The watershed of interest is the South Fork of the Iowa River (Hardin and Hamilton Counties, Iowa). The total drainage area of this watershed is approximately 78,000 ha, and the watershed area to be evaluated is about 76,250 ha. Major sub-basins or Tipton Creek (19,850 ha), Beaver Creek (18,200 ha), and the upper South Fork (25,600 ha) are instrumented with separate gaging stations. Instrumentation of two small drainage districts (500 – 2500 ha) in Tipton Creek is planned for 2005.
The Clarion-Nicollet-Webster soil association (Typic Hapludolls – Aquic Hapludolls –Typic Haplaquolls) dominates the landscape, with Harps soils (Typic Calciaquolls) occupying glacial potholes with the Webster soil. The landscape is composed of glacial till deposited 10-15,000 years ago. The terrain is poorly dissected and internally drained “prairie potholes” are common in the upper parts of the watershed. The low relief creates poor drainage conditions, and hydric soils occupy 54% of the watershed area. A major lateral moraine of the Des Moines Lobe crosses the upper part of the watershed. Subsurface tile drains and ditches were installed beginning more than 100 years ago. The artificial drainage accelerates transport of several dissolved contaminants. Normal annual precipitation is 750 mm with 60% falling during May through August in relatively short, but intense events. Annual baseflow constitutes 60% of the total stream discharge. Much of the remaining runoff is derived from subsurface drain inlets. About 85% of the watershed is under corn and soybean rotation, and about 6% in grass (CRP) and pasture. Most of the remainder is roadways and developed land cover, only about 1% is forest or wetland. There are about 100 confined swine-feeding operations, most of which are located in Tipton Creek and the upper South Fork.
1. Water Quality: Nitrate loads from subsurface drainage systems, phosphorus,
and sediment in runoff, and pathogens in streamflow are major water quality
1. Conservation tillage (329A and 329B)
The capacity of in-field and edge-of-field conservation practices to achieve water quality goals will be evaluated in large watersheds. Landscape assessment will use terrain-modeling techniques, applied to widely available data on topography, soils, and climate to conceptualize areas where conservation practices will be most effective. A comprehensive evaluation of the distribution of existing conservation practices in the watershed will be undertaken, with assistance from NRCS.
Synoptic sampling and long-term monitoring will be used to determine nutrient, sediment, and pathogen loads in streams draining watersheds at nested scales, and assess retentions and losses associated with conservation practices. The distribution of practices and sensitive areas within the watershed and its sub-basins will guide the final experimental design. Increased funding for new conservation practices (e.g., EQIP), if available, along with collaboration with the Southfork Alliance will help encourage implementation of new conservation practices. Paired watershed comparisons and/or water quality trends will be evaluated to determine the impact of new practices that producers volunteer to implement. Results will also be used to parameterize models (EPIC, SWAT) that predict the effects of management systems on watershed processes and water quality.
Soil quality assessments will be made using existing data, and employing two different approaches. First, recognizing that soil organic matter is a primary indicator of soil quality and an important factor in carbon sequestration and global change, the NRCS Soil Conditioning Index (SCI) will be used to assess the consequences of the tillage and cropping systems being used within the watershed. The SCI will provide estimates on whether the applied conservation practices are maintaining or increasing soil organic matter. The predictions will be verified with the available data being collected by either the farmer-cooperators (i.e. through their soil test records) or other researchers contributing to the overall CEAP database. A more comprehensive assessment of soil quality will be made using the Soil Management Assessment Framework (SMAF) that is currently being developed by the ARS and the NRCS Soil Quality Institute. SMAF is designed to evaluate the dynamic impact of soil management practices on soil function and consists of three steps: indicator selection, indicator interpretation, and integration into an index. Designed as a framework, SMAF allows researchers to continually update and refine the interpretations for many soils, climates, and land use practices. Therefore, in addition to providing soil quality assessments for CEAP, the project will provide data for further improvements of the SMAF. This will occur by applying decision rules based on management goals and other site-specific factors in the selection step for each watershed. The interpretation step will provide site-specific indicator scores. Individually and collectively (through the index), the indicator scores will be correlated to critical endpoints including crop yield, water quality (i.e. nitrate, phosphorus, and sediment loads), and air quality indicators.Selected References
Tomer, M.D., and D.E. James. 2004. Do soil surveys and terrain analyses
identify similar priority sites for conservation? Soil Sci. Soc. Am. J.
Southfork Watershed Alliance, a local organization, is working to encourage implementation of conservation
practices that can protect and improve water quality.