A global database of methane, nitrous oxide and ammonia emission factors for livestock housing and outdoor storage of manure

Livestock manure management systems can be significant sources of nitrous oxide (N2O) methane (CH4) and ammonia (NH3) emissions. Many studies have been conducted to improve our understanding of the emission processes and to identify influential variables in order to develop mitigation techniques adapted to each manure management step (animal house, outdoor storage, and manure spreading to land). The international project DATAMAN (http://www.dataman.co.nz) aims to develop a global database on greenhouse gases (N2O, CH4) and NH3 emissions from the manure management chain to refine emission factors (EF) for national greenhouse gas (GHG) and NH3 inventories. This paper deals with the housing and outdoor storage components of this database. Relevant information for different animal categories, manure types, livestock buildings, outdoor storage and climatic conditions were collated from published peer reviewed research, conference papers and existing databases published between 1995 and 2021. The storage database contains 654 NH3 EF from 16 countries, 243 CH4 EF from 13 countries and 421 N2O EF from 17 countries. Across all gases, dairy cattle and swine production in temperate climate zones are the most represented animal and climate categories. In the housing database, 2024 EF were collated (63% for NH3, 19.5% for CH4 and 17.5% for N2O). As for the storage database, the number of EF for the tropical climate zone is under-represented with only 8 values included. The DATAMAN database can be used for the refinement of national inventories and better assessment of the cost-effectiveness of a range of mitigation measures

Model for calculating ammonia emission from stored animal liquid manure

National inventories calculate ammonia emission from livestock manure using static emission factors. These do not account for local environmental condition, management practice or variation in manure composition. We present a model that estimates emission from liquid manure per area and time as related to slurry composition, temperature and surface covers. Data was extracted from articles and used to parameterize and validate the model, and the scenario calculations demonstrate the usefulness of the model

Validation of NH3 observations from AIRS and CrIS against measurements from DISCOVER-AQ and the Magic Valley

Ammonia is one of the most common forms of reactive nitrogen and the primary alkaline gas in the atmosphere. Intended and unintended releases of ammonia into the environment over the last century have significantly altered the natural nitrogen cycle, so that the current emission levels of ammonia are about four times higher than in previous centuries. Ammonia is the dominant base in the atmosphere, and it plays a significant role in the formation of fine particulate matter (PM2.5) which can penetrate deep into the lungs and severely impact the respiratory and circulatory systems. In situ measurement of ammonia remains a challenge as ammonia is easy to detect, but it is hard to measure accurately. The high spatial and temporal variability of ammonia exacerbates the lack of continuous, spatially well sampled data over extensive regions. Satellite data, even though they come with their own uncertainties, provide by virtue of their spatial and temporal density, another option for quantifying ammonia emissions. Our objective was to add to the satellite validation record at the single pixel scale, using aircraft and ground ammonia measurements with satellite retrievals from both the Atmospheric Infrared Sounder (AIRS) and Cross-track Infrared Sounder (CrIS) instruments. The AIRS and CrIS profiles individually have large uncertainties, which are driven by local conditions, most significantly temperature profiles and sub-pixel heterogeneity. However, average biases between satellite and aircraft data, after smoothing errors are accounted for, are below or close to 1 ppbv. Use of ground base measurements for validation clearly demonstrate the importance of having more than a few dozen data points to obtain useful information from space-based retrievals of ammonia. With 464 observations over three years, over a small region, it was possible to obtain a clear picture of the source distribution in the region through the application of a physics based oversampling algorithm

Nutrient Availability to Corn From Dairy Manures and Fertilizer in a Calcareous Soil

The expansion of the dairy industry in southern Idaho has lead to increased application of manures to meet crop nutrient demands which can alter the uptake pattern of both macro- and micro-nutrients. A greenhouse study was conducted to determine the effects of dairy manure, composted dairy manure, and fertilizer (mono-ammonium phosphate, MAP) application on soil test phosphorus (P), microbial activity, and nutrient uptake by silage corn. Two Portneuf soils, having either a low or high soil test P concentration, were amended with the three treatments at four application rates (25, 50, 100, and 200 mg P kg-1) with four replications of each treatment in a randomized complete design. Treatments were incubated for two weeks, then planted with corn grown for approximately three weeks. Soil samples were analyzed prior to planting, whereas plant samples were analyzed at the end of the growing period. Increases in Olsen P from P additions were greatest in the MAP and least in the manure treated soils. Plant dry matter production and tissue P concentration did not differ with treatment. Tissue K increased with manure and compost addition while tissue Ca decreased; there was also a decrease in tissue Mg with compost application. Tissue Zn increased with manure applications, while tissue Mn decreased with manure and compost application on the Low-P soil. It is important to consider plant nutrient interactions when applying manure and compost to feed-crops as imbalances in K, Ca, and Mg can have a negative impact on animal health

The characterization of microorganisms in dairy wastewater storage ponds

Dairy wastewaters from storage ponds are commonly land applied to irrigate silage crops. Given that diverse microbial populations are associated with cattle feces, the objective of this study was to use a culture-independent approach to characterize Bacteria and Archaea in dairy wastewaters. Using domain-specific primers, a region of the 16S rRNA gene was amplified from pooled DNA extracts from 30 dairy wastewaters and subsequently used to create a clone library. A total of 152 bacterial clones were examined and sequence matches were affiliated with the following groups: Actinobacteria, Bacteroidetes, Firmicutes, Proteobacteria, and Synergistetes. Firmicutes was identified as the largest phylum representing up to 69% of the clone sequences. Of 167 clones representing Archaea, 7 genera were found to be closely related (91–100% sequence similarity) to isolates obtained from sediments and feces. Most of the putative sequence matches (98%) represented members from the class Methanomicrobia. With respect to the archaeal clones, only one of the putative sequence matches was affiliated with a methanogenic bacterium known to inhabit the rumen. Our results suggest that the dairy wastewater ponds do not support populations of methanogenic bacteria normally found in the cattle rumen

Removing soluble phosphorus in irrigation return flows with alum additions

ABSTRACT: Phosphorus (P) losses from irrigated cropland transferred to surface waters via irrigation return flows, can impair regional water quality. Best management practices to reduce soil erosion on fields and sediment concentration in return flows do little to reduce soluble P concentrations, which can exceed total maximum daily load (TMDL) limits for total P. Laboratory and field tests were conducted to evaluate the effect of alum on soluble P concentration in return flow water from an irrigation tract in southern Idaho. The laboratory study used two water sources (tap and irrigation), three sediment concentrations (0, 100 and 1000 mg L-1), two added P concentrations (0 and 1 mg L-1), and five alum concentrations (0, 5, 10, 20 and 40 mg L-1). Field tests were conducted at sediment ponds on two irrigation drains with 20 to 500 mg L-1 sediment and 0.09 to 0.19 mg L-1 dissolved P in inflow water. Regression analysis of laboratory data showed a 53 percent reduction in soluble P concentration with 20 mg L-1 alum, which was similar to field data. Applying 40 mg L-1 alum to irrigation water reduced soluble P concentrations up to 98 percent in the field. Achieving 50 percent soluble P reduction would cost about $0.007 m-3 ($8.25 per ac ft) at the current alum cost of $0.33 kg-1 ($0.15 lb-1). Although alum effectively reduced soluble P in irrigation return flow, the cost of applying alum may be too high for routine use in many irrigation districts

Environmental implications of inositol phosphates in animal manures

Animal production in the USA is valued at more than $100 billion and has consolidated significantly during the last 20 years, with a larger number of animals being produced on an increasingly smaller land base (Kellogg et al., 2000). Manure generated from animal production is currently estimated to exceed 335 million t of dry matter per year in the USA, while global manure production is estimated at —13 billion t of dry matter per year (Mullins et al., 2005). Manures contain significant amounts of phosphorus, with values between 6.7 and 29.1 g P/kg on a dry weight basis reported for several species of animals (Barnett, 1994). This phosphorus includes inorganic and organic forms, with the latter constituting between 10°/a and 80% of the total (Peperzak et al., 1959; Gerritse and Zugec, 1977). Inositol phosphates are one of the primary organic phosphorus species found in manures, with myo-Inositol hexakisphosphate typically being the most abundant (Peperzak el al., 1959; Barnett, 1994; Turner and Leytem, 2004)

Changes in soil test phosphorus from broiler litter additions

Nutrient surpluses on the Delmarva Peninsula have led to a continual accumulation of soil test phosphorus (STP), a potential source for transport of phosphorus (P) to surface waters. This article examines the effects of initial soil test P concentrations and broiler litter additions on STP accumulation. Broiler litter (BL) was applied at rates of 0, 2.5, 5, 7.5, and 10 g kg -1 (dry weight) to three soils: an Evesboro sandy loam (Mesic, coated Typic Quartzipsamments), a Pocomoke sandy loam (coarseloamy, siliceous, thermic typic Umbraquults), and a Matapeake silt loam (fine-silty, mixed, semiactive, mesic Typic Hapludults). Soils and BL were incubated for 16 weeks with subsamples analyzed after 4 and 16 weeks. There was a linear increase in STP (Mehlich-3), water-soluble P (WS-P), iron-oxide strip-extractable P (FeO-P), and Mehlich-3 phosphorus saturation ratio (M3-PSR) with broiler litter additions. Regression analysis indicated few significant differences in STP response to added BL between soils within the same soil group having different initial STP levels. Correlation analysis and stepwise regression indicated that increases in WS-P and FeO-P from added BL were more closely related to the degree of P saturation of the soil rather than traditional STP measurements. Therefore, decisions regarding manure placement within a watershed should be based on the potential P sorption capacity of the soil as well as potential P transport pathways when the goal is the reduction of P transfer to waterbodies

Impact of sheep bedding on soil nutrient dynamics in the Centennial Mountains of Montana and Idaho

Sheep and lamb production is an important industry in Idaho, with summer sheep grazing in the mountains a common practice. Sheep are concentrated in bedding areas at night leading to concentrated grazing and manure and urine accumulation in these areas. To address the effects of bedding on soil nutrient status, we monitored 16 bedding areas in the Centennial Mountains, with a general survey performed in 2004 followed by more intense monitoring of six sites from 2005 to 2006. In 2004, soils were analyzed for total carbon (C) and nitrogen (N), organic C, total P, Olsen P, water-soluble phosphorus (WSP), soluble nitrate, and soluble ammonium. Over the period 2005–2006, soils were analyzed for soluble nutrients including Olsen P, WSP, soluble nitrate, and soluble ammonium. The 16 sites evaluated in 2004 had significantly greater total N, C, and organic C concentrations in the nonbedded areas, whereas Olsen P, WSP, and ammonium concentrations were greater in the bedding areas. When six sites were monitored over time, there was no significant effect of bedding on soluble P concentrations over time or between bedding and control areas, whereas there was a significant effect of time on soluble N concentrations but no significant differences between bedding and control areas. Although these results are preliminary, it seems as if sheep bedding can alter the nutrient content of soils increasing some measures of soil nutrients, while decreasing others, which ultimately can affect the productivity and plant species diversity in these areas

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