science for a changing world Water Quality in the White River Basin Indiana, 1992–96
U.S. Department of the Interior U.S. Geological Survey Circular 1150 A COORDINATED EFFORT
Coordination among agencies and organizations is an integral part of the NAWQA Program. We thank the following agencies and organizations who contributed data used in this report.
• The Indiana Department of Natural Resources provided water-withdrawal data. • The National Oceanic and Atmospheric Administration provided precipitation data. • The Indiana Agricultural Statistics Service provided pesticide-use data. • The Natural Resources Conservation Service provided soil-drainage data. • Many farmers and private landowners allowed us to drill and sample wells or tile drains on their properties. • The Indiana Department of Environmental Management provided ammonia and phosphorus data for the White River. • The Indiana State Department of Health, Indiana Department of Environmental Management, and Indiana Department of Natural Resources provided fish-consumption advisories. • The Indiana Department of Natural Resources, Division of Fish and Wildlife, provided historical fish-community data.
Additionally, the findings in this report would not have been possible without the efforts of the following U.S. Geological Survey employees.
Nancy T. Baker Derek W. Dice Harry A. Hitchcock Jeffrey D. Martin Danny E. Renn E. Randall Bayless Nathan K. Eaton Glenn A. Hodgkins Rhett C. Moore Douglas J. Schnoebelen Jennifer S. Board Barton R. Faulkner David V. Jacques Sandra Y. Panshin Wesley W. Stone Donna S. Carter Jeffrey W. Frey C.G. Laird Patrick P. Pease Lee R. Watson Charles G. Crawford John D. Goebel Michael J. Lydy Jeffrey S. Pigati Douglas D. Zettwock
The summary of compound detections and concentrations section of this report (pages 26-31) was designed and prepared by Sarah J. Ryker, Jonathan C. Scott, and Alan L. Haggland.
Front cover: White River near Martinsville, Indiana. (Photograph by Charles Crawford, U.S. Geological Survey.) Back cover: Scientists collecting fish and ground-water samples in the White River Basin. (Photographs by Jeffrey Martin, U.S. Geological Survey.)
FOR ADDITIONAL INFORMATION ON THE NATIONAL WATER-QUALITY ASSESSMENT (NAWQA) PROGRAM:
White River Study Unit, contact:
District Chief Chief, NAWQA Program U.S. Geological Survey U.S. Geological Survey Water Resources Division Water Resources Division 5957 Lakeside Blvd. 12201 Sunrise Valley Drive, M.S. 413 Indianapolis, IN 46278 Reston, VA 20192
Information on the NAWQA Program is also available on the Internet via the World Wide Web. You may connect to the NAWQA Home Page using the Universal Resources Locator (URL) http://wwwrvares.er.usgs.gov/nawqa/nawqa_home.html
The White River Study Unit’s Home Page is at URL http://www-dinind.er.usgs.gov/nawqa/wrnawqa.htm Water Quality in the White River Basin, Indiana, 1992–96
By Joseph M. Fenelon
U.S. GEOLOGICAL SURVEY CIRCULAR 1150
CONTENTS
National Water-Quality Assessment Program ...... 1 Summary of Findings...... 2 Environmental Setting and Hydrologic Conditions ...... 4 Major Findings ...... 6 Water-Quality Conditions in a National Context ...... 20 Study Design and Data Collection ...... 24 Summary of Compound Detections and Concentrations...... 26 References ...... 32 Glossary...... 33 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary
U.S. GEOLOGICAL SURVEY Thomas J. Casadevall, Acting Director
The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Government
1998
Free on application to the U.S. Geological Survey Information Services Box 25286 Federal Center Denver, CO 80225 NATIONAL WATER-QUALITY ASSESSMENT PROGRAM
EXPLANATION Began in 1991 Began in 1994 Began in 1997 Not scheduled yet
Knowledge of the quality of the Nation's streams and aquifers is impor- tant because of the implications to human and aquatic health and because of the significant costs associated with decisions involving land and water management, conservation, and regulation. In 1991, the U.S. Congress appropriated funds for the U.S. Geological Survey (USGS) to begin the National Water-Quality Assessment (NAWQA) Program to help meet the continuing need for sound, scientific information on the areal extent of the water-quality problems, how these problems are changing with time, and an understanding of the effects of human actions and natural factors on water- quality conditions. The NAWQA Program is assessing the water-quality conditions of more than 50 of the Nation's largest river basins and aquifers, known as Study Photo by Jeffrey Martin, U.S. Geological Survey Units. Collectively, these Study Units cover about one-half of the United States and include sources of drinking water used by about 70 percent of the U.S. population. Comprehensive assessments of about one-third of the Study Units are ongoing at a given time. Each Study Unit is scheduled to be revisited every decade to evaluate changes in water-quality conditions. NAWQA assessments rely heavily on existing information collected by the USGS and many other agencies as well as the use of nationally consistent study designs and methods of sampling and analysis. Such consistency simultaneously provides information about the status and trends in water- quality conditions in a particular stream or aquifer and, more importantly, provides the basis to make comparisons among watersheds and improve our understanding of the factors that affect water-quality conditions regionally and nationally. Photo by Charles Crawford, U.S. Geological Survey This report is intended to summarize major findings that emerged between 1992 and 1996 from the water-quality assessment of the White River Basin Study Unit and to relate these findings to water-quality issues of regional and national concern. The information is primarily intended for those who are involved in water-resource management. Indeed, this report addresses many of the concerns raised by regulators, water-utility managers, industry representatives, and other scientists, engineers, public officials, and members of stakeholder groups who provided advice and input to the USGS during this NAWQA Study-Unit investigation. Yet, the information con- tained here may also interest those who simply wish to know more about the quality of water in the rivers and aquifers in the area where they live.
Robert M. Hirsch, Chief Hydrologist
U.S. Geological Survey Circular 1150 1 SUMMARY OF FINDINGS
INDIANA The White River Basin was one of 20 Study Units in the United States to have a water- quality assessment completed between 1992 and 1996.
A variety of pesticides were commonly found in streams throughout the White River Basin. In contrast, only a few pesticides were detected in ground water, and these were at much lower concentrations (p. 6).
In streams: • Pesticide concentrations at urban and agricultural sites were among the highest in the Nation (p. 20). • Twenty-five different pesticides or pesticide degradation products were detected in at least 5 percent of samples near the mouth of the White River. Atrazine and metolachlor were always detected, whereas cyanazine and alachlor were frequently detected (p. 6). In a few samples, concentrations of atrazine, alachlor, or cyanazine exceeded Federal drinking-water standards or advisories (p. 26); however, annual average concentrations of each of these compounds in the White River were below their respec- tive standard or guideline. In shallow ground water: • Fourteen different pesticides were detected in a network of 94 monitoring wells; six were detected more than once (p. 6). No pesticide concentration came close to exceeding a Federal drinking-water standard or advisory. • In cropland areas with a surficial sand and gravel aquifer that is vulnerable to contamination but is also an important source of drinking water for residents of the basin, atrazine compounds were commonly detected (found in two-thirds of monitoring wells) but only at trace levels.
The occurrence of pesticides in streams is controlled by a variety of factors (p. 8–11).
Regional patterns in pesticide use (p. 8): • Concentrations of individual pesticides in streams are greatest where pesticide use is greatest. Temporal patterns in pesticide use (p. 9): • New pesticides introduced to the market can quickly show up in streams. Within 2 years of its registra- tion in 1994, maximum concentrations of the corn herbicide acetochlor in the White River were about 2 µg/L, similar to those of other commonly used herbicides. In contrast, concentrations of alachlor in the White River are declining as alachlor use in the basin declines. Land use (p. 10): • Pesticide concentrations in streams differ according to land use. Lawn insecticides (such as diazinon) are more commonly detected in urban watersheds, whereas corn herbicides (such as atrazine) are more commonly detected in agricultural watersheds. Soil drainage (p. 10–11): • Pesticide concentrations in streams are highest in watersheds with permeable, well-drained soils, all other factors being equal. Agricultural tile drains play a major role in transporting pesticides to streams in areas with poorly drained soils where drainage has been enhanced with tile drains.
Photo by Charles Crawford, U.S. Geological Survey
2 Water Quality in the White River Basin, Indiana, 1992-96 SUMMARY OF FINDINGS
Nitrate concentrations in ground water are low (commonly not detected) in some aquifer settings and high (sometimes exceeding the Federal drinking-water standard) in others. Nitrate concentrations in stream water typically are between these extremes (p. 12–15).
In streams: • Median concentrations of nitrate at monitoring sites generally ranged from 2 to 6 mg/L—higher than those at most other NAWQA monitoring sites in the United States (p. 20). Sample concentrations rarely exceeded the Federal drinking-water standard. In ground water: • Surficial sand and gravel aquifers underlying cropland had high nitrate concentrations. Samples from 17 percent of shallow monitoring wells in this setting exceeded the Federal drinking-water standard of 10 mg/L. However, deeper wells (25 to 50 feet below the water table) in these unconfined aquifers typ- ically had little or no detectable nitrate. • In many parts of the basin, nitrate concentrations in ground water were low. For example, sand and gravel aquifers protected by overlying clay typically had low concentrations of nitrate. Such aquifers are present in more than half the basin and are a common source of water for rural domestic users.
Urban areas degrade the quality of streams and ground water (p. 16–17).
In streams: • Concentrations of trace metals and organic compounds in streambed sediments tended to be above background concentrations in urban areas, particularly Indianapolis. Measured concentrations are generally not a human-health concern; however, fish-consumption advisories for PCBs and mercury are in effect for some areas of the basin. Several chemicals whose use has long been banned (chlor- dane, dieldrin, and PCBs) persist in streambed sediments and are concentrated in organisms such as freshwater clams. • Stormwater runoff and sewer overflows are a continuing problem and have contributed to fish kills in the basin by depleting oxygen in the stream water. One such incident in the White River at Indianapolis in 1994 killed 510,000 fish. In ground water: • Volatile organic compounds were detected in more than half the shallow monitoring wells in urban areas, as compared to 6 percent of shallow wells in cropland areas. Chloroform was the most common volatile organic compound found in urban ground water. No volatile organic compound was measured at a concentration in ground water that exceeded a Federal drinking-water standard or guideline.
Fish communities have significantly improved since the early 1970’s. However, poor communities of fish are still found in streams with poor water quality (p. 18–19).
• Some streams with good fish habitat presently have poor communities of fish, a disparity indicating nonhabitat stresses (such as poor water quality). In areas where the fish communities are poorer than expected on the basis of fish habitat, nutrient and pesticide concentrations are high.
Photo by Charles Crawford, U.S. Geological Survey
U.S. Geological Survey Circular 1150 3 ENVIRONMENTAL SETTING AND HYDROLOGIC CONDITIONS
ENVIRONMENTAL SETTING IN THE EXPLANATION WHITE RIVER BASIN Urban or built-up land Muncie Agricultural land The population of the Forest land Anderson Rivers White River Basin in 1990 Noblesville Cities was approximately 2.1 million New Castle people, about three-fourths of which were concentrated in Indianapolis the northern part of the basin Greenfield (Schnoebelen and others, in press). About 70 percent of the land-use area is agriculture. Greencastle Soybean and corn production is extensive in the northern, Shelbyville southwestern, and southeast- Martinsville ern parts of the basin. In 1992, these two crops accounted for Columbus 78 percent of all cropland. The south-central part of the basin Bloomington is not farmed as extensively as other parts because of the Seymour Bedford steep hills and valleys; most of the forested land in the basin is in this area. Parts of the cities of Indianapolis, Muncie, and Mitchell Anderson are intensively Washington industrialized. Paoli 0 10 20 30 40 MILES 8,000 7071 0102030 40 KILOMETERS TOTAL AREA = 11,350 SQUARE MILES
60 1,200 100
GROUND WATER 90 6,000 1,000 SURFACE WATER 80 50 (1,541) 70 800 POPULATION SERVED, IN THOUSANDS 60 40 600 50 40 4,000 400 30 30
(1,541) PERCENTAGE OF TOTAL WATER WITHDRAWALS, WATER 20 WATER WITHDRAWALS 200 AREA, IN SQUARE MILES (538) 10 PERCENTAGE OF TOTAL AREA IN MILLIONS OF GALLONS PER DAY 20 0 0 2,000 TOTAL MINING SUPPLY 10 THERMO- ELECTRIC DOMESTIC LIVESTOCK COMMERCIAL PUBLIC SUPPLY IRRIGATION AND IRRIGATION INDUSTRIAL AND INDUSTRIAL 0 0 ESTIMATED WATER WITHDRAWALS IN 1990 LAND WATER
Most of the water withdrawn in the White River Basin is from AGL LAND URBAN LAND FOREST LAND BARREN LAND
surface-water sources. Most of this water is used for thermoelectric AGRICULTURAL power. However, approximately 55 percent of the people in the The primary land use in the White River White River Basin rely on ground water as the primary source of Basin is agriculture, which accounts for drinking water (Schnoebelen and others, in press). about 70 percent of the basin area.
4 Water Quality in the White River Basin, Indiana, 1992-96 ENVIRONMENTAL SETTING AND HYDROLOGIC CONDITIONS
HYDROLOGIC CONDITIONS DURING THE STUDY PERIOD
Precipitation during the period of intensive data collection (1993– Understanding the hydro- 95) was near normal. Average annual precipitation ranges from 38 inches logic conditions during the study in the northern part of the White River Basin to 48 inches in the south- period is helpful for interpreting the central part and usually is distributed fairly evenly throughout the year. water quality. For example, during wet periods, nonpoint sources (such 60 PRECIPITATION AT as agricultural runoff) contribute 50 COLUMBUS, INDIANA most of the nutrients to streams in Normal precipitation 40 the White River Basin. Wet periods also cause ground-water levels to IN INCHES 30 rise. Excess ground water sustains PRECIPITATION, 20 tile-drain flow and contributes 10 GROUND-WATER LEVELS directly to streamflow, thus having NEAR COLUMBUS, INDIANA a greater influence on stream qual- 15 ity than during dry periods. In con- No data trast, during dry periods, discharges from point sources (such as an 20 industrial discharge pipe) can sig- DEPTH, IN FEET Collection period for nificantly degrade stream quality
BELOW LAND SURFACE ground-water data 25 because the discharges are not 1985 1986 1987 1988 1989 1990 1991 1992 1993 1994 1995 diluted with large amounts of stream water from other sources. Ground-water levels in an unconfined outwash aquifer near Colum- The seasonal timing of pre- bus were not unusually high or low during the study period. Water levels cipitation also is important to recovered in 1993 from low levels caused by a very dry year in 1992 and understanding stream quality. For then followed a seasonal pattern of high levels in winter and spring and low example, a wet May will allow levels during the summer and fall. more pesticides to be washed into streams than a wet January.
700 600 500 400 300 200 OF NORMAL Streamflow in the PERCENTAGE 100 0 basin is typically highest in 125 early spring and lowest in WHITE RIVER AT MOUTH late summer and fall. This 100 pattern of high runoff in the spring coincides with agricul- 75 tural pesticide applications, 50 often resulting in pesticides being washed into streams 25 during storms. CUBIC FEET PER SECOND STREAMFLOW, IN THOUSAND 0 1992 1993 1994 1995 1996 Intensive collection period for stream-water data
Streamflow at the mouth of the White River was well above normal during the latter half of 1993 and the spring of 1996 but was normal or near normal during the remainder of the study period.
U.S. Geological Survey Circular 1150 5 MAJOR FINDINGS
OCCURRENCE OF PESTICIDES IN STREAMS AND GROUND WATER
Agriculture is the major land use in the White River Basin, and most pesticides detected in streams and ground water during the study period were used primarily in agriculture. Herbi- cides applied to corn and soybeans dominate pes- ticide use. Herbicides are applied during spring planting to virtually all of the corn and soybean crop. Insecticides are applied during the summer to about 25 percent of the corn crop. Approximately 5,000 tons of agricultural pesticides are applied annually in the White River Basin. (Data from Anderson and Gianessi, 1995.)
PESTICIDES MORE COMMON IN STREAMS THAN IN GROUND WATER
Commonly used pesticides were frequently detected in White River. Pesticides were commonly detected in streams in [Samples from 1992–95 except where footnoted; >, greater than or equal to; the White River Basin (Crawford, 1995; Carter and µg/L, micrograms per liter] others, 1995). The highest concentrations occur between May and July when rains wash recently Most com- May–July August–April applied pesticides into streams. Near the mouth of the µ monly used Percent samples > concentration listed below ( g/L) White River, 25 different pesticides or pesticide deg- compounds 0.01 0.1 1.0 10 0.01 0.1 1.0 10 radation products were detected in at least 5 percent of Atrazine 100 100 94 6 100 94 8 0 the samples. Atrazine, metolachlor, cyanazine, and Metolachlor 100 100 49 0 100 63 2 0 alachlor were always or frequently detected. Concen- Alachlor 100 70 6 0 60 8 0 0 trations of atrazine, alachlor, or cyanazine in some individual samples exceeded Federal drinking-water Butylate 40 0 0 0 8 0 0 0 standards or advisories (p. 26); however, annual aver- Cyanazine 91 91 32 0 71 24 0 0 age concentrations of each of these compounds in the Glyphosate no data no data no data no data no data no data no data no data White River were below their respective standard or Pendimethalin 9 0 0 0 0 0 0 0 advisory. Diazinon, chlorpyrifos, and fonofos were 2,4-D1 >57 33 0 0 >6 3 0 0 the most commonly detected insecticides. Maximum concentrations of the insecticides diazinon and chlor- Fonofos 2 0 0 0 0 0 0 0 pyrifos exceeded U.S. Environmental Protection Chlorpyrifos 26 2 0 0 2 0 0 0 Agency (USEPA) water-quality criteria for the protec- Bentazon1 >43 33 0 0 >3 0 0 0 tion of aquatic life (p. 27) (Nowell and Resek, 1994). 2 Acetochlor 84 47 0 0 33 6 0 0 Pesticides are much less common in ground water 11993-95 21994-95 than in streams (Fenelon and Moore, 1996a). Fourteen different pesticides were detected in a network of 94 Six pesticides were detected more than once in ground water. shallow monitoring wells, but only six compounds (all [Samples collected 1994–95; >, greater than or equal to; µg/L, micrograms per liter] herbicides) were detected more than once. All six her- bicides have a high potential for leaching into ground Percent wells > 0.01 µg/L Percent wells > 0.1 µg/L water because of their physical and chemical charac- teristics. Concentrations of all pesticides detected Compounds were very low (less than 0.2 µg/L). USEPA drinking- detected more than once water standards or advisories exist for 13 of the 14 pesticides detected; no pesticide came close to Surficial Surficial Surficial Surficial Confined Confined aquifer in aquifer in urban area urban area cultural area cultural area cultural area cultural area exceeding an existing standard or advisory. For exam- aquifer in agri- aquifer in agri- aquifer in agri- aquifer in agri- Atrazine 17 9 12 0 0 0 ple, the maximum atrazine concentration was less than 1/20th the standard. Confined aquifers protected Metolachlor 4 4 4 4 0 0 by overlying clay soils had very few detections of pes- Prometon 0 0 8 0 0 0 ticides. In a surficial aquifer that is an important Simazine 0 0 4 0 0 0 source of drinking water, atrazine or its degradation Metribuzin 0 8 0 0 4 0 product desethylatrazine were detected in two-thirds Tebuthiuron 0 0 4 0 0 0 of the monitoring wells but only at trace levels (0.001–0.1 µg/L).
6 Water Quality in the White River Basin, Indiana, 1992-96 MAJOR FINDINGS
PESTICIDE CONCENTRATIONS VARY WITH STREAM SIZE
100 In the White River Basin, pesticide White River (11,305-mi2 drainage area at sampling site) concentrations in small streams typically 80 are extremely high or low, whereas con- Sugar Creek centrations in large rivers are moderate. (93-mi2 drainage area at sampling site) 60 For example, during the period when USEPA Maximum Contaminant Level most pesticides are washed into streams (May through July), the maximum con- 40 centration of atrazine measured in Sugar Creek was about twice as high as in the MAY THROUGH JULY 20 PERCENTAGE OF SAMPLES
White River. In contrast, at low concen- EXCEEDING CONCENTRATION, trations, approximately 40 percent of the 0 0 5 10 15 20 25 30 Sugar Creek samples were less than ATRAZINE CONCENTRATION, IN MICROGRAMS PER LITER 1 µg/L as compared to less than 5 per- cent of the samples from the White The USEPA Maximum Contaminant Level (MCL) for atrazine of 3 µg/L was River. exceeded in about 28 percent of the Sugar Creek samples and 45 percent of the White River samples collected during the period May through July, 1992-95.
PESTICIDE CONCENTRATIONS IN STREAMS SHOW SEASONAL PATTERN Pesticide concentrations in streams in Samples of stream water can exceed (which is based on an annual average the White River Basin follow a seasonal USEPA MCL’s during seasonal peaks. concentration for treated water). pattern (Crawford and others, 1995). For example, for about 6 weeks each Although the water near the mouth of Herbicide concentrations are highest in year following spring herbicide appli- the White River is not used as a late spring or early summer, whereas cation, concentrations of atrazine near drinking-water source, some commu- insecticide concentrations typically the mouth of the White River are nities upstream, including Indianapo- peak in midsummer. The highest pesti- greater than the MCL of 3 µg/L. How- lis, Seymour, and Bedford, rely on cide concentrations typically occur dur- ever, the annual average atrazine con- water from the White or East Fork ing the first one or two periods of runoff centration in the White River for 1992 White Rivers for at least part of their following pesticide application. through 1995 never exceeded the MCL drinking-water supply.
14 140
WHITE RIVER NEAR MOUTH Atrazine
12 Streamflow 120
USEPA Maximum Contaminant Level
10 100
8 80
6 60
4 40
2 20 ATRAZINE CONCENTRATION, IN MICROGRAMS PER LITER STREAMFLOW, IN THOUSANDS OF CUBIC FEET PER SECOND 0 0 J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O ND 1992 1993 1994 1995 The seasonal pattern for concentrations of the herbicide atrazine in the White River Basin was typical of the pattern observed for most of the commonly used herbicides.
U.S. Geological Survey Circular 1150 7 MAJOR FINDINGS
FACTORS INFLUENCING minants of pesticide occurrence in PESTICIDE OCCURRENCE IN streams. In addition, the distribution of individual pesticides in streams through- STREAMS out the watershed depends on the physi- cal and chemical properties of the Pesticide occurrence in streams in the pesticides that are in use—properties White River Basin is influenced by land such as sorption (the ability of a pesticide use and agricultural practices such as to stick to soil particles), degradation (the pesticide application, drainage of crop- ease with which a pesticide breaks down Photo by Jeffrey Martin, U.S. Geological Survey land, and cropping methods. Natural fac- in the environment), and volatilization Agriculture is the primary source of tors, such as the type of terrain and soil (the tendency of a pesticide to become pesticides found in streams in the characteristics, also are important deter- gaseous and rise into the atmosphere). White River Basin.
PESTICIDE PROPERTIES AFFECT CONCENTRATIONS IN STREAMS
1.5 Pesticide concentrations in streams in the White River RELATION OF PESTICIDE USE Basin generally increase with increasing use. Yet as TO CONCENTRATION IN shown in the figure to the left, the correlation between use Atrazine WHITE RIVER NEAR MOUTH, and concentration is not strong for every compound. The 1992-94 1.0 properties of individual pesticides affect their behavior in the environment and, consequently, their ultimate concen- trations in streams. Some pesticides stay close to areas where they are used, whereas others are mobile in water Metolachlor and are easily transported into streams. Pesticides that 0.5 degrade quickly may not be found at concentrations that Cyanazine
(1994 concentration only) are anticipated solely on the basis of use; however, degra- IN MICROGRAMS PER LITER
Alachlor dation products of the pesticides may be present in appre- 2,4-D ANNUAL AVERAGE CONCENTRATION, Pendimethalin Chlorpyrifos Fonofos Butylate ciable concentrations. The human health and ecological 0 0200 400 600 800 1,000 1,200 implications of many, though not all, pesticides found in ANNUAL AVERAGE USE, IN TONS streams can be evaluated with guidelines available from scientific and regulatory agencies. The health effects of Pesticide use only partially determines degradation products generally are not known. pesticide concentrations in streams.
STREAM QUALITY REFLECTS REGIONAL HERBICIDE USE
Differences in butylate concen- 1.40 Upper shaded area denotes change in concentration scale trations from streams of similar 1.00 size in two different parts of the 0.60 White River Basin illustrate the Kessinger Ditch effect of regional patterns of pesti- 0.20 Sugar Creek cide use on pesticide concentra- (Unfilled circle indicates butylate tions in streams (Crawford, 1996). was not detected in sample.) Butylate, a corn herbicide, was 0.15 commonly applied in 1993. During 1993, about eight times as many 0.10 acres were treated with butylate and four times more butylate was
applied in southern Indiana than in 0.05 central Indiana. This difference in use was reflected in stream qual- ity—concentrations in Kessinger 0 J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O ND
Ditch (in southern Indiana) were BUTYLATE CONCENTRATION, IN MICROGRAMS PER LITER 1993 1994 1995 substantially higher than in Sugar Creek (in central Indiana). High butylate application rates near Kessinger Ditch result in high concentrations in the ditch.
8 Water Quality in the White River Basin, Indiana, 1992-96 MAJOR FINDINGS
TRENDS IN HERBICIDE USE WITH TIME ARE REFLECTED IN STREAM QUALITY
2.5
2.0 ACETOCHLOR IN WHITE RIVER NEAR MOUTH
1.5
1.0 Open symbol indicates 0.5 acetochlor was not
IN MICROGRAMS PER LITER No data detected in sample ACETOCHLOR CONCENTRATION, 0 2.5 2.6 ALACHLOR IN WHITE RIVER NEAR MOUTH 2.0
1.5
1.0 Open symbol indicates alachlor 0.5 was not detected in sample IN MICROGRAMS PER LITER ALACHLOR CONCENTRATION, 0 J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J A S O ND 1992 1993 1994 1995 1996
3 ALACHLOR USE IN INDIANA
2 ACETOCHLOR USE IN INDIANA
ACTIVE 1 IN THOUSAND TONS INGREDIENT APPLIED, 0 Acetochlor not registered for use Acetochlor not registered for use 1992 1993 1994 1995 1996
Alachlor concentrations in streams in the White River Basin steadily declined from 1992 through 1996, which corresponded with a decline in alachlor use in the basin. Application of acetochlor, a corn herbicide registered for use in 1994, has partially replaced the use of alachlor in the basin. Acetochlor was detected at only trace concentrations during the 1994 growing season. By 1996, acetochlor was commonly detected in the White River with a peak concentration of about 2 micrograms per liter (Crawford, 1997).
Photo by Charles Crawford, U.S. Geological Survey Herbicides applied to corn and soybeans dominate pesticide use in the White River Basin.
U.S. Geological Survey Circular 1150 9 MAJOR FINDINGS
BETTER DRAINED SOILS TRANSMIT MORE PESTICIDES TO STREAMS
JAN FEB MAR APR MAY JUNE JULY AUG Watershed with well-drained SEPT soils (Kessinger Ditch) OCT Watershed with poorly Photo by Jeffrey Martin, U.S. Geological Survey NOV drained soils (Sugar Creek) Clay soils in the Sugar Creek DEC watershed cause ponding of water 0 5 10 15 20 25 and inhibit drainage. AVERAGE MONTHLY CONCENTRATION (1993-95) OF ATRAZINE, IN MICROGRAMS PER LITER Well-drained soils in the Kessinger Ditch watershed carry more pesticides to Differences in atrazine concentra- streams than the clay soils in the Sugar Creek watershed. tions in streams from two similar-sized watersheds with different soil-drainage ping and pesticide-application practices in the Kessinger Ditch watershed, characteristics are illustrated above. throughout the basin, differences in in southern Indiana, are moderately Atrazine was chosen for this illustra- concentrations of atrazine are attributed well drained to well drained without tion because of its widespread use in to natural factors, such as soil drainage. artificial drainage because of coarse- the White River Basin. In 1993, atra- The Sugar Creek watershed, in central textured soils and hilly terrains. Aver- zine was applied to 90 percent of the Indiana, has poorly drained clay soils; age monthly concentrations of atrazine corn crop in central and southern Indi- only 29 percent of the soils in the in Kessinger Ditch, where dissolved ana, and the rate of application was watershed are moderately well drained atrazine is carried through the better similar in these two areas. Because of to well drained without artificial drain- drained soils into the ditch, were typi- this widespread use and similar crop- age. In contrast, 68 percent of the soils cally twice those in Sugar Creek.
LAND USE AFFECTS TYPES OF PESTICIDES FOUND IN STREAMS The types of land use—agricultural 1.30 1.10 Upper shaded area denotes change in concentration scale or urban—in a watershed help deter- 0.90 0.70 mine the types of pesticides expected 0.50 in streams draining the watershed. 0.30 0.10 Trends in the concentration of the Agricultural watershed Urban watershed insecticide diazinon illustrate the effect (Kessinger Ditch) (Little Buck Creek) of land use on pesticide occurrence in 0.08 (Unfilled symbol indicates diazinon not detected.) streams. Diazinon is commonly applied during midsummer in Indiana 0.06 to combat insect infestations in lawns and gardens. It is less commonly used 0.04 for agricultural purposes in the basin. Diazinon was present in almost all samples collected from Little Buck 0.02 Creek, which drains a predominantly urban watershed (57 percent urban). In 0 J F M A M J J A S O N D J F M A M J J A S O N D J F M A M J J AS contrast, diazinon was not found in DIAZINON CONCENTRATION, IN MICROGRAMS PER LITER 1993 1994 1995 Kessinger Ditch, where 94 percent of the watershed is agricultural and less Common urban pesticides, such as diazinon, occur at higher concentrations in than 2 percent is urban. streams in urban watersheds than in streams in agricultural watersheds.
10 Water Quality in the White River Basin, Indiana, 1992-96 MAJOR FINDINGS
SPRING RUNOFF TRANSPORTS MOST HERBICIDES INTO STREAMS
50 Most of the annual herbicide load (the amount of herbi- ATRAZINE IN THE 1996 WHITE RIVER NEAR MOUTH cides carried by a river in one year) enters the White River 40 between May and July. For example, from 1994 through 1996, 69 to 90 percent of the annual load of the five most 30 1995 commonly applied agricultural pesticides entered the river during this period. The amount of runoff from May through July is a key factor in determining the amount of herbicides, 20 1993 such as atrazine, in streams of the White River Basin (see 1994 illustration). During this period, which is shortly after atra- 10 zine application, atrazine concentrations in and on the soil 1992
ANNUAL LOAD, IN TONS PER YEAR are high, and the herbicide is susceptible to moving into
0 streams when runoff occurs. Within 1 to 2 months, most of 5305 10 15 20 25 the applied atrazine is unavailable for transport because it is RUNOFF (MAY THROUGH JULY), IN INCHES degraded or bound up in soil and plant material. Even heavy The annual amount of atrazine carried in the White River runoff at this time contributes only small amounts of atra- reflects the amount of runoff received from May through July. zine to the river.
TILE DRAINS ARE SIGNIFICANT PATHWAYS FOR PESTICIDES Agricultural tile drains pro- vide an important pathway for 1,600 the transport of pesticides to 1,200 STREAMFLOW IN streams in the White River Basin SUGAR CREEK (Fenelon and Moore, in press). 800 Most poorly drained agricultural soils, which are common in the 400
FLOW, IN CUBIC 0
upper midwestern United States, FEET PER SECOND contain tile-drain systems. Tile 14 drains “short circuit” the ground- ATRAZINE COMPOUNDS Atrazine IN SUGAR CREEK water system by intercepting 10 water percolating through the Atrazine degradation soil and shallow ground water products and rapidly transporting it to 5 streams. Because tile drains typi- cally flow during wet periods from late winter to early summer, 0 they are able to transport recently 14 applied pesticides to streams. In 20.5 ATRAZINE COMPOUNDS IN TILE DRAIN the example to the right, atrazine Atrazine DISCHARGING TO SUGAR CREEK 10 concentrations become elevated Atrazine degradation in the tile drain and the creek products
after atrazine is applied in early 5 Tile drain spring. Within about 2 months, not flowing as atrazine is naturally degraded, CONCENTRATION, IN MICROGRAMS PER LITER the concentration of atrazine 0 degradation products is greater FEB MAR APR MAY JUNE JULY AUG than the concentration of atra- 1996 zine. In mid-August, the tile drain stops flowing and concen- In spring, tile-drain water with elevated concentrations of atrazine empties into trations of all atrazine com- Sugar Creek and raises atrazine concentrations in the creek. pounds in the creek are low.
U.S. Geological Survey Circular 1150 11 MAJOR FINDINGS
NITRATE IN STREAMS AND GROUND WATER The primary source of nitrate in the White River Basin is nitrogen fertilizer (Martin and others, 1996). Most of the nitrogen fertilizer in the basin (about 90 percent) is applied to corn. Much of the remaining nitrogen fertilizer is applied to wheat. Nitrate is a public concern primarily because of its adverse effects on human health. The USEPA MCL for nitrate in drinking water is 10 mg/L. In some aquifers in the White River Basin, nitrate concen- trations exceed this level (see p. 14). In streams, median nitrate concentrations generally ranged from 2 to 6 mg/L—much higher than those at most other streams monitored in the United States (see p. 20). Even so, con- centrations of nitrate in streams in the White River Basin rarely exceeded 10 mg/L. The primary concern with nitrogen in streams in the basin is not drinking-water quality but its role in stimulating excessive growth of algae in lakes in Indiana and in the Gulf of Mexico. Run- off from Corn Belt States, which includes Indiana, is a Photos by Jeffrey Martin and Charles Crawford, U.S. Geological Survey possible cause of a “dead” zone in the Gulf of Mex- Sources of nitrate, such as farm-animal manure, commercial ico—one of the largest oxygen-deficient zones in the fertilizers, and effluent from sewage-treatment plants, can stimulate world (U.S. Environmental Protection Agency, 1997). excessive aquatic vegetation in lakes or streams (lower right).
NITRATE CONCENTRATIONS IN STREAMS SHOW A SEASONAL PATTERN Nitrate concentrations in streams in water, it is easily flushed from satu- trations in streams begin to increase. the White River Basin have a seasonal rated soils and transported to rain- Concentrations remain high into late pattern that is controlled by the trans- swollen streams during wet periods. spring and then start to decline as port and availability of nitrate (Martin Nitrate concentrations in streams and streamflow declines and plants begin and others, 1996). Nitrate is primarily streamflow are typically lowest in late to remove nitrate and water from the available for transport during the non- summer and early fall when plants soils. Included in this seasonal pattern growing season, when it may build up (both on land and in the streams) are is a large rise in nitrate concentrations in the soil because plants are not tak- using nitrate and soils are dry. As in June and July, soon after applica- ing up large amounts of nutrients. plants die or go dormant and soils tion of nitrogen-based fertilizer to Because nitrate is very mobile in regain moisture in fall, nitrate concen- corn crops in mid-May to mid-June.
25,000 NONGROWING SEASON GROWING SEASON NONGROWING SEASON 3 MEDIAN NITRATE 20,000 CONCENTRATION, 1991-96
MEDIAN STREAMFLOW 15,000 2 AT TIME OF SAMPLE COLLECTION
10,000
1 5,000 IN CUBIC FEET PER SECOND NEAR MOUTH, IN MILLIGRAMS PER LITER
NITRATE CONCENTRATION IN WHITE RIVER 0 0 STREAMFLOW IN WHITE RIVER NEAR MOUTH,
JAN FEB APR OCT DEC MAR MAY JUNE JULY AUG SEPT NOV Nitrate concentrations in the White River typically are highest during wet periods (high streamflow) and decrease during the growing season.
12 Water Quality in the White River Basin, Indiana, 1992-96 MAJOR FINDINGS
MOST NITROGEN IN WHITE RIVER IS FROM NONPOINT SOURCES
NITROGEN INPUTS TO BASIN Most of the nitrogen input into the White 100 River Basin comes from nonpoint sources, Nitrogen in White River primarily from application of commercial near mouth, 1981-90 Commercial fertilizer fertilizer (Martin and others, 1996). Only 80 (61%) about 3 percent of the nitrogen enters the Load in basin from point sources (municipal sew- 60 river age and industrial discharge).
Farm-animal Much of the nitrogen throughout the basin 40 manure (19%) is consumed by plant uptake and other natural NITROGEN, Point- processes. About 11 percent of the nitrogen in source the water at the mouth of the White River 20 load to
Atmospheric IN THOUSAND TONS PER YEAR deposition (17%) comes from point-source discharges; the river Municipal remainder enters the river from nonpoint sewage and 0 industrial discharge (3%) sources (Martin and others, 1996).
NITRATE CONCENTRATIONS IN STREAMS RELATED TO SOIL DRAINAGE Soil drainage is a major factor Nitrate concentrations in streams expected on the basis of percentage controlling the concentrations of increase as the proportion of well- of well-drained soils. In this water- nitrate in streams in the White River drained soils (both naturally and arti- shed, animal waste is believed to be Basin. Natural drainage is a function ficially well drained) increase. This contributing to high nitrate concen- of the coarseness of soils (a sand pattern holds for five of six agricul- trations in the stream. The amount of drains better than a clay) and the tural streams studied. The one excep- nitrogen produced by manure from slope (hills drain better than flat tion is Clifty Creek (watershed farm animals in the counties drained areas). Drainage is artificially number 2), where nitrate concentra- by Clifty Creek is higher than in each enhanced by ditches and tile drains. tions are much higher than would be of the other watersheds. 7 6 3 Nitrogen produced by manure STREAM DRAINING 2 2 6 in 1987 in tons/mi AGRICULTURAL
.28 - 2.2 WATERSHED Lost River 2.3 - 5.1 (Number on top 5.2 - 16 of bar refers to 5
Watershed 4 Clifty Creek watershed number 5 boundary 3 on map inset)
4
2 Kessinger Ditch
3
4 5 1 2
3 6
1 1 Big Walnut Creek MEDIAN NITRATE CONCENTRATION, IN MILLIGRAMS PER LITER Sugar Creek Muscatatuck River 0 0 10 20 30 40 50 60 70 80 90 PERCENTAGE OF WATERSHED WITH NATURALLY AND ARTIFICIALLY MODERATELY WELL AND WELL-DRAINED SOILS Nitrate concentrations in streams increase as the proportion of well-drained soils increases. Manure from farm animals also can increase nitrate concentrations.
U.S. Geological Survey Circular 1150 13 MAJOR FINDINGS
AQUIFER TYPE DETERMINES VULNERABILITY TO NITRATE Nitrate (shown in red) can leach downward Ground water is most vulnerable to Confined (artesian) sand and into ground water when there is more nitrate in nitrate contamination in surficial, gravel aquifers are protected from soil than plants can use. Where dissolved oxy- coarse-textured, well-drained depos- nitrate contamination by clay-rich gen concentrations in ground water are low, its such as glacial outwash (sand and glacial deposits. These confined this excess nitrate can be removed by denitrifi- gravel deposited by glacial streams). aquifers are present in more than cation (the biochemical conversion of nitrate However, nitrate contamination typi- half the basin and are a common to nitrogen gas by bacteria). Nitrate can also cally decreases with depth. (See story source of water for rural house- be removed by tile drains, which siphon off on next page.) Outwash aquifers pro- holds that use domestic wells. soil water and shallow ground water that is vide a major source of drinking water high in nitrate. (See story on next page.) in the White River Basin. Shallow monitoring Domestic well Paired shallow well and deep monitoring
wells Stream Tile drain
R£ Q¢
River Water table Clay-rich glacial deposits