Controlled coal burning and heat collecting method and apparatus

1988 ◽  
Vol 14 (3) ◽  
pp. II-III
Keyword(s):  
Coal Burning

scholarly journals Quantifying primary and secondary humic-like substances in urban aerosol based on emission source characterization and a source-oriented air quality model

2018 ◽  
Author(s):  
Xinghua Li ◽  
Junzan Han ◽  
Philip K. Hopke ◽  
Jingnan Hu ◽  
Qi Shu ◽  
...  
Keyword(s):  
Organic Carbon ◽  
Biomass Burning ◽  
Coal Combustion ◽  
Power Plants ◽  
Water Soluble ◽  
Aerosol Formation ◽  
Source Characterization ◽  
Air Quality Model ◽  
Coal Burning ◽  
Residential Coal

Abstract. Humic-like substances (HULIS) are a mixture of high molecular weight, water-soluble organic compounds that are widely distributed in atmospheric aerosol. Their sources are rarely studied quantitatively. Biomass burning is generally accepted as a major primary source of ambient humic-like substances (HULIS) with additional secondary material formed in the atmosphere. However, the present study provides direct evidence that residential coal burning is also a significant source of ambient HULIS, especially in the heating season in northern China based on source measurements, ambient sampling and analysis, and apportionment with source-oriented CMAQ modeling. Emissions tests show that residential coal combustion produces 5 to 24 % of the emitted organic carbon (OC) as HULIS carbon (HULISc). Estimation of primary emissions of HULIS in Beijing indicated that residential biofuel and coal burning contribute about 70 % and 25 % of annual primary HULIS, respectively. Vehicle exhaust, industry, and power plants contributions are negligible. Average concentration of ambient HULIS was 7.5 μg/m3 in atmospheric PM2.5 in urban Beijing and HULIS exhibited obvious seasonal variations with the highest concentrations in winter. HULISc account for 7.2 % of PM2.5 mass, 24.5 % of OC, and 59.5 % of water-soluble organic carbon, respectively. HULIS are found to correlate well with K+, Cl−, sulfate, and secondary organic aerosol suggesting its sources include biomass burning, coal combustion and secondary aerosol formation. Source apportionment based on CMAQ modeling shows residential biofuel and coal burning, secondary formation are important annual sources of ambient HULIS, contributing 57.5 %, 12.3 %, and 25.8 %, respectively.

scholarly journals Technological exchanged natural radioactivity in vicinity of the Coal Burning Power Plant Kakanj, BiH

2009 ◽  
Vol 44 (5) ◽  
pp. 759-764
Author(s):  
D. Samek ◽  
L. Saracevic ◽  
N. Gradascevic ◽  
A. Mihalj
Keyword(s):  
Power Plant ◽  
Natural Radioactivity ◽  
Coal Burning

scholarly journals Emission of PM2.5-Bound Polycyclic Aromatic Hydrocarbons from Biomass and Coal Combustion in China

Atmosphere ◽  
2021 ◽  
Vol 12 (9) ◽  
pp. 1129
Author(s):  
Xinghua Li ◽  
Zihao Wang ◽  
Tailun Guo
Keyword(s):  
Polycyclic Aromatic Hydrocarbons ◽  
Mass Balance ◽  
Aromatic Hydrocarbons ◽  
Coal Combustion ◽  
Emission Factors ◽  
Chemical Mass Balance ◽  
Open Burning ◽  
Coal Burning ◽  
Receptor Modelling ◽  
Polycyclic Aromatic

Field measured PAH emissions from diverse sources in China are limited or even not available. In this study, the PM2.5-bound PAH emission factors (EFs) for typical biomass and coal combustion in China were determined on-site. The measured total PAH EFs were 24.5 mg/kg for household coal burning, 10.5–13.9 mg/kg for household biofuel burning, 8.1–8.6 mg/kg for biomass open burning, and 0.021–0.31 mg/kg for coal-fired boilers, respectively. These EF values were compared with previous studies. The sources profiles of PAHs for four sources were developed to use in chemical mass balance receptor modelling. BaP equivalent EFs (EFBaPeq) were calculated to evaluate PAH emission toxicity among different combustion sources, and were 6.81, 2.94–4.22, 1.59–3.62, and 0.0006–0.042 mg/kg for those four types of sources, respectively.

scholarly journals Historical black carbon deposition in the Canadian High Arctic: a <i>></i>250-year long ice-core record from Devon Island

2018 ◽  
Vol 18 (16) ◽  
pp. 12345-12361 ◽  
Author(s):  
Christian M. Zdanowicz ◽  
Bernadette C. Proemse ◽  
Ross Edwards ◽  
Wang Feiteng ◽  
Chad M. Hogan ◽  
...  
Keyword(s):  
Black Carbon ◽  
20Th Century ◽  
Ice Core ◽  
Detection Sensitivity ◽  
Anthropogenic Sources ◽  
The Arctic ◽  
Coal Burning ◽  
Ice Cap ◽  
Devon Ice Cap ◽  
Ice Core Record

Abstract. Black carbon aerosol (BC), which is emitted from natural and anthropogenic sources (e.g., wildfires, coal burning), can contribute to magnify climate warming at high latitudes by darkening snow- and ice-covered surfaces, and subsequently lowering their albedo. Therefore, modeling the atmospheric transport and deposition of BC to the Arctic is important, and historical archives of BC accumulation in polar ice can help to validate such modeling efforts. Here we present a > 250-year ice-core record of refractory BC (rBC) deposition on Devon ice cap, Canada, spanning the years from 1735 to 1992. This is the first such record ever developed from the Canadian Arctic. The estimated mean deposition flux of rBC on Devon ice cap for 1963–1990 is 0.2 mg m−2 a−1, which is at the low end of estimates from Greenland ice cores obtained using the same analytical method ( ∼ 0.1–4 mg m−2 a−1). The Devon ice cap rBC record also differs from the Greenland records in that it shows only a modest increase in rBC deposition during the 20th century. In the Greenland records a pronounced rise in rBC is observed from the 1880s to the 1910s, which is largely attributed to midlatitude coal burning emissions. The deposition of contaminants such as sulfate and lead increased on Devon ice cap in the 20th century but no concomitant rise in rBC is recorded in the ice. Part of the difference with Greenland could be due to local factors such as melt–freeze cycles on Devon ice cap that may limit the detection sensitivity of rBC analyses in melt-impacted core samples, and wind scouring of winter snow at the coring site. Air back-trajectory analyses also suggest that Devon ice cap receives BC from more distant North American and Eurasian sources than Greenland, and aerosol mixing and removal during long-range transport over the Arctic Ocean likely masks some of the specific BC source–receptor relationships. Findings from this study suggest that there could be a large variability in BC aerosol deposition across the Arctic region arising from different transport patterns. This variability needs to be accounted for when estimating the large-scale albedo lowering effect of BC deposition on Arctic snow/ice.

scholarly journals Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community

2018 ◽  
Vol 8 (1) ◽  
Author(s):  
Vitaly V. Kadnikov ◽  
Andrey V. Mardanov ◽  
Denis A. Ivasenko ◽  
Dmitry V. Antsiferov ◽  
Alexey V. Beletsky ◽  
...  
Keyword(s):  
Microbial Community ◽  
Altai Mountains ◽  
Coal Burning ◽  
Lignite Coal
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