Sheryl H. Ehrman
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Previous Organizations / Institutes
The organizations / institutes from the scholar's other articles in the past ten years
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Research Interests
Sheryl H. Ehrman has a total of 98 co-authors. Here are the top co-authors by number of shared publications:
- Russell R. Dickerson
Department of Atmospheric and Oceanic Science University of Maryland College Park MD USA
7 shared publications - Yujia Liang
Department of Chemical and Biomolecular Engineering University of Maryland College Park MD 20742 USA
7 shared publications - Xinrong Ren
NOAA Air Resources Laboratory (College Park, United States of America)
5 shared publications - Doyeon Ahn
Goddard Earth Sciences Technology and Research (GESTAR) II Morgan State University Baltimore MD USA
4 shared publications - Hao He
Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD 20742, USA
4 shared publications Howard Glicksman
DuPont Electronic Technologies , Research Triangle Park, North Carolina 27709, United States
4 shared publications
Latest Publications
- Open Access
- 28 April 2019
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 46 (8) , 4531-4540
Estimating Methane Emissions From Underground Coal and Natural Gas Production in Southwestern Pennsylvania
Production of coal and natural gas is responsible for one third of anthropogenic methane (CH4) emissions in the United States. Here we examine CH4 emissions from coal and natural gas production in southwestern Pennsylvania. Using a top‐down methodology combining measurements of CH4 and ethane, we conclude that while Environmental Protection Agency inventories appear to report emissions from coal accurately, emissions from unconventional natural gas are underreported in the region by a factor of 5 (±3). However, production‐scaled CH4 emissions from unconventional gas production in the Marcellus remain small compared to other basins due to its large production per well. After normalizing emissions by energy produced, total greenhouse gas emissions from Pennsylvania unconventional natural gas production produce half the carbon footprint compared to regionally produced coal, with carbon dioxide emissions from combustion being the dominant source of greenhouse gas emissions for both sources.
- 28 April 2019
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 46 (8) , 4531-4540
Open AccessEstimating Methane Emissions From Underground Coal and Natural Gas Production in Southwestern Pennsylvania
Production of coal and natural gas is responsible for one third of anthropogenic methane (CH4) emissions in the United States. Here we examine CH4 emissions from coal and natural gas production in southwestern Pennsylvania. Using a top‐down methodology combining measurements of CH4 and ethane, we conclude that while Environmental Protection Agency inventories appear to report emissions from coal accurately, emissions from unconventional natural gas are underreported in the region by a factor of 5 (±3). However, production‐scaled CH4 emissions from unconventional gas production in the Marcellus remain small compared to other basins due to its large production per well. After normalizing emissions by energy produced, total greenhouse gas emissions from Pennsylvania unconventional natural gas production produce half the carbon footprint compared to regionally produced coal, with carbon dioxide emissions from combustion being the dominant source of greenhouse gas emissions for both sources.
- Open Access
- 5 February 2019
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 124 (3) , 1862-1878
Methane Emissions from the Marcellus Shale in Southwestern Pennsylvania and Northern West Virginia Based on Airborne Measurements
Natural gas production in the United States has increased rapidly over the past decade, along with concerns about methane (CH4) fugitive emissions and its climate impacts. Quantification of CH4 emissions from oil and natural gas (O&NG) operations is important for establishing scientifically sound policies for mitigating greenhouse gases. We use the aircraft mass balance approach for three flight experiments in August and September 2015 to estimate CH4 emissions from O&NG operations over the southwestern Marcellus Shale. We estimate a mean CH4 emission rate as 21.2 kg/s with 28% coming from O&NG operations. The mean CH4 emission rate from O&NG operations was estimated to be 1.1% of total NG production. The individual best‐estimate emission rates from the three flight experiments ranged from 0.78 to 1.5%, with overall limits of 0% and 3.5%. These emission rates are at the low end of other top‐down studies, but consistent with the few observational studies in the Marcellus Shale region as well as the U.S. Environmental Protection Agency CH4 inventory. A substantial source of CH4 (~70% of observed CH4 emissions) was found to contain little ethane, possibly due to coalbed CH4 emitted either directly from coal mines or from wells drilled through coalbed layers in O&NG operations. Recent regulations requiring capture of gas from the completion‐venting step of hydraulic fracturing appear to have reduced the atmospheric release of CH4. Our study suggests that for a 20‐year time scale, energy derived from the combustion of natural gas extracted from this region likely exerts a net climate benefit compared to coal.
- 5 February 2019
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 124 (3) , 1862-1878
Open AccessMethane Emissions from the Marcellus Shale in Southwestern Pennsylvania and Northern West Virginia Based on Airborne Measurements
Natural gas production in the United States has increased rapidly over the past decade, along with concerns about methane (CH4) fugitive emissions and its climate impacts. Quantification of CH4 emissions from oil and natural gas (O&NG) operations is important for establishing scientifically sound policies for mitigating greenhouse gases. We use the aircraft mass balance approach for three flight experiments in August and September 2015 to estimate CH4 emissions from O&NG operations over the southwestern Marcellus Shale. We estimate a mean CH4 emission rate as 21.2 kg/s with 28% coming from O&NG operations. The mean CH4 emission rate from O&NG operations was estimated to be 1.1% of total NG production. The individual best‐estimate emission rates from the three flight experiments ranged from 0.78 to 1.5%, with overall limits of 0% and 3.5%. These emission rates are at the low end of other top‐down studies, but consistent with the few observational studies in the Marcellus Shale region as well as the U.S. Environmental Protection Agency CH4 inventory. A substantial source of CH4 (~70% of observed CH4 emissions) was found to contain little ethane, possibly due to coalbed CH4 emitted either directly from coal mines or from wells drilled through coalbed layers in O&NG operations. Recent regulations requiring capture of gas from the completion‐venting step of hydraulic fracturing appear to have reduced the atmospheric release of CH4. Our study suggests that for a 20‐year time scale, energy derived from the combustion of natural gas extracted from this region likely exerts a net climate benefit compared to coal.
- 5 September 2018
- Published by American Chemical Society (ACS) in The Journal of Physical Chemistry C
- Vol. 122 (39) , 22232-22240
Rational Design of Core–Shell-Structured Particles by a One-Step and Template-Free Process for High-Performance Lithium/Sodium-Ion Batteries
- 5 September 2018
- Published by American Chemical Society (ACS) in The Journal of Physical Chemistry C
- Vol. 122 (39) , 22232-22240
Rational Design of Core–Shell-Structured Particles by a One-Step and Template-Free Process for High-Performance Lithium/Sodium-Ion Batteries
- Open Access
- 20 August 2018
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 123 (16) , 8869-8882
Methane Emissions From the Baltimore‐Washington Area Based on Airborne Observations: Comparison to Emissions Inventories
Urban areas are responsible for a substantial fraction of anthropogenic emissions of greenhouse gases (GHGs) including methane (CH4), with the second largest anthropogenic direct radiative forcing relative to carbon dioxide (CO2). Quantification of urban CH4 emissions is important for establishing GHG mitigation policies. Comparison of observation‐based and inventory‐based urban CH4 emissions suggests possible improvements in estimating CH4 source emissions in urban environments. In this study, we quantify CH4 emissions from the Baltimore‐Washington area based on the mass balance aircraft flight experiments conducted in Winters 2015 and 2016. The field measurement‐based mean winter CH4 emission rates from this area were 8.66 ± 4.17 kg/s in 2015 and 9.14 ± 4.49 kg/s in 2016, which are 2.8 times the 2012 average U.S. GHG Inventory‐based emission rate. The observed emission rate is 1.7 times that given in a population‐apportioned state of Maryland inventory. Methane emission rates inferred from carbon monoxide (CO) and CO2 emission inventories and observed CH4/CO and CH4/CO2 enhancement ratios are similar to those from the mass balance approach. The observed ethane‐to‐methane ratios, with a mean value of 3.3% in Winter 2015 and 4.3% in Winter 2016, indicate that the urban natural gas system could be responsible for ~40–60% of total CH4 emissions from this area. Landfills also appear to be a major contributor, providing 25 ± 15% of the total emissions for the region. Our study suggests there are grounds to reexamine the CH4 emissions estimates for the Baltimore‐Washington area and to conduct flights in other seasons.
- 20 August 2018
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 123 (16) , 8869-8882
Open AccessMethane Emissions From the Baltimore‐Washington Area Based on Airborne Observations: Comparison to Emissions Inventories
Urban areas are responsible for a substantial fraction of anthropogenic emissions of greenhouse gases (GHGs) including methane (CH4), with the second largest anthropogenic direct radiative forcing relative to carbon dioxide (CO2). Quantification of urban CH4 emissions is important for establishing GHG mitigation policies. Comparison of observation‐based and inventory‐based urban CH4 emissions suggests possible improvements in estimating CH4 source emissions in urban environments. In this study, we quantify CH4 emissions from the Baltimore‐Washington area based on the mass balance aircraft flight experiments conducted in Winters 2015 and 2016. The field measurement‐based mean winter CH4 emission rates from this area were 8.66 ± 4.17 kg/s in 2015 and 9.14 ± 4.49 kg/s in 2016, which are 2.8 times the 2012 average U.S. GHG Inventory‐based emission rate. The observed emission rate is 1.7 times that given in a population‐apportioned state of Maryland inventory. Methane emission rates inferred from carbon monoxide (CO) and CO2 emission inventories and observed CH4/CO and CH4/CO2 enhancement ratios are similar to those from the mass balance approach. The observed ethane‐to‐methane ratios, with a mean value of 3.3% in Winter 2015 and 4.3% in Winter 2016, indicate that the urban natural gas system could be responsible for ~40–60% of total CH4 emissions from this area. Landfills also appear to be a major contributor, providing 25 ± 15% of the total emissions for the region. Our study suggests there are grounds to reexamine the CH4 emissions estimates for the Baltimore‐Washington area and to conduct flights in other seasons.
- 15 August 2018
- Published by Taylor & Francis in Aerosol Science and Technology
- Vol. 52 (9) , 984-991
Copper–zinc particles with zinc-enriched surfaces generated via spray pyrolysis
Copper is an inexpensive replacement for silver in electronic applications such as solar cell metallization, electromagnetic interference packaging, and printable electronics. However, copper has a characteristically low reduction potential under ambient conditions, favoring formation of non-conducting copper oxides. Here, a spray pyrolysis method of producing oxidation resistant copper particles with surfaces rich in zinc, without need for post-fabrication modifications is described. The effects of precursor and reactor parameters on the particle surface composition with respect to the bulk composition are explored. At reactor temperature conditions of 1000 °C with a precursor containing 90 at% copper–10 at% zinc, the formation of desired morphologies was achieved, smooth dense particles with surfaces enriched in zinc. Increasing the concentration of zinc in the precursor did not improve enrichment, and instead led to the formation of a zinc diamine chloride [Zn(NH3)2Cl2] byproduct. © 2018 American Association for Aerosol Research
- 15 August 2018
- Published by Taylor & Francis in Aerosol Science and Technology
- Vol. 52 (9) , 984-991
Copper–zinc particles with zinc-enriched surfaces generated via spray pyrolysis
Copper is an inexpensive replacement for silver in electronic applications such as solar cell metallization, electromagnetic interference packaging, and printable electronics. However, copper has a characteristically low reduction potential under ambient conditions, favoring formation of non-conducting copper oxides. Here, a spray pyrolysis method of producing oxidation resistant copper particles with surfaces rich in zinc, without need for post-fabrication modifications is described. The effects of precursor and reactor parameters on the particle surface composition with respect to the bulk composition are explored. At reactor temperature conditions of 1000 °C with a precursor containing 90 at% copper–10 at% zinc, the formation of desired morphologies was achieved, smooth dense particles with surfaces enriched in zinc. Increasing the concentration of zinc in the precursor did not improve enrichment, and instead led to the formation of a zinc diamine chloride [Zn(NH3)2Cl2] byproduct. © 2018 American Association for Aerosol Research
- 1 July 2018
- Published by Elsevier in Energy Storage Materials
- Vol. 13, 8-18
Colloidal spray pyrolysis: A new fabrication technology for nanostructured energy storage materials
- 1 July 2018
- Published by Elsevier in Energy Storage Materials
- Vol. 13, 8-18
Colloidal spray pyrolysis: A new fabrication technology for nanostructured energy storage materials
- 25 January 2018
- Published by Tsinghua University Press in Nano Research
- Vol. 11 (8) , 4049-4061
Scalable fabrication of SnO2/eo-GO nanocomposites for the photoreduction of CO2 to CH4
Artificial photosynthesis uses a catalyst to convert CO2 into valuable hydrocarbon products by cleaving the C=O bond. However, this technology is strongly limited by two issues, namely insufficient catalytic efficiency and complicated catalyst-fabrication processes. Herein, we report the development of a novel spray-drying photocatalyst-engineering process that addresses these two issues. Through one-step spray drying, with a residence time of 1.5 s, nanocomposites composed of tin oxide (SnO2) nanoparticles and edge-oxidized graphene oxide (eo-GO) sheets were fabricated without post-treatment. These nanocomposites exhibited 28-fold and five-fold enhancements in photocatalytic efficiency during CO2 reduction compared to SnO2 and commercialized TiO2 (P25), respectively, after irradiation with simulated sunlight for 4 h. This scalable approach, based on short residence times and facile equipment setup, promotes the practical application of artificial photosynthesis through the potential mass production of efficient photocatalysts. Open image in new window
- 25 January 2018
- Published by Tsinghua University Press in Nano Research
- Vol. 11 (8) , 4049-4061
Scalable fabrication of SnO2/eo-GO nanocomposites for the photoreduction of CO2 to CH4
Artificial photosynthesis uses a catalyst to convert CO2 into valuable hydrocarbon products by cleaving the C=O bond. However, this technology is strongly limited by two issues, namely insufficient catalytic efficiency and complicated catalyst-fabrication processes. Herein, we report the development of a novel spray-drying photocatalyst-engineering process that addresses these two issues. Through one-step spray drying, with a residence time of 1.5 s, nanocomposites composed of tin oxide (SnO2) nanoparticles and edge-oxidized graphene oxide (eo-GO) sheets were fabricated without post-treatment. These nanocomposites exhibited 28-fold and five-fold enhancements in photocatalytic efficiency during CO2 reduction compared to SnO2 and commercialized TiO2 (P25), respectively, after irradiation with simulated sunlight for 4 h. This scalable approach, based on short residence times and facile equipment setup, promotes the practical application of artificial photosynthesis through the potential mass production of efficient photocatalysts. Open image in new window
- RetractionOpen Access
- 22 January 2018
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 123 (2) , 1478
Retraction: Methane Emissions From the Marcellus Shale in Southwestern Pennsylvania and Northern West Virginia Based on Airborne Measurements
- 22 January 2018
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 123 (2) , 1478
RetractionOpen AccessRetraction: Methane Emissions From the Marcellus Shale in Southwestern Pennsylvania and Northern West Virginia Based on Airborne Measurements
- Open Access
Infectious virus in exhaled breath of symptomatic seasonal influenza cases from a college community
Little is known about the amount and infectiousness of influenza virus shed into exhaled breath. This contributes to uncertainty about the importance of airborne influenza transmission. We screened 355 symptomatic volunteers with acute respiratory illness and report 142 cases with confirmed influenza infection who provided 218 paired nasopharyngeal (NP) and 30-minute breath samples (coarse >5 μm and fine 4 /30-min fine, 1.2×10 4 /30-min coarse aerosol sample, and 8.2×10 8 per NP swab. Fine and coarse aerosol viral RNA was positively associated with body mass index (fine p<0.05, coarse p<0.10) and number of coughs (fine p<0.001, coarse p<0.01) and negatively associated with increasing days since symptom onset (fine p<0.05 to p<0.01, coarse p<0.10) in adjusted models. Fine aerosol viral RNA was also positively associated with having influenza vaccination for both the current and prior season (p<0.01). NP swab viral RNA was positively associated with upper respiratory symptoms (p<0.01) and negatively associated with age (p<0.01) but was not significantly associated with fine or coarse aerosol viral RNA or their predictors. Sneezing was rare, and sneezing and coughing were not necessary for infectious aerosol generation. Our observations suggest that influenza infection in the upper and lower airways are compartmentalized and independent. Significance: Lack of human data on influenza virus aerosol shedding fuels debate over the importance of airborne transmission. We provide overwhelming evidence that humans generate infectious aerosols and quantitative data to improve mathematical models of transmission and public health interventions. We show that sneezing is rare and not important for, and that coughing is not required for influenza virus aerosolization. Our findings, that upper and lower airway infection are independent and that fine particle exhaled aerosols reflect infection in the lung, open a new pathway for understanding the human biology of influenza infection and transmission. Our observation of an association between repeated vaccination and increased viral aerosol generation demonstrated the power of our method, but needs confirmation.
Open AccessInfectious virus in exhaled breath of symptomatic seasonal influenza cases from a college community
Little is known about the amount and infectiousness of influenza virus shed into exhaled breath. This contributes to uncertainty about the importance of airborne influenza transmission. We screened 355 symptomatic volunteers with acute respiratory illness and report 142 cases with confirmed influenza infection who provided 218 paired nasopharyngeal (NP) and 30-minute breath samples (coarse >5 μm and fine 4 /30-min fine, 1.2×10 4 /30-min coarse aerosol sample, and 8.2×10 8 per NP swab. Fine and coarse aerosol viral RNA was positively associated with body mass index (fine p<0.05, coarse p<0.10) and number of coughs (fine p<0.001, coarse p<0.01) and negatively associated with increasing days since symptom onset (fine p<0.05 to p<0.01, coarse p<0.10) in adjusted models. Fine aerosol viral RNA was also positively associated with having influenza vaccination for both the current and prior season (p<0.01). NP swab viral RNA was positively associated with upper respiratory symptoms (p<0.01) and negatively associated with age (p<0.01) but was not significantly associated with fine or coarse aerosol viral RNA or their predictors. Sneezing was rare, and sneezing and coughing were not necessary for infectious aerosol generation. Our observations suggest that influenza infection in the upper and lower airways are compartmentalized and independent. Significance: Lack of human data on influenza virus aerosol shedding fuels debate over the importance of airborne transmission. We provide overwhelming evidence that humans generate infectious aerosols and quantitative data to improve mathematical models of transmission and public health interventions. We show that sneezing is rare and not important for, and that coughing is not required for influenza virus aerosolization. Our findings, that upper and lower airway infection are independent and that fine particle exhaled aerosols reflect infection in the lung, open a new pathway for understanding the human biology of influenza infection and transmission. Our observation of an association between repeated vaccination and increased viral aerosol generation demonstrated the power of our method, but needs confirmation.
- 27 September 2017
- Published by American Chemical Society (ACS) in ACS Applied Materials & Interfaces
- Vol. 9 (40) , 34587-34591
Conductive One- and Two-Dimensional Structures Fabricated Using Oxidation-Resistant Cu–Sn Particles
Cu-Sn powders are promising alternatives to Ag and Au in applications including printed electronics because of their low cost and high oxidation-resistance. Further development requires the knowledge of the conductivity of their corresponding one-dimensional and two-dimensional structures. Herein, CuSny (y=atom ratio of Sn/Cu) wires and films were produced by direct printing. In-situ measurements of structural resistivities while varying the temperature from 2 K to 400 K in oxygen-free conditions revealed that CuSn0.1 wires have comparable resistivities to Cu wires. Furthermore, CuSn0.1 films exhibited significantly lower resistivity increase after being heated at 573 K in ambient air, compared with Cu films.
- 27 September 2017
- Published by American Chemical Society (ACS) in ACS Applied Materials & Interfaces
- Vol. 9 (40) , 34587-34591
Conductive One- and Two-Dimensional Structures Fabricated Using Oxidation-Resistant Cu–Sn Particles
Cu-Sn powders are promising alternatives to Ag and Au in applications including printed electronics because of their low cost and high oxidation-resistance. Further development requires the knowledge of the conductivity of their corresponding one-dimensional and two-dimensional structures. Herein, CuSny (y=atom ratio of Sn/Cu) wires and films were produced by direct printing. In-situ measurements of structural resistivities while varying the temperature from 2 K to 400 K in oxygen-free conditions revealed that CuSn0.1 wires have comparable resistivities to Cu wires. Furthermore, CuSn0.1 films exhibited significantly lower resistivity increase after being heated at 573 K in ambient air, compared with Cu films.