Spatial distribution of ammonia concentrations and modelled dry deposition in an intensive dairy production region

Agriculture generates ~83% of total U.S. ammonia (NH3) emissions, potentially adversely impacting sensitive ecosystems through wet and dry deposition. Regions with intense livestock production, such as the dairy region of south-central Idaho, generate hotspots of NH3 emissions. Our objective was to measure the spatial and temporal variability of NH3 across this region and estimate its dry deposition. Ambient NH3 was measured using diffusive passive samplers at 8 sites in two transects across the region from 2018-2020. NH3 fluxes were estimated using the Surface Tiled Aerosol and Gaseous Exchange (STAGE) model. Peak NH3 concentrations were 4-5 times greater at a high-density dairy site compared to mixed agriculture/dairy or agricultural sites, and 26 times greater than non-agricultural sites with prominent seasonal trends driven by temperature. Annual estimated dry deposition rates in areas of intensive dairy production can approach 50 kg Nitrogen ha/yr, compared to < 1 kg Nitrogen ha/yr in natural landscapes. Modeling work highlighted a need for better understanding of soil emission potential in environments with high soil pH and low leaf area. Research toward better understanding soil processes is needed to improve understanding of ammonia dry deposition to arid and sparsely vegetated natural ecosystems across the western U.S

Patterns and associations between dominant crop productions and water quality in an irrigated watershed

Irrigation consumes the largest share of freshwater resources but is a necessary practice to boost agricultural output to meet increasing global demand for food and fiber. Irrigation not only impacts water quantity but can also degrade water quality. Research efforts have explored various aspects of irrigation efficiency and irrigated crop productivity, but few studies have examined how different crops collectively modulate water utilization and water quality at the watershed scale. In this study long-term water quantity and quality monitoring data collected as part of the Conservation Effect Assessment Project (CEAP) combined with crop and evapotranspiration (ET) modeling products were used to elucidate relationships between crop and water processes in an irrigated watershed. We use a correlational approach to build relationships between water quantity and quality metrics and the fractional volumes of ET associated with major crops in the Twin Falls Canal Company irrigation tract. Results suggest that sub-watershed size and subsurface flow contribution in drainage tunnels influenced hydrologic patterns observed and led to 2 distinct groups. Group 1 sub-watersheds were large, typically included subsurface drain tunnels and had high return flow volumes and low sediment concentration while group 2 sub-watersheds were smaller in size, had low return flow volumes and high sediment concentration. Irrigation return flow volume normalized by sub-watershed area was positively associated with ET fractions of potato (Solanum tuberosum) in group 1 during the spring and summer months. Spring sediment loss per return flow volume showed a negative association with ET fractions of sugar beet and combined alfalfa (Medicago sativa) and pasture crops in group 2. A negative association was found between phosphorus (P) load per return flow volume and ET fractions of alfalfa / pasture, corn (Zea mays), dry beans (Phaseolus vulgaris), and sugar beet (Beta vulgaris) across sub-watershed groups. Nitrate (NO3-N) load per return flow volume was negatively associated with potato and corn ET fractions in group 1 especially during the spring and fall month but positively associated with dry beans over the irrigation season. While direct cause and effect were not established between crops and water quantity and quality, results from this study provide valuable information on management factors associated with various crop production systems that may control observed hydrologic response. Example of factors considered in explaining some of the observed patterns include early germination and ground coverage, tight control on soil water content, and the erosion attenuation effect of sedimentation ponds

Climate change in a semi-arid environment: effects on crop rotation with dairy manure application

Agricultural crops grown in the irrigated semi-arid region of southern Idaho account for almost two-thirds of the median household income in the region. The impacts of climate change on cropping systems and the availability of water for irrigation would be a serious challenge for the state's economic dependence on agriculture. The objective of the study was to simulate the future impact of climate change on a crop rotation of spring wheat-potato-spring barley-sugarbeet grown in the semi-arid region of southern Idaho using conventional management practices and a high dairy manure application. The Root Zone Water Quality Model (RZWQM2) simulations used bias-corrected and spatially disaggregated projections from the World Climate Research Program’s coupled model inter-comparison project phase 5 to generate 40 GCM projections for the time from 2071-2099. The 28-yr scenarios were designed to simulate the impact of temperature and CO2 regimes on crop production, soil nitrogen mineralization, nitrogen seepage, deep seepage of water, and nitrous oxide emissions. Data from a field experiment in southern Idaho with conventional fertilizer practices and annual applications of 52 Mg ha-1 dairy manure with a crop rotation of spring wheat-potato-spring barley-sugarbeet were used in the RZWQM2 simulations. Results were compared to a baseline scenario of conventional management practices, historical weather data, and ambient CO2. Spring wheat yield increased by 22% and 16% for manure and fertilizer treatments, respectively, compared to the baseline scenario. Using the same comparison, potato tuber yield decreased by 65% and 60% in the manure and fertilizer treatments, respectively, for the highest temperature and CO2 increase scenarios. Spring barley produced a 33% higher yield with increased temperature and CO2. However, yield decreased when temperature increased, but CO2 remained unchanged. Sugarbeet yields decreased by 16% and 18% for manure and fertilizer treatments, respectively, compared to the baseline scenario. Nitrogen mineralization, N seepage from the profile, and nitrous oxide emissions were strongly influenced by the manure applications, and there was little simulated impact of climate change on these processes. These simulation results indicate that genetic enhancements or alternative management will be needed to maintain potato and sugar beet production levels in semi-arid areas, while spring barley and wheat yields may increase, assuming adequate irrigation water supplies are available

Moving toward sustainable irrigation in a southern Idaho irrigation project

Private and public irrigation development projects were a fundamental part of bringing irrigation arid regions of the western U.S. The Twin Falls Canal Company in southern Idaho provides a case study of private and public irrigation development because the project was developed by private investors under the Carey Act and receives a portion of its irrigation water from Bureau of Reclamation reservoirs. The project survived initial financial struggles and waterlogged soil to focus on sustaining the production by reducing chronic furrow irrigation erosion and nutrient losses in irrigation return flow. Average sediment loss from the project was 460 kg/ha in 1970. A cooperative effort by the canal company, state and federal agencies, and farmers improved water quality by installing sediment ponds on fields, applying polyacrylamide with furrow irrigation, converting from furrow to sprinkler irrigation, and constructing water quality ponds on irrigation return flow streams. From 2006-2018, the project retained on average 165 kg/ha of sediment and 0.4 kg/ha of total phosphorus annually, which removed 13,000 Mg of sediment and 33 Mg of total phosphorus from the Snake River each year. Nitrate-N from subsurface drainage, however, was lost at 10 kg/ha each year, which is equivalent to 380 Mg of urea fertilizer from the entire project. While sediment and phosphorus concentrations in irrigation return flow have decreased, they were still greater than the irrigation water concentrations, indicating that more can be done to reduce the project’s influence on water quality in the Snake River

A strategic plan for future USDA- Agricultural Research Service erosion research and model development

Soil erosion is a natural process, and the erosion potential of a site is the result of complex interactions among soil, vegetation, topographic position, land use and management, and climate. Soil erosion occurs when aeolian and hydrologic processes exceed a soil’s inherent resistance to these forces. Soil erosion was recognized as a significant problem at both local and national scales in the United States in the 1920s; by 1935 soil erosion was considered a national disaster, covering over one-half of the country (Sampson and Weyl 1918; Weaver 1935), and is still a concern with 21% of the western United States degraded and vulnerable to accelerated soil erosion (Herrick et al. 2010; Weltz et al. 2014a; Duniway et al. 2019). In 1995, it was estimated that 4 × 109 t (4.4 × 109 tn) of soil was lost from US cropland (Pimentel et al. 1995). The most vulnerable areas for soil movement and thus erosion occur where annual precipitation is 100 to 400 mm y–1 (4 to 16 in yr–1), which limits soil moisture available to sustain plant growth. Anthropogenic-driven dust emissions have dramatically increased across the globe (Webb and Pierre 2018) and in the United States (Neff et al. 2008) over last several decades. On-site and off-site costs associated with wind erosion exceeds US$8 billion y–1 Huszar and Piper 1986; USDA 1993). The combined off-site and on-site costs of erosion from agriculture in the United States is estimated to be about US$44 billion y–1, or about US$100 ha–1 (US$40 ac–1) of cropland and pasture (Pimentel et al. 1995), and US$44.5 billion in the European Union (Montanarella 2007). Cropland and livestock production contribute US$132.8 billion or 1% of the US gross domestic product. Erosion increases production costs by ~25% each year