:	06-0327
		ISL ID:	000000000842 Original UID: 831 FIRST WORD: Order

824:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to maintain corporate status.
		Date Created:	09 26 2006
		Agency ID:	06-0480
		ISL ID:	000000000843 Original UID: 837 FIRST WORD: Order

825:		Title:	River geometry, bank erosion, and sand bars within the main stem of the Kankakee River in Illinois and Indiana.
		Volume/Number:	2001
		Issuing Agency:
		Description:	This is the third and final report on the Kankakee River in Illinois supported by the Conservation 2000 Program of the Illinois Department of Natural Resources. For this project, the Illinois State Water Survey mapped the bank erosion of the main stem of the Kankakee River from the Route 30 bridge in Indiana to the mouth of the Kankakee River with the Illinois River near Wilmington, collected about 100 bed and bank material samples, resurveyed all the previously surveyed river cross sections, surveyed four sand bars, and analyzed all historical and new data. This research has shown that of 223.6 river bank miles (includes both sides of the river), about 10.4 river bank miles have severe erosion, 39.4 river bank miles have moderate erosion, 70.8 river bank miles have minor erosion, and the remainder are either protected or stabilized or data are not available. The median diameter of the bed materials varied from 0.27 millimeters (mm) to 0.52 mm. The median diameter of bank materials varied from 0.07 mm to 0.41 mm. Analyses of the long-term flows from six gaging stations in Illinois showed an increasing trend in flows through the 1960s with no discernible increase since that time. Cross-sectional analyses of the river from the Kankakee Dam to the State Line Bridge did show some trends. The river reach from the Kankakee Dam to Aroma Park called Six-Mile Pool has lost 13.4 percent of its capacity due to sediment deposition since 1980. Similarly, Momence Wetland also has lost about 10.2 percent of its capacity since 1980. The section of the river between Aroma Park and Singleton Ditch showed both scour and sediment deposition. In general areas close to Aroma Park exhibited sediment deposition and the middle reach experienced scour. The recurring sand bar at the State Line Bridge area contains about 8,500 cubic yards of additional sediment in 1999 than were measured in 1980. The volumetric measurement of three additional sand bars showed some changes since 1980. The river is accumulating sediments within Six-Mile Pool and Momence Wetland. The middle reach is in semi-equilibrium with some sediment accumulation at several areas. Several management alternatives, both in-channel and watershed-based also are included to assist in the reduction of sedimentation problems of the Kankakee River.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-09
		ISL ID:	000000000844 Original UID: 999999994327 FIRST WORD: River

826:		Title:	Remote sensing of corn and soybean canopy productivity : data collection and documentation.
		Volume/Number:	2001
		Issuing Agency:
		Description:	As part of a study to estimate corn and soybean yields using satellite remote sensing techniques, biomass measurements, ground-level spectral measurements, and weather and energy flux measurements were taken at three locations in McLean County, Illinois. The locations were near Colfax, Lexington, and Stanford, Illinois. Plant samples and leaf area measurements were taken during the weeks of 12-17 June, 26-30 June, 10-14 July, 31 July-4 August, and 14-18 August 2000 in McLean County, Illinois. Corn plants were separated into leaf, stem, husk, and ear components, and soybean plants into leaf, stem, and pod components. The wet weights of the different plant parts were determined. To determine the plant dry biomass, the plant parts were dried in an oven until there was no weight change over two consecutive days. Leaf area for both corn and soybean canopies was measured using a LiCor-2000 instrument. Corn leaf area was also determined by manual measurements of leaf length and width. The smallest corn and soybean plants were at the Lexington location. The largest corn plants were at Colfax, and the largest soybean plants were at Stanford. The smaller plants at Lexington were a result of sandier soils containing less organic matter than the soils at either Stanford or Colfax. Although final yield was not measured as part of this sampling protocol, the size of the plants would indicate that Lexington should have the smallest corn and soybean yields, while the highest corn yields should have occurred at Colfax, and the highest soybean yields at Stanford.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-13
		ISL ID:	000000000845 Original UID: 999999994328 FIRST WORD: Remote

827:		Title:	Sediment and nutrient monitoring at selected watersheds within the Illinois River Watershed for evaluating the effectiveness of the Illinois River Conservation Reserve Enhancement Program (CREP).
		Volume/Number:	2001
		Issuing Agency:
		Description:	This report documents the progress that has been made to date on the Conservation Reserve Enhancement Program (CREP) monitoring project. The Illinois Department of Natural Resources (IDNR) through the CREP provides support for this project. This monitoring program collects hydrologic, sediment, and nutrient data for selected watersheds within the Illinois River watershed to assist in the evaluation of the effectiveness of the program. The Illinois River CREP is a new initiative by the State of Illinois and the United States Department of Agriculture to implement conservation practices in the Illinois River watershed over a 15-year period that improve water quality and habitat for wildlife. Monitoring programs were established for sediment and nutrients for two pairs of watersheds within the Illinois River basin to collect hydrologic, sediment, and nutrient data during the implementation phase of the project. The two pairs of watersheds are the Court and Haw Creek watersheds (Spoon River basin) and the Panther-Cox Creek watershed (Sangamon River basin). This report details the location, equipment, and installation techniques used at the five monitoring stations and associated raingages that were installed as part of the data collection effort for this project. Samples of the data collection format and frequency are presented and described. Stage, nutrient concentration, and suspended sediment concentrations for data collected through June 2000 are also presented as appendices.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-12
		ISL ID:	000000000846 Original UID: 999999994329 FIRST WORD: Sediment

828:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Application for Certificate of Service Authority Under Section 16-115 of the Public Utilities Act.
		Date Created:	09 26 2006
		Agency ID:	06-0584
		ISL ID:	000000000847 Original UID: 849 FIRST WORD: Order

829:		Title:	Proposal Writing: The Basic Steps in Planning and Writing A Successful Grant Application
		Volume/Number:
		Issuing Agency:
		Description:	Written by Eric Rinehart and Barbara Bouie-Scott, edited by Melissa Pantier, the purpose of this development guide is to help nonprofit community program developers and planners with the basic elements and concepts in planning and preparing winning proposals for project funding. This guide begins with a pre-proposal section which describes the initial action to be taken in planning the proposal. The next section provides insight on how to identify funders and gives tips on preparing an effective proposal. The third section instructs, step by step, how to organize and write the proposal. Section four discusses submission of a complete, well-structured budget. Section five addresses the typical items included in an Appendix to the proposal.
		Date Created:	09 1998
		Agency ID:
		ISL ID:	000000000848 Original UID: 853 FIRST WORD: Proposal

830:		Title:	Proposal Writing: The Basic Steps in Planning and Writing A Successful Grant Application
		Volume/Number:
		Issuing Agency:
		Description:	Written by Eric Rinehart and Barbara Bouie-Scott, edited by Melissa Pantier, the purpose of this development guide is to help nonprofit community program developers and planners with the basic elements and concepts in planning and preparing winning proposals for project funding. This guide begins with a pre-proposal section which describes the initial action to be taken in planning the proposal. The next section provides insight on how to identify funders and gives tips on preparing an effective proposal. The third section instructs, step by step, how to organize and write the proposal. Section four discusses submission of a complete, well-structured budget. Section five addresses the typical items included in an Appendix to the proposal.
		Date Created:	09 1998
		Agency ID:
		ISL ID:	000000000849 Original UID: 854 FIRST WORD: Proposal

831:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to maintain corporate status.
		Date Created:	09 26 2006
		Agency ID:	06-0481
		ISL ID:	000000000850 Original UID: 838 FIRST WORD: Order

832:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to maintain corporate status.
		Date Created:	09 26 2006
		Agency ID:	06-0482
		ISL ID:	000000000851 Original UID: 839 FIRST WORD: Order

833:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to maintain corporate status.
		Date Created:	09 26 2006
		Agency ID:	06-0486
		ISL ID:	000000000852 Original UID: 840 FIRST WORD: Order

834:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to maintain corporate status.
		Date Created:	09 26 2006
		Agency ID:	06-0487
		ISL ID:	000000000853 Original UID: 841 FIRST WORD: Order

835:		Title:	Order
		Volume/Number:
		Issuing Agency:
		Description:	Citation for failure to maintain corporate status.
		Date Created:	09 26 2006
		Agency ID:	06-0488
		ISL ID:	000000000854 Original UID: 842 FIRST WORD: Order

836:		Title:	Streamflow assessment model for the Little Wabash River Watershed : hydrologic analysis
		Volume/Number:	2001
		Issuing Agency:
		Description:	The Illinois Streamflow Assessment Model (ILSAM) is an analytical and information tool developed to predict the frequency of streamflows, and water use impacts on streamflows, for every stream in selected major watersheds in Illinois. The current version of ILSAM was developed to operate on a personal computer having a Microsoft Windows 95/98/2000/NT operating system. The model user can obtain streamflow frequency estimates for any location in the watershed by identifying the desired stream and location. The ILSAM has been developed for use with streams in five such watersheds: the Sangamon, Fox, Kaskaskia, Kankakee, and Little Wabash River. This report includes a description of the steps used to develop ILSAM for application to the Little Wabash River watershed, along with a description of the physical characteristics of the watershed, its surface water hydrology, and the factors that influence streamflow variability. The Little Wabash River watershed is located in the southeastern portion of Illinois and has a total area of approximately 3238 square miles. The river and its major tributaries provide the source of water supply for all of the major communities in the watershed, either through direct withdrawals from the river or from the storage of water in impounding reservoirs. Many of these communities were forced to undertake emergency measures to sustain their water supply from these sources during the major droughts of the early- and mid-1900s. Thus, an understanding of the frequency of low flows and drought flows is critical for assessing surface water availability and yields for these communities. Streamflow frequency predictions produced by the model are also useful for evaluating instream flow levels for the protection of aquatic habitat, providing streamflow estimates for water quality analyses and regulations, and classifying Illinois streams by their hydrologic character for use in watershed management. The hydrologic analyses used to develop the model include evaluating the flow frequency from all streamgage records in the Little Wabash River region, evaluating impacts to flow quantity from dams, water supply, and treated wastewaters, and developing regional equations to estimate flows at ungaged sites throughout the watershed. All streamflow frequency estimates produced by the model are representative of the long-term expected flow conditions of streams, reflecting hydrologic conditions over a base period of nearly 50 years (1952-1999).
		Date Created:	9 24 2004
		Agency ID:	CR-2001-14
		ISL ID:	000000000855 Original UID: 999999994330 FIRST WORD: Streamflow

837:		Title:	Operation of rain gauge and groundwater monitoring networks for the Imperial Valley Water Authority. Year Eight : September 1999-August 2000.
		Volume/Number:	2001
		Issuing Agency:
		Description:	The Illinois State Water Survey (ISWS), under contract to the Imperial Valley Water Authority (IVWA), has operated a network of rain gauges in Mason and Tazewell Counties since August 1992. The ISWS also established a network of groundwater observation wells in the Mason-Tazewell area in 1994. These networks are located in the most heavily irrigated region of the state. The region's major source of water for irrigation, municipal, and domestic water supplies is groundwater pumped from thick sand-and-gravel deposits associated with the confluence of two major ancient river valleys, the Mississippi and the Mahomet-Teays. Relatively recent extreme weather events (e.g., the drought of 1988 and the great flood of 1993) resulted in large fluctuations in groundwater levels in the Imperial Valley area. The purpose of the rain gauge network and the groundwater observation well network is to collect long-term data to determine the rate of groundwater drawdown in dry periods and during the growing season, and the rate at which the aquifer recharges. This report presents data accumulated from the rain gauge and observation well networks since their inception through August 2000. Precipitation is recorded continuously at 20 rain gauges for each storm that traverses the Imperial Valley. Groundwater levels at the 13 observation wells are measured the first of each month. The database from these networks consists of eight years of precipitation data and six years of groundwater observations. At the beginning of groundwater observations in late 1994, the water levels were at their highest in the six years of observation. These high groundwater levels were the result of the very wet 1992-1995 period when annual precipitation was above the 30-year normals at both Havana and Mason City. From September 1995-August 1997, precipitation in the region was well below the 30-year normal followed by the 1997-1998 and 1998-1999 observation years with rainfall totals that were slightly above and slightly below normal, respectively. Groundwater levels in the observation wells reflected the multi-year rainfall patterns, showing a general downward trend during the dry years, a recovery in the wet 1997-1998 year, and a leveling off in 1998-1999. Precipitation in the region during observation year 1999-2000 was well below normal, mirroring the quite low totals observed during the dry years of 1995-1997. In response, groundwater levels fell to levels similar to those experienced in 1996-1997. Analysis indicates that groundwater levels are affected by both the precipitation in the Imperial Valley area and, for wells close to the Illinois River, by river stage. Generally, water levels in wells follow antecedent precipitation and Illinois River stage by one to two months, i.e., June groundwater levels are most highly correlated with the Illinois River stage or precipitation that occurs in April or May. The analyses conducted indicate the need for continued operation of both networks due to inconsistencies associated with groundwater levels, precipitation, and the Illinois River stage. For instance, although observation well number 2 (MTOW-2) is located near the center of Mason County, well away from the Illinois River, it has an equal correlation with the Illinois River stage and area precipitation. Additional data collection and analyses are needed to determine the reasons for this and other data disparities.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-15
		ISL ID:	000000000856 Original UID: 999999994332 FIRST WORD: Operation

838:		Title:	Management strategies for flood protection in the Lower Illinois River, Phase II: real-time simulation of flooding with UNET model.
		Volume/Number:	2001
		Issuing Agency:
		Description:	This report documents the structure and the use of a windows-based interface developed by the Illinois State Water Survey for the Office of Water Resources, Illinois Department of Natural Resources. The current version of the interface program is able to download historic, real-time, and forecasted stage and flow data from the U.S. Geological Survey, U.S. Army Corps of Engineers, and the National Weather Service websites interactively. These data are used to update existing Data Storage System (DSS) database or to create new ones; to run the UNET model for historic, design, real-time, and forecasted flood events in the Lower Illinois River; and to post-process model outputs from DSS files in tabular and graphical formats.. This interface program uses the original UNET generic geometry and boundary condition files to maintain the same level of accuracy as the UNET model, but it also allows the user to change some of the parameters, such as, the simulation time interval, time windows, and numerical Corant number, and etc., in the BC file. The real-time simulation of a flood event simulates the flood stage profiles using forecasted stage and real-time flow data downloaded from related websites. With the primary focus on simulations of levee failures, the interface program lets the users modify parameters to simulate simple levee failures through the simple spillway approach for two types of complicated embankment failures, overtopping and piping. A new simulation can be performed using the modified levee information. The change of water surface elevation induced by modifying the levees can be compared with another simulation graphically and also in table format. Stage profiles from all the simulations can be plotted together with the levee heights on both sides of the channel along the Lower Illinois River to provide a visual view of the locations of overtopping. Overtopping locations and magnitudes will be tabulated should they occur.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-16
		ISL ID:	000000000857 Original UID: 999999994333 FIRST WORD: Management

839:		Title:	Benchmark sedimentation survey of the lower Cache River wetlands.
		Volume/Number:	2001
		Issuing Agency:
		Description:	The Cache River located in the southernmost part of Illinois flows through an area containing the Cache River Wetlands. These unique and important wetlands were designated as a Ramsar Site in 1996. Drainage activities divided the Cache River in half in the early 1900s, effectively separating the river into the Upper and Lower Cache Rivers. The Lower Cache River contains a remnant of a vast wetland system called the Lower Cache River State Natural Area (LCRSNA), commonly referred to as Buttonland Swamp. Sediment inflow from several tributary streams has an impact on the wetland. Previous research has determined that 217,000 tons of sediment were deposited in Buttonland Swamp between 1986 and 1988. The wetlands of the Lower Cache River have been targeted for preservation and restoration by state, federal, and private environmental organizations. A program to monitor the sediment deposition rate within the wetland area at regular intervals would be useful in evaluating and guiding preservation and restoration efforts. This project established a benchmark measure of the deposition rates and cross-sectional profiles at selected locations in the LCRSNA wetland.
		Date Created:	9 24 2004
		Agency ID:	CR-2001-17
		ISL ID:	000000000858 Original UID: 999999994334 FIRST WORD: Benchmark

840:		Title:	Watershed monitoring for the Lake Decatur Watershed, 1999-2000.
		Volume/Number:	2002
		Issuing Agency:
		Description:	Lake Decatur is the water supply reservoir for the City of Decatur. The reservoir was created in 1922 by constructing a dam to impound the flow of the Sangamon River. The dam was modified in 1956 to increase the maximum capacity of the lake to 28,000 acre-feet. The drainage area of the Sangamon River upstream of Decatur is 925 square miles and includes portions of seven counties in east-central Illinois. Lake Decatur has high concentrations of total dissolved solids and nitrates, and nitrate-N concentrations have been exceeding drinking water standards in recent years. This has created a serious situation for the drinking water supply of the City of Decatur, since nitrate-nitrogen (N) cannot be removed from finished drinking water through regular water purification processes. Nitrate-N concentrations in Lake Decatur have exceeded the Illinois Environmental Protection Agency (IEPA) drinking water standard of 10 milligrams per liter (mg/l) on occasions each year for the period between 1970 and 2000, except from 1993 to 1995. Since 1993, the Illinois State Water Survey has been monitoring the Lake Decatur watershed for trends in nitrate-N concentrations and loads and to identify any significant changes in the watershed. The purpose of the monitoring is to collect reliable hydrologic and water quality data throughout the watershed for use by city planners and resource managers to develop watershed management alternatives based on scientific data. This report presents the annual data for all seven years of monitoring (May 1993-April 2000) and monthly data for Year 7 of monitoring (May 1999-April 2000). Based on the seven years of data, it can be concluded that the unit of nitrate-N loads are relatively uniform over the entire watershed but tend to be slightly higher at the tributary streams in the upper Sangamon River watershed than at the Sangamon River stations closer to the lake. Nitrate-N loads vary with concentrations and streamflow and were the lowest in Year 7 because of the low streamflows during that year. Flow-weighted nitrate-N concentrations have been increasing during the study period at the Monticello station. The highest nitrate-N concentrations during the monitoring period were observed in years 6 and 7.
		Date Created:	9 24 2004
		Agency ID:	CR-2002-01
		ISL ID:	000000000859 Original UID: 999999994336 FIRST WORD: Watershed

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