ライフサイエンスコーパス: mass balance

1 n of polyfluorinated compounds and check the mass balance.

2 xperiments forced only by changes in surface mass balance.

3 ning to determine their rates of melting and mass balance.

4 ial cycles through their impact on ice-sheet mass balance.

5 ent ion cluster that carries most of the TMT mass balance.

6 tion plays a significant role in the overall mass balance.

7 ure changes in ice sheet dynamics or surface mass balance.

8 de fractions were identified by performing a mass balance.

9 heric oxidants and stratospheric thermal and mass balance.

10 997 (+/-5 years) as a tipping point for GICs mass balance.

11 l as setting sea level through change in ice-mass balance.

12 kinetic experiments suggested an incomplete mass balance.

13 d influence on contemporary ice dynamics and mass balance.

14 ne systems, in a way to be conservative in a mass balance.

15 atographic system is done by the solution of mass balances.

16 maximum steroid concentrations predicted by mass balances.

17 ger than that estimated directly by a (22)Na mass balance (5.13 x 10(16) sites/m(2)), suggesting addi

18 In an attempt to close the mass balance, a systematic evaluation of 3M and fluorote

19 Long-term and large-scale patterns of mass balance achieved through sedimentary processes, rat

20 - and glucose-derived components by isotopic mass balance, allowing quantification of SOM priming ove

21 Mass balance analysis based on multiple sampling events

22 g anaerobic methanogenic sludge and based on mass balance analysis of carbon transformation.

23 Mass balance analysis showed a high percentage of MS2 in

24 Mass balance analysis showed that nitrate produced by An

25 Our mass balance analysis shows that net global carbon uptak

26 The mass-balance analysis recovered urea-C as CO2 at 77%, wh

27 ost (15)N enrichment was coupled by isotopic mass balance and determined that aphid (15)N depletion a

28 he constraints and consequences of elemental mass balance and energy cycling in biological systems to

29 This first mass balance and first United States nationwide wastewat

30 gions, time intervals, and models of surface mass balance and glacial isostatic adjustment to estimat

31 xidation of a range of ethers with excellent mass balance and high turnover numbers under 1 atm of O2

32 The mass balance and hydration results showed that during th

33 ssment Report, new observations of ice-sheet mass balance and improved computer simulations of ice-sh

34 ally determined from a global carbon isotope mass balance and may have varied over geological time, m

35 Here we examine mercury mass balance and mercury stable isotope composition in a

36 approach to study cell metabolism, combining mass balance and proteomic constraints to extend and com

37 The evaluation of mass balance and temperature steady shows that this NH3

38 re system was then evaluated in terms of the mass balance and the energy consumption of each unit.

39 influence the ice sheet's flow dynamics and mass balance and the global sea level, whereas some may

40 No significant differences between the mass balance and the total lead concentration in the sui

41 antitative IR spectroscopic methods to track mass balance and uncover previously unobserved chemistry

42 Finally, mass balances and column dissections revealed that in th

43 Transport experiments, along with mass balances and column dissections, were conducted as

44 hensive analysis of metabolic networks using mass balances and elementary metabolite unit balances.

45 Using mass balances and estimates of P leaching losses, we est

46 Mass balances and quantification of l-cysteine via its s

47 First, a metabolic model (MM) based on mass balancing and mouse liver perfusion data was establ

48 ypical constraints in stoichiometric models: mass balancing and thermodynamics (irreversibility).

49 es in B15 discharge and Antarctica's surface mass balance, and (ii) varies widely depending on the su

50 ed transmission electron microscopy (EFTEM), mass balance, and elemental analysis unambiguously prove

51 hanging winds influences Antarctic ice-sheet mass balance, and hence global sea level, on annual to d

52 he known metabolism of these microorganisms, mass balance, and isotope studies, we hypothesize that D

53 n fluxes affect the long-term carbon isotope mass balance, and may lead to reassessment of the role t

54 gional climatic transitions that affect EAIS mass balance, and, in a global paleoclimatic context, th

55 ing approach agreed well with those from the mass balance approach (1-21% difference), indicating tha

56 ide WM-system, advantages and drawbacks of a mass balance approach are discussed.

57 The results reveal the benefits of a mass balance approach due to redundancy, data consistenc

58 We followed a matrix-based mass balance approach for quantifying exposure from indo

59 Results provide a mass balance approach for tracking ARG fate and insights

60 Under dynamic flow conditions a mass balance approach indicates that even after remobili

61 Using a mass balance approach on eight different flight days in

62 We employed a mass balance approach to estimate the N loss to the envi

63 inties, we used experimental mesocosms and a mass balance approach to estimate the TBA metabolite lea

64 A field study was performed that used a mass balance approach to gain insight into the transport

65 We used a mass balance approach to quantify MeHg production in two

66 (2)H-labeling derivatization strategy and a mass balance approach to quantify phosphorylation.

67 When compared with a chemical mass balance approach using measurement-based source pro

68 mission measurements from the aircraft-based mass balance approach were a factor of 3.2-5.8 greater t

69 nce in the field were compared: the chemical mass balance approach, and a novel chemical benchmarking

70 Compared to the mass balance approach, the benchmarking approach partial

71 monitoring data in the Allegheny River and a mass-balance approach to elucidate bromide contributions

72 ned pasture in lowland Costa Rica, we used a mass-balance approach to quantify N accumulation in vege

73 Significant positive glacier mass balances are noted along the edge of the Upper Tari

74 of catchment export and wetland input-output mass balances are reported for inorganic Hg (Hg(inorg)),

75 Mass balance arguments require that the other half of th

76 nt (16 +/- 3 to 1216 +/- 42 mg kg(-1)) using mass balance assessment as a quality control tool.

77 th the expected Ra/Ba ratios calculated from mass balance assuming a complete recrystallization.

78 tudied without any phase separation steps or mass balance assumptions.

79 Accounting for all TPs detected, a total mass balance at two concentration levels in batch reacto

80 was only detectable using nitrogen isotopic mass balances at two of six stations, and rates ranged f

81 athway models while phenolic production fits mass-balance based allocation models (such as the CNBH).

82 esource being invested in increased defense (mass-balance based allocation).

83 Zealand, were used to constrain the Cd soil mass balance between 1959 and 2015 AD, informing future

84 teady-state model and find that the isotopic mass balance between nitrate and nitrogen fixation impli

85 tructure for soil, for example, attempting a mass balance between soil erosion and production, which

86 Comparison of PFAA mass balances between the two catchments further suggest

87 results of the analysis were validated using mass balance by comparing the sum of extracted As with t

88 for the blood samples was demonstrated using mass balance by comparing the sum of the concentrations

89 The characterization consisted of a mass balance by dissolved organic carbon (DOC), volatile

90 Mass balance calculation identified dexamethasone, spiro

91 A mass balance calculation using the water chemistry data

92 Mass balance calculations demonstrated the high carbohyd

93 Mass balance calculations require that the missing DIC i

94 ydrogeology, chemistry, stable isotopes, and mass balance calculations to evaluate groundwater NO3(-)

95 According to mass balance calculations, the pups are exposed to consi

96 , long term grassland experiments and simple mass balance calculations.

97 Mass-balance calculations indicate soil weathering has d

98 Mass-balance calculations using the (222)Rn data gave a

99 g to quantify microbial mineralization using mass-balance calculations.

100 Ethene mass balance can be used as a direct indicator to assess

101 Herein we demonstrate that chemical mass balancing can successfully isolate, differentiate,

102 According to mass balance, cation loss represents >30% of the base-ca

103 e solar radiation as a significant driver of mass balance changes in high-latitude mountain systems,

104 effects account for a sizeable proportion of mass-balance changes observed in modern ice sheets.

105 The nitrogen mass-balance clearly demonstrates that the total amount

106 positional analysis of algae and process and mass balance closure, emphasis should be placed on unamb

107 The source-receptor model Chemical Mass Balance (CMB) generally used for air pollution stud

108 er and gases is developed using the chemical mass balance (CMB) method and the U.S. EPA's National Em

109 er and gases is developed using the chemical mass balance (CMB) method and the U.S. EPA's National Em

110 Arkansas is examined by a weighted chemical mass balance (CMB) model and positive matrix factorizati

111 es new source profiles for use in a chemical mass balance (CMB) SA of fine particulate matter (PM2.5)

112 ncluding levoglucosan, for use in a chemical mass balance (CMB) source apportionment model.

113 total SOA mass, a significant improvement in mass balance compared to previous studies.

114 Here we estimate the mass balance components for all ice shelves in Antarctic

115 otal aerosol composition, as calculated from mass balance, confirms that fs-LA produces a stoichiomet

116 tral America margin while at other locations mass balance considerations and N contents of high press

117 sed on spatial, chemical, oceanographic, and mass balance considerations, we calculate that this cont

118 eries from an eastern Amazonian forest, with mass balance constraints from an ecosystem carbon cycle

119 The overall mass balance could be closed by including several degrad

120 The terbutryn mass balance could be closed over the entire study perio

121 , all identified TPs were quantified and the mass balance could be closed without having authentic st

122 No complete mass balance could be obtained for these surfaces.

123 Both soil N distribution and mass balance data suggested higher leaching risk from ch

124 tential environmental persistences, and full mass balance data were collated.

125 k at a site by distinguishing between actual mass balance deficits during reductive dechlorination an

126 rding to a series of patient-specific iodine mass-balance differential equations, the solutions to wh

127 ed progressively less influence on ice sheet mass balance during the retreat of the Laurentide Ice Sh

128 Mass balance, epimerization, and aqueous-phase degradati

129 The model solves simultaneous mass balance equations (MBE) using simple matrix algebra

130 wind, finite volume scheme to the hyperbolic mass balance equations and a finite element scheme with

131 five compartments and is governed by kinetic mass balance equations with Michaelis-Menten type expres

132 amics for major substrates were described by mass balance equations.

133 about 30 per cent smaller than the previous mass balance estimate that most closely matches our stud

134 Most previous global mass balance estimates for GICs rely on extrapolation of

135 tudy provide baseline data for ocean plastic mass balance exercises, and assist in prioritizing futur

136 uoyant ocean plastic vertical mixing models, mass balance exercises, impact assessments and mitigatio

137 n-wide CH4 emissions estimated from regional mass balance flights during the campaign.

138 flowing ice with those expected from surface mass-balance fluctuations.

139 Constraint-based modeling uses mass balances, flux capacity, and reaction directionalit

140 Sorbent stability and a closed mass balance for both H(2)O and CO(2) are demonstrated f

141 We calculated SO4(2-) mass balances for 27 forested, unglaciated watersheds fr

142 have solidified the concept that deficits in mass balances for chloroethene fate in sulfate reducing

143 ersistent metabolites were formed, while the mass balances for octylisothiazolinone could not be clos

144 The mass balance found for gadolinium implies the occurrence

145 large enough to affect interpretation of its mass balance from altimetry.

146 les, sand crystals, stable isotopic data and mass balance geochemistry.

147 alkyl groups which are also employed for the mass balance group via N-alkylation, reducing the cost a

148 We evaluated 1936 chemicals using far-field mass balance human exposure models (USEtox and RAIDAR) a

149 Results show that subtle changes in mass balance impart major changes in the concentration o

150 The Karakoram showed a near-stable mass balance in its western part (-0.020 +/- 0.064 m w.e

151 The mass balance in the batch experiments was closed, as mea

152 Cenozoic isotopic records with the need for mass balance in the long-term carbon cycle has been a ma

153 Bromide measurements and mass balances in the catchments of major Swiss rivers re

154 standing problems with chemical and isotopic mass balances in the ocean.

155 Analysis of Deltam sheds light on the mass balance (in addition to the charge and energy balan

156 Overall, the mass balances indicate that a considerable portion of th

157 As mass balances indicated that users filtered less than re

158 Mass balances indicated that, under nonflood conditions,

159 surface mass balance models we partition the mass balance into a term for surface mass balance (that

160 Here we show that the carbon isotope mass balance is also significantly affected by tectonic

161 t ethene are not well characterized and poor mass balance may reflect biotransformation of ethene rat

162 tes for GICs rely on extrapolation of sparse mass balance measurements representing only a small frac

163 ectrometry and ultrafiltration and performed mass balance measurements to study the distribution of A

164 inty in top-down estimates by using repeated mass balance measurements, as well as ethane as a finger

165 A mass balance method and a radiotracer, (32)P (as H3PO4),

166 ates for the whole city based on an aircraft mass balance method and from inverse modeling of CH4 tow

167 A mass balance method is described for determining the mas

168 , GA) PM2.5 was performed using the chemical mass balance method with ensemble-averaged source impact

169 days of measurements and the aircraft-based mass balance method, we calculate an average CH4 flux of

170 The use of mass balance methodology was key to their discovery.

171 "West") 35 x 35 km grids, two aircraft-based mass balance methods measured emissions repeatedly at fi

172 We used a state-space oxygen mass balance model and continuous dissolved oxygen measu

173 o this end, we consider a minimal stochastic mass balance model and identify a parsimonious mechanism

174 oids were determined using a two-compartment mass balance model and parameters determined in experime

175 ly predictable fate properties and a generic mass balance model for activated sludge treatment to com

176 Using a mass balance model for lithium inputs and outputs from t

177 Here we present a carbon and sulfur isotope mass balance model for the latest Cambrian time interval

178 , uptake, and bioaccumulation into an indoor mass balance model provides a quantitative framework lin

179 These observations and isotope mass balance model results imply that large variations i

180 on of in vitro toxicity data, we developed a mass balance model that can be parametrized and applied

181 tabase of sedimentary metal enrichments to a mass balance model that includes spatially variant metal

182 We validated the use of the mass balance model to determine the effectiveness of por

183 Here we derive a mass balance model to quantify the extent of Fe atom exc

184 Subsequently, a recently proposed mass balance model was applied to calculate the specific

185 A one-compartment pharmacokinetic (1-CoPK) mass balance model was developed to estimate organic che

186 Through a mass balance model we show that Mg uptake into the funga

187 dynamic diameter (PM2.5) based on a chemical mass balance model, criteria air pollutants from governm

188 Using a mass balance model, we estimate that this isotopic shift

189 itzerland, and interpreted with a multimedia mass balance model.

190 A chemical mass-balance model estimated that delayed petcoke was th

191 ticular, we used a spatially explicit simple mass-balance model forced with idealized sinusoidal load

192 e emission inventory and a global multimedia mass-balance model generally agree well with reported fi

193 A mass-balance model indicated that the flowing solution w

194 We use a global multimedia mass-balance model to calculate the Globally Balanced St

195 Finally, we derived a simple mass-balance model to estimate fish abundance from eDNA

196 A fugacity-based indoor mass-balance model was used to simulate the fate and tra

197 , which we show theoretically using a simple mass-balance model.

198 in solution are determined precisely using a mass-balance model.

199 cleaning processes using an indoor-particle mass-balance model.

200 Furthermore, isotope mass balance modeling revealed that Cd removal processes

201 carbon and noble-gas measurements with reach mass-balance modeling to estimate thermogenic methane co

202 argeted analytical approaches and multimedia mass-balance modeling, compounds of particular relevance

203 tic fate and transport models and multimedia mass balance models can be used for the exposure predict

204 Furthermore, using two surface mass balance models we partition the mass balance into a

205 Using both starvation experiments and mass balance models, it was found that excretion of C, N

206 This is because, in standard isotope mass balance models, there are more variables than const

207 When applied to mass balance models, these results support previous inte

208 Three trophic mass-balance models representing coral reef ecosystems a

209 Multimedia mass-balance models require fewer input parameters to ca

210 /- 144 gigatonnes per year and a total basal mass balance of -1,454 +/- 174 gigatonnes per year.

211 zation mass spectrometry (GC/VUV-MS), with a mass balance of 68 +/- 22%.

212 ing the biomass weight and ensuring complete mass balance of a model.

213 Mass balance of As chemical fractionation showed that ~8

214 A mass balance of benthic solute fluxes and the correspond

215 were in excellent agreement, providing 100% mass balance of detected analyte.

216 glacial isostatic adjustment to estimate the mass balance of Earth's polar ice sheets.

217 min) minimizes interference with the natural mass balance of gases in environmental systems, and allo

218 Volcanic eruptions can impact the mass balance of ice sheets through changes in climate an

219 ts, electrochemical measurements supported a mass balance of lead release demonstrating that a greate

220 In three WWTPs, the total mass balance of LMG-N2-G ranged from 71 to 102%.

221 Here we argue that the Earth's mass balance of moderately volatile elements is inconsis

222 d region of FAK, was employed to monitor the mass balance of post-translational modifications (PTMs)

223 The mass balance of pyrite oxidation and nitrate reduction r

224 Dechlorination pathways were confirmed by mass balance of substrates and products.

225 s sulfur bacteria have failed to demonstrate mass balance of sulfur, indicating that unidentified oxi

226 Ice shelves play a key role in the mass balance of the Antarctic ice sheets by buttressing

227 cal prerequisite when modeling the long-term mass balance of the EAIS during past warm climates and i

228 entrations high enough to satisfy the (40)Ar mass balance of the Earth can be preserved in the lower

229 Mass balance of the global hydrogen budget constrains th

230 These events are likely to alter the surface mass balance of the ice sheet, leaving the surface susce

231 A mass balance of the Oder River watershed was assembled t

232 Recovery mass balances of 115 +/- 18% and 60 +/- 30% of the Ce we

233 Based on stable isotopic mass balances of CH4 , inputs and outputs to the water c

234 s satisfying constraints on the steady-state mass balances of intermediates) has been developed using

235 servative estimates of accumulating negative mass balances of magnitude -15 m water equivalent by 190

236 Mass balances of ten individual perfluorinated alkyl aci

237 In addition, mass balances of terbutryn and octylisothiazolinone were

238 forts are seeking to understand the heat and mass balances of the equatorial Pacific, and possible ch

239 Here, we model the Cook Ice Cap mass balance on the Kerguelen Islands (Southern Indian O

240 hrough curves, solvent extraction of BAC and mass balance on the reactor provided consistent results

241 use of dual-tracer stable isotope, although mass balance or other isotope methods are still used occ

242 tively used in photochemical models that use mass balance oxygen atom transfer mechanisms to infer at

243 lated copper life cycle in terms of a closed mass balance, particularly the matching of recycled meta

244 n ((15)N, (13)C) across the reporter and the mass balancing parts of the reagents.

245 have become more globally significant from a mass-balance perspective.

246 chanistic air exchange rate (AER) model to a mass-balance PM2.5 infiltration model to predict residen

247 olved differential equations on the basis of mass balance principles.

248 Through the use of a novel mass balancing procedure, SRF quality is understood, thu

249 Here we use a novel, 1 km surface mass balance product, evaluated against in situ and remo

250 study revisits and updates the Lake Michigan Mass Balance Project (LMMBP) for polychlorinated bipheny

251 ion estimates agreed well with concentration mass balances, providing a proof-of-principle validation

252 A radiocarbon mass balance quantified a predominantly natural petrogen

253 Mass balances range from 72 to 95%.

254 The mass balances ranged from 49 to 130% of the parent compo

255 To accomplish this, a nitrogen mass-balance regression (NMBR) model was developed and a

256 Here, we combine atmospheric mass balance, remote sensing-modeled datasets of vegetat

257 Conversely, Chemical Mass Balance results are sensitive to the source profile

258 udy is the first to show consistency between mass balance results on so many different days and in tw

259 The aircraft-based mass balance results revealed comparable variability.

260 bioreactors, inorganic carbon stable isotope mass balances results indicated that AOM accounted for b

261 le based on PGEs and ambient quantification, mass balancing revealed that approximately half the fine

262 ansport over the Tibetan Plateau for glacier mass balance, river runoff and local ecology, changes in

263 Mass balances show that ~4% of the initial carbonate was

264 The resulting mass balance showed a mismatch of >50% for 23 metals, wh

265 A mass balance showed insignificant removal of imidaclopri

266 Mass balance shows that a modest volume of brine, most l

267 Climate and snowpack mass-balance simulations show evidence for enhanced ice

268 e attribute 77% of the increasingly negative mass balance since the 1960s to atmospheric drying assoc

269 012, partitioned into changes due to surface mass balance (SMB) and ice dynamics.

270 However, a recent input-output mass balance study during 2007-2010 revealed a black ald

271 ere we present a comprehensive Hg-deposition mass-balance study, and show that most of the Hg (about

272 Second, best estimates of mass balance suggest decreasing net deposition of SS and

273 Results of mass balance suggest growth of bacterial hosts containin

274 Fluvial mass balances suggest strong in-lake retention of partic

275 en, using a natural abundance stable isotope mass balance technique.

276 and three refineries using an aircraft-based mass balance technique.

277 We also reveal that the surface mass balance term shows a considerable decrease since 20

278 eductive dechlorination and apparent lack of mass balance that is related to biotransformation of eth

279 ogen input (NANI) approach is a simple quasi-mass-balance that estimates the human-induced nitrogen i

280 ion the mass balance into a term for surface mass balance (that is, total precipitation minus total s

281 core, adding the years with negative glacier mass balance, that is, years with melting and subsequent

282 ly quantified the calving flux and the basal mass balance (the balance between accretion and ablation

283 In a multiple-exposure temporal mass balance, three major metabolites accounted for >60%

284 Here, we used a (228)Ra mass balance to demonstrate that the total SGD contribut

285 evaporation, and sea level data in an ocean mass balance to estimate freshwater discharge into the g

286 First of all, ICP-MS allowed mass balances to be carried out (all along the sample pr

287 This study used mass balances to compare wastewater treatment plant (WWT

288 ea level change that explicitly accounts for mass balance uncertainty over an entire ice sheet.

289 utes a minor component of the carbon isotope mass balance under the modern, high levels of atmospheri

290 ived meltwater influenced East Antarctic ice mass balance under warmer-than-present climate condition

291 otal fluorine after extraction indicate that mass balance was achieved (within analytical error) of t

292 A mass balance was assembled for perfluorohexanoic acid (P

293 ase of VX was measured and almost a complete mass balance was obtained, which characterizes the behav

294 In all cases, mass balance was verified by carrying out the total dige

295 s determined using a two end-member isotopic mass balance were between 1.6 and 9.3 mg/L lower than to

296 High mass balances were observed under aerobic or anaerobic c

297 These new insights into the energy and mass balance will inform design of more ethanol-tolerant

298 r univariate models, the PLS models achieved mass balance with better accuracy.

299 from Lakes, FENL) is based on a steady-state mass balance with loading, output, loss/retention, and N

300 Simulations of glacier mass balances with radiative forcing-equivalent changes