scholarly journals The Development of a Dynamic Flux Chamber System for the Collection of Gaseous Emissions During On-Farm Composting of Animal Mortalities.

2006 ◽  
Author(s):  
P J Linton ◽  
B J Van Heyst
2015 ◽  
Vol 12 (6) ◽  
pp. 1683-1696 ◽  
Author(s):  
E. Bahlmann ◽  
I. Weinberg ◽  
J. V. Lavrič ◽  
T. Eckhardt ◽  
W. Michaelis ◽  
...  

Abstract. Coastal zones are important source regions for a variety of trace gases, including halocarbons and sulfur-bearing species. While salt marshes, macroalgae and phytoplankton communities have been intensively studied, little is known about trace gas fluxes in seagrass meadows. Here we report results of a newly developed dynamic flux chamber system that can be deployed in intertidal areas over full tidal cycles allowing for highly time-resolved measurements. The fluxes of CO2, methane (CH4) and a range of volatile organic compounds (VOCs) showed a complex dynamic mediated by tide and light. In contrast to most previous studies, our data indicate significantly enhanced fluxes during tidal immersion relative to periods of air exposure. Short emission peaks occurred with onset of the feeder current at the sampling site. We suggest an overall strong effect of advective transport processes to explain the elevated fluxes during tidal immersion. Many emission estimates from tidally influenced coastal areas still rely on measurements carried out during low tide only. Hence, our results may have significant implications for budgeting trace gases in coastal areas. This dynamic flux chamber system provides intensive time series data of community respiration (at night) and net community production (during the day) of shallow coastal systems.


2014 ◽  
Vol 11 (7) ◽  
pp. 10571-10603 ◽  
Author(s):  
E. Bahlmann ◽  
I. Weinberg ◽  
J. V. Lavrič ◽  
T. Eckhard ◽  
W. Michaelis ◽  
...  

Abstract. Coastal zones are important source regions for a variety of trace gases including halocarbons and sulphur-bearing species. While salt-marshes, macroalgae and phytoplankton communities have been intensively studied, little is known about trace gas fluxes in seagrass meadows. Here we report results of a newly developed dynamic flux chamber system that can be deployed in intertidal areas over full tidal cycles allowing for high time resolved measurements. The trace gases measured in this study included carbon dioxide (CO2), methane (CH4) and a variety of hydrocarbons, halocarbons and sulphur-bearing compounds. The high time resolved CO2 and CH4 flux measurements revealed a complex dynamic mediated by tide and light. In contrast to most previous studies our data indicate significantly enhanced fluxes during tidal immersion relative to periods of air exposure. Short emission peaks occured with onset of the feeder current at the sampling site. We suggest an overall strong effect of advective transport processes to explain the elevated fluxes during tidal immersion. Many emission estimates from tidally influenced coastal areas still rely on measurements carried out during low tide only. Hence, our results may have significant implications for budgeting trace gases in coastal areas. This dynamic flux chamber system provides intensive time series data of community respiration (at night) and net community production (during the day) of shallow coastal systems.


2014 ◽  
Vol 119 (9) ◽  
pp. 1789-1806 ◽  
Author(s):  
Zhongjie Yu ◽  
Lee D. Slater ◽  
Karina V. R. Schäfer ◽  
Andrew S. Reeve ◽  
Ruth K. Varner

2009 ◽  
Author(s):  
Ricardo Rafael Acevedo ◽  
Hong - Li ◽  
Hongwei - Xin ◽  
Stacey Ann Roberts

2017 ◽  
Vol 60 (4) ◽  
pp. 1235-1258 ◽  
Author(s):  
David B. Parker ◽  
Kenneth D. Casey ◽  
Richard W. Todd ◽  
Heidi M. Waldrip ◽  
Gary M. Marek ◽  
...  

Abstract. Nitrous oxide (N2O) emission rates have traditionally been measured using non-flow-through (NFT), non-steady-state (NSS) chambers, which rely on measuring the increase in N2O concentration in the sealed chamber headspace over time. These flux measurements are very labor- and time-intensive, requiring three to four gas samples collected over a 30 to 60 min period, followed by laboratory N2O measurement with a gas chromatograph (GC) and subsequent flux rate calculation. The objective of this research was to develop and evaluate improved, real-time flux chamber designs that rapidly quantify N2O emissions from manure and soil. The first chamber system consisted of six square 0.95 m2 chamber pans. The chamber pans were mounted on a rail system to facilitate controlled indoor/outdoor laboratory research at a pilot scale. An aluminum lid was moved among the chamber pans. A second portable chamber system with a circular footprint (0.49 m internal dia.) was designed for use in field measurements. With both systems, N2O concentrations were measured each second with 0.1 ppb resolution by recirculating sample air through a real-time continuous N2O analyzer with return flow into the recirculating-flow-through (RFT-NSS) chamber. Performance and observational data are presented for different chamber vent designs, sealing mechanisms between the chamber pan and lid, recirculation pumps, and presence/absence of an internal fan that mixes headspace air within the sealed chamber. As examples of the repeatability and precision of the methodology, ten consecutive flux measurements were obtained using moist manure (32.6% wet basis water content, WCWB) within a 15 min period in which chamber pans were fitted with lids for 60 s and removed for 30 s. The mean calculated N2O flux was 43.08 ±0.89 mg N2O m-2 h-1. Using dry manure (WCWB = 10.8%), five consecutive flux measurements showed a very low, but consistent, flux that averaged 0.025 ±0.0016 mg N2O m-2 h-1. Five case study experiments demonstrate the usefulness of these chamber systems and highlight discoveries and lessons learned to enhance future research efforts. Major discoveries and observations include: (1) installation of a small internal fan within the chamber lids decreased N2O fluctuation over small time periods, allowing precise measurement of manure N2O fluxes as low as 0.0073 mg N2O m-2 h-1 during a 60 s measurement period; (2) two distinct N2O peaks were observed at 1 and 21 d following the addition of water to manure (initial WCWB = 32.6%), with the second peak accounting for 83% of the total N2O emitted over 45 d; and (3) there was notable diurnal variation in N2O fluxes due to temperature variation, even when the manure was dry (WCWB = 10.8%). These flux chamber systems proved to be more rapid, precise, and repeatable than traditional flux chamber methods and offer promise for future greenhouse gas emissions research on manure and soil. Keywords: Cattle, Chamber, Diurnal, Fan, Feedlot, Greenhouse gas, Manure, Precision.


2018 ◽  
Vol 20 (3) ◽  
pp. 523-530 ◽  
Author(s):  
Adrian C. Heggie ◽  
Bill Stavropoulos

A conceptually new method to quantify mass fluxes of toxic vapours for contaminated land risk assessment applications was developed and compared against the traditional dynamic flux chamber.


Author(s):  
Ghulam Abbas Shah ◽  
Ghulam Mustafa Shah ◽  
Muhammad Imtiaz Rashid ◽  
Maqsood Sadiq ◽  
Faheem Khan ◽  
...  

We studied the influence of lava meal, zeolite and top layer of sandy soil as bedding additives on gaseous C and N losses from a sloping-floor barn of naturally ventilated animal housing. We selected four barn units where eight young bulls’ group was reared in each barn. Chopped straw of wheat and barley applied daily at the rate of 5 kg per livestock unit (LU) in bedding areas where one LU consisted of 500 kg body mass of live bulls. Zeolite, lava meal and sandy soil (18% clay + silt) applied in barn at the rate of 10, 20 and 30% of straw dose, respectively. Static flux chamber was used to measure gases emissions from the barn unit and mass balance calculation was used to calculate straw manure total N (TN) losses during housing phase. On an average, all bedding additives decreased 85% of the NH3 emission compared to control; however, they did not influence CH4 emission. Zeolite decreased CO2 (35%) and N2O (37%) emission rates. Subsequently, lava meal, sandy soil and zeolite decreased 23, 37, and 50% of TN losses from barn manure, respectively. Overall, measured N emissions through NH3-N and N2O-N from the barns was 11% of calculated TN losses while remainder 89% was most probably attributed to di-nitrogen (N2), a harmless gas. Hence, in straw-based cattle housings, zeolite could be a promising additive for reduction of CO2, N2O and NH3 emissions and sandy soil can be considered as cheap and readily available resource for reducing NH3 emission.


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