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Record W2392546987

Study on mercury emission during underground coal gasification of lignite

2004· article· en· W2392546987 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueActa Scientiae Circumstantiae · 2004
Typearticle
Languageen
FieldEngineering
TopicMining and Gasification Technologies
Canadian institutionsnot available
Fundersnot available
KeywordsMercury (programming language)ChemistryUnderground coal gasificationEnvironmental chemistryCoalSulfideWaste managementMineralogyCoal mining
DOInot available

Abstract

fetched live from OpenAlex

underground coal gasification (UCG) is a process in which underground coal, without mining and transportation, is directly converted into combustible gas. The regularity of mercury emission during UCG of lignite was studied with aims of prevention and control of mercury emission released from UCG. Mercury form in lignite is analyzed by sequential chemical extraction. It was found that the average mercury content of the test lignite is 0.3986?μg·g~(-1) and mercury in lignite mainly occurs in bound-sulfide and residue, taking up 77.8% and 19.1%, respectively. Based on UCG simulation test of lignite, the change of mercury content in UCG gas varying with time and temperature and the influence of gasification technology were investigated. Elemental mercury, Hg~0(g), and divalent mercury, Hg~(2+)(g), in UCG gas was captured by Ontario Hydro Method (recommended by EPA in USA) and detected by atomic fluorescence spectrometer. In addition, the mechanism of mercury transformation and emission during UCG process was analyzed. Mercury exists mainly in the form of Hg~0(g) in UCG gas. Small amount of Hg~(2+)(g) is produced through chemical reaction of Hg~0(g) and the product gas in the gasification tunnel, and it easily decomposes into Hg~0(g) when the temperature is above 700K. The content of mercury in UCG gas changes with gasification time. At the initial stage of UCG, the content of Hg~0(g) is lower and Hg~(2+)(g) can not be detected. The content of both Hg~0(g) and Hg~(2+)(g) increases in the stable gasification process and decreases at the end of UCG due to different amounts of gasified coal in the different periods of UCG. The average content of Hg~0(g) is 50~60μg·m~(-3) and that of Hg~(2+)(g) is 0.30~0.35?μg·m~(-3). The highest content of Hg~0(g) is found to be 160 times as much as that of Hg~(2+)(g). Changes of Hg~0(g) and Hg~(2+)(g) content in UCG gas with temperature of gasification zone was obtained based on the results of temperature field. The content of Hg~0(g) and Hg~(2+)(g) increases with elevated temperature of gasification zone. The content of Hg~0(g) reaches saturation when the temperature is higher than 600K, similar to the results of surface gasification. Gaseous mercury contents in UCG gas under different technologies were compared. It indicates that UCG gas contains more Hg~(2+)(g) under oxygen gasification and less Hg~(2+)(g) under oxygen-steam gasification since steam slows down the oxidation tendency of Hg~0(g) to Hg~(2+)(g). Analysis of mercury balance in UCG process shows that gaseous mercury takes up less than 20% of the total mercury in UCG products, lower than that from surface gasification and coal burning, and solid mercury takes up more than 60%. Since mercury content in UCG ash is lower, the majority of solid mercury is particulate mercury absorbed by char and ash when UCG gas flows through the long air stream tunnel. UCG gas from simulation test contains higher percentage of Hg~0(g) than that from field test, since the tunnel length is shorter in simulation gasification.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.181
Threshold uncertainty score0.753

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.024
GPT teacher head0.251
Teacher spread0.227 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it