A Wind Tunnel for Measuring Selenium Volatilization under Field‐Like Conditions

A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field‐like conditions. The wind tunnel consisted of a volatilization chamber made of Plexiglas (2.4 m long × 0.8 m wide × 1.2 m high), which was set above a stainless steel lysimeter (0.5 m2 surface area × 0.8...

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Published inJournal of environmental quality Vol. 29; no. 2; pp. 460 - 466
Main Authors Dungan, R. S., Stork, A., Frankenberger, W. T.
Format Journal Article
LanguageEnglish
Published Madison, WI American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America 01.03.2000
Crop Science Society of America
American Society of Agronomy
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Abstract A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field‐like conditions. The wind tunnel consisted of a volatilization chamber made of Plexiglas (2.4 m long × 0.8 m wide × 1.2 m high), which was set above a stainless steel lysimeter (0.5 m2 surface area × 0.8 m deep). High air exchange rates (avg. 700 air changes h−1) were used to simulate field‐like environmental conditions inside the wind tunnel. To monitor the fate and transport of the Se, radiolabeled 75Se as sodium selenite (Na275SeO3) was incorporated into the top 5 cm of soil. Volatile Sc was trapped on activated carbon filters and measured directly using gamma counting. A 135‐d bare‐soil experiment was carried out, during which 2.7% of the Se was released through volatilization without added C. The average flux rate of gaseous Se was 17 mg m−2 h−1, with a high of 72 mg m−2 h−1 occurring on Day 6. After 135 d, 59 and 34% of the 75Se was located in the 0 to 5 and 5 to 10 cm soil layers, respectively. A total of 84.5% of all applied 75Se was recovered. The purpose of this study was to improve estimates on Se volatilization from seleniferous soils and help close the gap between previous laboratory and field experiments.
AbstractList A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field-like conditions. The wind tunnel consisted of a volatilization chamber made of Plexiglas (2.4 m long x 0.8 m wide x 1.2 m high), which was set above a stainless steel lysimeter (0.5 m{sup 2} surface area x 0.8 m deep). High air exchange rates (avg. 700 air changes h{sup {minus}1}) were used to simulate field-like environmental conditions inside the wind tunnel. To monitor the fate and transport of the Se, radiolabeled {sup 75}Se as sodium selenite (Na{sub 2}{sup 75}SeO{sub 3}) was incorporated into the top 5 cm of soil. Volatile Se was trapped on activated carbon filters and measured directly using gamma counting. A 135-d bare-soil experiment was carried out, during which 2.7% of the Se was released through volatilization without added C. The average flux rate of gaseous Se was 17 mg m{sup {minus}2} h{sup {minus}1}, with a high of 72 mg m{sup {minus}2} h{sup {minus}1} occurring on Day 6. After 135 d, 59 and 43% of the {sup 75}Se was located in the 0 to 5 and 5 to 10 cm soil layers, respectively. A total of 84.5% of all applied {sup 75}Se was recovered. The purpose of this study was to improve estimates on Se volatilization from seleniferous soils and help close the gap between previous laboratory and field experiments.
Abstract A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field‐like conditions. The wind tunnel consisted of a volatilization chamber made of Plexiglas (2.4 m long × 0.8 m wide × 1.2 m high), which was set above a stainless steel lysimeter (0.5 m 2 surface area × 0.8 m deep). High air exchange rates (avg. 700 air changes h −1 ) were used to simulate field‐like environmental conditions inside the wind tunnel. To monitor the fate and transport of the Se, radiolabeled 75 Se as sodium selenite (Na 2 75 SeO 3 ) was incorporated into the top 5 cm of soil. Volatile Sc was trapped on activated carbon filters and measured directly using gamma counting. A 135‐d bare‐soil experiment was carried out, during which 2.7% of the Se was released through volatilization without added C. The average flux rate of gaseous Se was 17 mg m −2 h −1 , with a high of 72 mg m −2 h −1 occurring on Day 6. After 135 d, 59 and 34% of the 75 Se was located in the 0 to 5 and 5 to 10 cm soil layers, respectively. A total of 84.5% of all applied 75 Se was recovered. The purpose of this study was to improve estimates on Se volatilization from seleniferous soils and help close the gap between previous laboratory and field experiments.
A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field‐like conditions. The wind tunnel consisted of a volatilization chamber made of Plexiglas (2.4 m long × 0.8 m wide × 1.2 m high), which was set above a stainless steel lysimeter (0.5 m2 surface area × 0.8 m deep). High air exchange rates (avg. 700 air changes h−1) were used to simulate field‐like environmental conditions inside the wind tunnel. To monitor the fate and transport of the Se, radiolabeled 75Se as sodium selenite (Na275SeO3) was incorporated into the top 5 cm of soil. Volatile Sc was trapped on activated carbon filters and measured directly using gamma counting. A 135‐d bare‐soil experiment was carried out, during which 2.7% of the Se was released through volatilization without added C. The average flux rate of gaseous Se was 17 mg m−2 h−1, with a high of 72 mg m−2 h−1 occurring on Day 6. After 135 d, 59 and 34% of the 75Se was located in the 0 to 5 and 5 to 10 cm soil layers, respectively. A total of 84.5% of all applied 75Se was recovered. The purpose of this study was to improve estimates on Se volatilization from seleniferous soils and help close the gap between previous laboratory and field experiments.
Author Stork, A.
Dungan, R. S.
Frankenberger, W. T.
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  surname: Frankenberger
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  organization: Univ. of California
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Issue 2
Keywords Natural origin pollution
Atmospheric condition
Radioactive tracers
Pollutant emission
Selenium 75
Wind tunnel
Medium effect
Volatilization
Air pollution
Air ground interface
Measurement method
Selenium
Field study
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PublicationTitle Journal of environmental quality
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Snippet A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field‐like conditions. The wind tunnel consisted of a volatilization...
Abstract A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field‐like conditions. The wind tunnel consisted of a...
A wind tunnel was developed to measure the loss of volatile selenium (Se) from soil under field-like conditions. The wind tunnel consisted of a volatilization...
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SubjectTerms AIR-BIOSPHERE INTERACTIONS
Analysis methods
Applied sciences
Atmospheric pollution
Dispersed sources and other
ENVIRONMENTAL SCIENCES
ENVIRONMENTAL TRANSPORT
Exact sciences and technology
MONITORING
Pollution
Pollution sources. Measurement results
SELENIUM
SOILS
VOLATILITY
WIND TUNNELS
Title A Wind Tunnel for Measuring Selenium Volatilization under Field‐Like Conditions
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