Science Inventory

Metrics for Nitrate Contamination of Ground Water at CAFO Land Application Site - Iowa Swine Study

Citation:

Hatfield, J. L. Metrics for Nitrate Contamination of Ground Water at CAFO Land Application Site - Iowa Swine Study. U.S. Environmental Protection Agency, Washington, DC, EPA/600/R-09/045, 2009.

Impact/Purpose:

The objectives of this research were to monitor changes in soil nutrient composition at various depths in response to various scenarios of swine manure applications according to an approved CNMP and determine if site characteristics or management protocols that pose a risk to ground water can be identified.

Description:

Nitrate (NO3-) is the most common chemical contaminant found in ground water and there are increasing indications that agriculture contributes to this contamination. In the United States, concentrated animal feeding operations (CAFO) are a common agricultural practice. CAFO lead to concentrated production of animal waste and manure. In most instances, this manure is then utilized as an input for crop production because the manure is relatively rich in plant nutrients, including nitrogen (N) and phosphorus (P). Manure disposal on agricultural land by CAFO is usually dictated by a Comphrensive Nutrient Management Plan (CNMP or NMP). The stated intention of the CNMP is to utilize the manure as beneficially as possible without a high risk of contaminating surface and ground water. The objectives of this research were to monitor changes in soil nutrient composition at various depths in response to various scenarios of swine manure applications according to an approved CNMP and determine if site characteristics or management protocols that pose a risk to ground water can be identified. A study was conducted for one year (2006) on a swine-row crop farm in central Iowa. The row crop operation consisted primarily of corn (Zea mays L.) –soybean (Gylcine max (L.) Merr.) rotation. Swine production consisted of growing-finishing operation of 4,200 head. Swine waste was stored in pits for up to a year before being applied. Land application consisted of injecting the effluent into a slit approximately 20 cm below the soil’s surface. Eight plots (10 x 10 m) were established. Two plots were in a field in which swine manure effluent was applied in the fall to supply a corn crops’ N requirement (approximately 150 kg N ha-1). Four plots were in a field in which swine manure effluent was applied in the spring to supply approximately 100 kg N ha-1 with the additional crop N (50 kg ha -1) being supplied post-planting as side-dressed fertilizer. The last two plots were in soybeans field, one of which received swine effluent application in 2005 and the other did not. Soil core samples (0-15, 15-30, 30-45, 45-60, and 60-120 cm depths) were taken in May (planting time) and October (after harvesting). Soil samples from the top 22.5 cm were also collected biweekly throughout the growing season. These samples were analyzed for soluble components (nitrate, ammonium, SRP, pH, and EC), as well as exchangeable ammonium and Mehlich III extractable P. Plant samples were also collected and analyzed for biomass and N content. Detailed soil sampling revealed that soil N and P concentrations were greatest in the upper 20 and 10 cm, respectively. In addition, the variations in soil P and N were greater at the soil surface than at lower depths. Concentrations of soil P and N at all depths decreased during the growing season. The largest decrease in soil P and N concentrations was found in the upper 10 cm, and at 20-40 cm, respectively. Nutrient removal from the soil was also calculated from changes in soil concentrations. Changes in soil N concentration indicated that the soybean and corn crop removed approximately 140 and 200 N ha-1. Analyses of the plant biomass indicated that approximately 140 and 200 kg N ha-1 had been accumulated in the soybean and corn crop, respectively. Crop removal by the two methods was in excellent agreement. The results from this study indicate that application of swine manure effluent at this farm according to the existing CNMP should supply N in sufficient amounts for crop production without leading to a further accumulation of N in the soil. Sparse rainfall during the early part of 2006 growing season resulted in weather that was not typical of central Iowa. Therefore, far reaching conclusions from this research may not be possible. The use of soil characteristics in the top soil as indicators of the potential of downward movement of soil N and P will be made more difficult by the large variations in soil N and P concentrations in this zone.

Record Details:

Record Type:DOCUMENT( PUBLISHED REPORT/ REPORT)
Product Published Date:10/22/2009
Record Last Revised:07/14/2011
OMB Category:Other
Record ID: 205669