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1 ger characterisitic thermal constants, theta(char).
2 amounts of thermally altered organic matter (chars).
3 nd donate up to 2 mmol electrons per gram of char.
4 are considered by critical appraisal of one, char.
5 um, whereas 8% of the right atrium burns had char.
6 uced by cold-weather species, such as Arctic char.
7 ven assuming high long-term stability of the char.
8 ined progressively with carbonization of the char.
9 icient) to sorption on graphite, but less on chars.
10 ace burns was more homogeneous than open air chars.
11 d for efficient utilisation of waste derived chars.
12 monstration of CH(4) suppression by wildfire chars.
13 possibly condensed aromatics in the high-HTT chars.
14 iscrete, continuous, and without evidence of charring.
15 selenoneine concentrations comprised Arctic char (1.07 [1.02, 1.12]) and beluga mattaaq (1.15 [1.08,
16 ergothioneine concentrations included Arctic char (1.07 [1.04, 1.10]) and caribou meat (1.06 [1.03, 1
18 ric tetrylene dichalcogenolates of formula M(ChAr)2 (M = Si, Ge, Sn, Pb; Ch = O, S, or Se; Ar = bulky
19 verted recalcitrant heavy hydrocarbons into "char" (a carbonaceous material similar to petroleum coke
20 The mechanism of the graphitization of bio-char, a "non-graphitizable" carbon, is explored, suggest
21 sion of biogenic methane (CH(4)) by wildfire chars, a previously unrecognized, potentially beneficial
22 ith char is also needed to determine whether char accumulation has long-term redox effects on microbi
25 n Atlantic salmon, rainbow trout, and Arctic char also revealed extensive conservation of syntenic bl
26 ta) values for pyDOM generated from wildfire char and a series of lab-prepared chars produced by comb
27 atmospheric black carbon (BC, in the form of char and soot) is still constrained for inland areas.
28 hern India on emission factors of OC and EC (char and soot) was assessed for four cookstoves (advance
29 Variation in terms of EFs for OC and EC (char and soot) within the cooking cycle was also found t
30 ic (OC) and black carbon (BC, in the form of char and soot), have long been recognized in modern wild
32 lated to the different formation pathways of char and soot, which are governed by combustion efficien
34 en isolates collected from table beet, Swiss chard and common lambsquarters in mixed-cropping farms a
35 ranslocation, and accumulation of nitrate in chard and spinach under greenhouse conditions with optim
36 opulations of C. beticola derived from Swiss chard and table beet were not genetically differentiated
37 analyses of the stomach and liver, including charred and bloody tissues after electrocauterization.
38 n North Africa, archaeobotanical evidence of charred and desiccated plant organs denotes that Early H
40 ound to be similar in energy content to wood chars and bituminous coal, having a heating value of 25.
41 rom pecan shell biochar, a model for natural chars and human-made chars used in soil remediation and
43 d FTS compounds in water, sediment, juvenile char, and benthic invertebrates from lakes in the high A
45 , green lettuce, lamb's lettuce, mizuna, red chard, and red lettuce, were observed under high PAR.
46 d chard, red lettuce, rocket, spinach, Swiss chard, and tatsoi) and quality traits of the selected le
47 grees of internal doneness, surface browning/charring, and cooking technique was linked to a database
48 zole 71 undergoes destructive pyrolysis with charring, and the calculations predict the occurrence of
49 cepting quinone moieties in intermediate-HTT chars, and by electron accepting quinones and possibly c
53 he exocyclic C=C bond of pentafulvenes C5H4(=CHAr) (Ar=2-MeOPh and related species) results in enanti
55 e technologies are not suitable for use with charred archaeobotanicals and urge great caution when in
56 peciation and availability in sludge-derived chars are tunable by varying treatment techniques and co
59 the feasibility of using human feces-derived char as a solid fuel for heating and cooking and a poten
61 rs have been recently described, positioning chars as active participants in microbial redox processe
63 perfluorooctanesulfonate (PFOS) dominated in char, benthic chironomids (their main prey), and sedimen
64 of organic carbon (C) ranging from partially charred biomass and charcoal to soot) is a widely acknow
66 components, and the PyOM (i.e., all visually charred, blackened materials) produced in each of them.
67 commercial charcoal briquettes, making fecal char briquettes a potential substitute that also contrib
68 cted an extensive programme of AMS-dating of charred broomcorn millet grains from 75 prehistoric site
69 ion and the end of testing (e.g., refueling, char burnout) drive high emissions during pellet tests.
70 all solutes maximized with the 500 degrees C char, but failed to trend regularly with N2 or CO2 surfa
71 on in the uncertainty of prediction of theta(char) by a factor or f approximately 2 and, in a constan
72 n-donating, phenolic moieties in the low-HTT chars, by newly formed electron accepting quinone moieti
75 thetic material and as a constituent of bone char, can serve as an effective and relatively inexpensi
76 indings suggest that coral species with high-CHAR capability during bleaching and recovery, irrespect
77 n of microbially utilized chars restored the chars' capacity to suppress CH(4), confirming the redox-
79 undescribed stable isotope determinations of charred cereals and pulses from 13 Neolithic sites acros
81 r, the most favorable result is obtained for char cofiring substituting fossil coal, even assuming hi
84 Assessment of ceramide mass by TLC lipid charring confirmed that PSC 833 markedly enhanced cerami
87 easurements on bones of humans, animals, and charred crops allow the detection of spatio-temporal pat
89 nilateral Meniere's disease were enrolled at Charing Cross Hospital (London, UK) and Leicester Royal
91 84 safely discharged) from two UK hospitals (Charing Cross Hospital, London, and Hammersmith Hospital
92 red between January, 1993, and May, 2008, at Charing Cross Hospital, London, UK, who had persistently
94 id evidence and suggest that most of the 101 charred deposits analysed, from across the major islands
96 systematically characterized P speciation in chars derived from thermal (i.e., pyrolysis) and hydroth
97 limited utility for the characterization of chars due to incomplete solubility in common solvents.
99 Although RDX transformation correlated with char electrical conductivity, no RDX transformation was
100 anic matter content can significantly affect char electrochemical properties and microbial interactio
102 ntal black carbon (fossil fuel soot, biomass char), engineered carbons (biochar, activated carbon), a
103 s the first significant data set of wildfire char ESC, and the first quantitative demonstration of CH
104 On average, 28.4 +/- 2.2% of the wildfire chars' ESC was utilized to divert electrons away from CH
105 effects of thermal air oxidation of biomass chars experienced during formation or production on thei
107 e analysis and lipid residue analysis on the charred food macro-remains, carbonized thin layer organi
108 of anoxically prepared wood and pecan shell chars for up to 40 min enhanced the mass-normalized adso
109 nergy absorbed by snowpacks occurred beneath charred forests over the past two decades, with enhanced
114 No steam pop, myocardial perforation, or char formation was observed in any of the 111 ablations
116 tic investigation of the redox properties of chars formed under different pyrolysis conditions has be
118 e conditions, the microstructure of residual char from fungal fibers grown with higher content of Si
121 ot steel slags, a man-made iron resource via char gasification and the employment of hematite, a natu
122 sts where the apparent activation energy for char gasification got remarkably reduced from 95.7 kJ/mo
124 erived soils in the U.S. (Mollisols) contain char (generated by presettlement fires) that is structur
125 topic analyses of human and animal bones and charred grains; and radiocarbon dating of millet grains
126 ynamic model incorporating solvent-water and char-graphite partition coefficients permitted for the f
127 k earths in Amazonia that were enriched with char >800 years ago) consist predominantly of char resid
133 nt fires) that is structurally comparable to char in the Terra Preta soils and much more abundant tha
135 metabolites were immediately adsorbed by the char, including l-asparagine, l-glutamine, and l-arginin
137 Here, we introduce a formal definition of charring intensity (CI) to more accurately characterize
138 sembled those in bio-oil, but the increasing charring intensity caused a marked reduction in the mole
139 m monitoring of complex systems amended with char is also needed to determine whether char accumulati
143 n, P. ramorum-infected bay laurel amidst the charred landscape may have allowed these trees to serve
144 a decreased thickness and continuity of the char layer and yielded the only specimens with new bone
145 taneous saline irrigation; 2) CO2 laser with char layer intact; 3) CO2 laser with char layer removed;
146 AG laser with air/water surface cooling, and char layer intact; 5) Nd:YAG laser with air/water surfac
147 ustic spectroscopic results suggest that the char layer is limited to an area less than approximately
148 val of the char layer, and Nd:YAG laser with char layer removed and with and without use of an air/wa
150 er with char layer intact; 3) CO2 laser with char layer removed; 4) Nd:YAG laser with air/water surfa
151 AG laser with air/water surface cooling, and char layer removed; and 6) Nd:YAG laser without air/wate
153 r, CO2 laser with and without removal of the char layer, and Nd:YAG laser with char layer removed and
154 arized light and evaluated for presence of a char layer, heat induced cracking, heat related alterati
155 in open leaf structure produce (i.e., kale, chard, lettuce, greens, and spinach) being most likely t
156 esults indicate that: (1) the composition of charred macro-remains represent the final foodstuffs coo
157 initrobenzene from water to a series of wood chars made anaerobically at different heat treatment tem
159 ng value of 25.6 +/- 0.08 MJ/kg, while fecal chars made at 750 degrees C had an energy content of 13.
161 iated electrochemical analysis, we show that chars made from different feedstock and over a range of
165 icating that the addition of pyDOM from wood chars may not strongly impact surface water photochemist
166 ished or ceased around 1050-800 BCE, despite charred millet grains still being found in the archaeolo
167 s (PolyNARA), likely formed through combined charring of plant and animal biomass, abiotic nitrogen i
169 ical conductivity was addressed by producing chars of increasing electrical conductivity via pyrolysi
172 out structural degradation due to shrinkage, charring or decomposition during the sintering of printe
173 nriched carbon stable isotope values of bulk charred organic matter sampled from pottery vessel surfa
175 extremely low pollen production and limited charred-particle deposition, indicating insufficient veg
176 markedly increasing their feeding rates and CHAR (per cent contribution of heterotrophically acquire
179 er reanalysed part of an existing dataset on charred plant material, and found all purported endogeno
181 2023 were collected from across the U.S. All chars possessed sizable ESC, from 0.54 to 2.85 mmol e(-)
183 nalysis of two thermosequences revealed that chars produced at intermediate to high heat treatment te
185 henanthrene and anthracene in grass and wood chars produced in 100 degrees C increments across a temp
187 0% reduction in water uptake and doubling of char production while largely retaining other key proper
188 show that sorption is a complex function of char properties and solute molecular structure, and not
190 spectroscopic analyses of the thermosequence chars provide evidence that the pool of redox-active moi
192 eased at circumneutral pH from a total of 14 chars pyrolyzed from wood and grass feedstocks from 200
193 , green lettuce, lamb's lettuce, mizuna, red chard, red lettuce, rocket, spinach, Swiss chard, and ta
194 ghts the need for a broader understanding of char redox processes to predict and effectively manage u
196 actors that determine whether the effects of char redox properties are enhanced or attenuated in comp
197 sed with increasing pyrolysis temperature of chars, reflecting the increasing degree of condensation
198 har >800 years ago) consist predominantly of char residues composed of ~6 fused aromatic rings substi
199 Our findings indicate that these oxidized char residues represent a particularly stable, abundant,
200 ed at the expense of (13)CH(4), as anaerobic char respirers outcompeted acetoclastic methanogens.
201 tron storage capacity (ESC) that can support char-respiring microbes, enabling them to outcompete met
205 also identify critical knowledge gaps about chars' role in microbial redox processes that are import
206 s have advanced mechanistic understanding of char's behavior and potential effects, translating these
207 l sustainability and postulate that managing char's redox properties, such as electron donating, acce
208 r with measured PCB concentrations in Arctic char (Salvelinus alpinus) and brown trout (Salmo trutta)
209 proved relative condition of resident Arctic char (Salvelinus alpinus) and increased diatom diversity
210 and in brown trout (Salmo trutta) and Arctic char (Salvelinus alpinus) collected in a reference lake
211 y contaminated by a small airport and Arctic char (Salvelinus alpinus) from these lakes had over 100
213 ; brook trout, Salvelinus fontinalis; Arctic char, Salvelinus alpinus; Atlantic salmon, Salmo salar;
216 (MARGI (mapping RNA-genome interactions) and ChAR-seq (chromatin-associated RNA sequencing)), which a
217 we use chromatin-associated RNA sequencing (ChAR-seq) to map the global network of ncRNA interaction
222 e that lipids can be recovered reliably from charred surface deposits adhering to pottery dating from
224 ization of two kindreds (K144 and K145) with Char syndrome containing 22 and 5 affected members, resp
225 ctor expressed in neural crest cells, to the Char syndrome critical region and identified missense mu
226 nes should lead to the identification of the Char syndrome gene, which will provide insights into car
228 entified recombinant events that defined the Char syndrome locus with high probability to a 3.1-cM re
229 acial and limb development and suggests that Char syndrome results from derangement of neural-crest-c
230 en to determine the gene responsible for the Char syndrome, an autosomal dominant disorder characteri
234 d cold-water species like trout, salmon, and char that are already constrained to high elevations and
235 The carbon net negative conversion of bio-char, the low value byproduct of pyrolysis bio-oil produ
236 g the different use options of the pyrolysis char, the most favorable result is obtained for char cof
237 ese processes would inform the production of chars to enhance beneficial processes such as increased
238 salmonids (salmon, marine trout, and Arctic char) to identify opportunities to reduce environmental
242 bioavailability of perchlorate in spinach or chard used in the production of baby foods commodities.
245 eachable organic matter characteristics from chars visually characterized as low burn severity that w
246 yDOM from the highest combustion temperature char was found to possess extremely low Phi(Delta) value
249 ate was moist, relatively high quantities of char were deposited in Linsley Pond, Connecticut, USA wh
250 he root zone of spinach compared to those of chard were correlated with a high rate of accumulation i
251 The higher heating values of the studied chars were evaluated using their elemental composition a
253 cold-water fishes (e.g., salmon, trout, and char) with relatively large body sizes and mobility.
254 otothermal-photocatalytic materials that use charred wood substrates to convert liquid water to water