ライフサイエンスコーパス: dissolved oxygen

1 ironmental influences (i.e., trace water and dissolved oxygen).

2 in natural sunlight, even in the presence of dissolved oxygen.

3 As(III), independent to the availability of dissolved oxygen.

4 ccurs through the inactivation of (3)DOM* by dissolved oxygen.

5 variable availability of organic carbon and dissolved oxygen.

6 ments like streambeds is the distribution of dissolved oxygen.

7 s(III) oxidation reaction in the presence of dissolved oxygen.

8 s heterogeneously oxidized to ferric iron by dissolved oxygen.

9 T) technique is evaluated for measurement of dissolved oxygen.

10 performance was affected by illumination and dissolved oxygen.

11 re, salinity and substrate concentration and dissolved oxygen.

12 ve species in the catalytic redox cycle) and dissolved oxygen.

13 lution conditions such as pH and presence of dissolved oxygen.

14 respiratory activity via the consumption of dissolved oxygen.

15 ow in the presence of greater than 5 micro M dissolved oxygen.

16 , so strict care must be taken to remove all dissolved oxygen.

17 terms of, for example, water temperature and dissolved oxygen.

18 sufficient alkalinity, and a diel rhythm in dissolved oxygen.

19 which then likely deprotonate and react with dissolved oxygen.

20 sed on GOx-glucose enzyme reaction, depletes dissolved oxygen.

21 dTe dissolution rate increased linearly with dissolved oxygen.

22 I) formation and an unexpected production of dissolved oxygen.

23 hardonnay with two initial concentrations of dissolved oxygen (0.5 and 10 mg/L) was stored in differe

24 Differences in dissolved oxygen across ensemble members highlight the p

25 The SECM methodology also demonstrates how dissolved oxygen affects the rate of hydrogen extraction

26 the transport of heat, nutrients, plankton, dissolved oxygen and carbon in the ocean.

27 Vertical profiles of dissolved oxygen and dissolved and solid Mn suggest that

28 Optical sensors for dissolved oxygen and dissolved carbon dioxide are now co

29 Redox agents such as dissolved oxygen and hydrogen peroxide have no effect on

30 minantly anoxic and ferruginous (depleted in dissolved oxygen and iron-bearing), but with a tendency

31 ones (OMZ) of the Pacific and Indian Oceans, dissolved oxygen and N2O concentrations in the Atlantic

32 decomposition and water clarity and elevated dissolved oxygen and net primary productivity.

33 nce of mixing shallow groundwater containing dissolved oxygen and nitrate with deeper, anoxic groundw

34 tively affected abundance and biomass, while dissolved oxygen and potassium positively impacted bioma

35 erference from the irreversible reduction of dissolved oxygen and present methods to circumvent these

36 enosine triphosphate level, concentration of dissolved oxygen and produced CO(2).

37 tive associations between THM occurrence and dissolved oxygen and recharge indicate the recycling of

38 tic crust, which we calculate from modelling dissolved oxygen and strontium pore water gradients in b

39 Significant differences in the effluent dissolved oxygen and sulfate concentrations were noted a

40 Here we analyse a combined total of 45,148 dissolved oxygen and temperature profiles and calculate

41 -dioxane is often hindered by the absence of dissolved oxygen and the co-occurrence of inhibiting chl

42 ission is attributed to the reaction between dissolved oxygen and two different products of TPrAH oxi

43 pelagic carbonate dissolution, a decrease in dissolved oxygen, and a benthic foraminiferal extinction

44 rmed from the hydroxido ligands and not from dissolved oxygen, and ammine ligands are products from t

45 aquatic factors included water temperature, dissolved oxygen, and baseflow.

46 dimentation, and diel fluctuations of pH and dissolved oxygen, and did not differ between native and

47 2) /pH (and other carbonate parameters), and dissolved oxygen, and discuss what is known about behavi

48 Subsurface hydrocarbon composition, dissolved oxygen, and dispersant data are used to assess

49 hetes were exposed to differential levels of dissolved oxygen, and distinct alterations were observed

50 uently observed in samples with high pH, low dissolved oxygen, and low nitrate.

51 had the strongest effect on bacteria, while dissolved oxygen appeared to be a major driver for eukar

52 In AN containing naturally dissolved oxygen (approx. 2 mM), the superoxide radical

53 The role of dissolved oxygen as a principal electron acceptor for mi

54 Under anoxic conditions (absence of dissolved oxygen), As(III) oxidation occurred, but the A

55 d porous media structure requires control of dissolved oxygen, as geospatial variation in the partial

56 A zone of higher dissolved oxygen at the mat surface promotes Fe(III)-oxi

57 and 4-8 hPa (approximately 0.16-0.32 mg/L of dissolved oxygen) at ambient air oxygen concentrations (

58 0.5-2.0 hPa (approximately 0.02-0.08 mg/L of dissolved oxygen) at low oxygen concentrations (<50 hPa)

59 al (temperature) and chemical (conductivity, dissolved oxygen) attributes have become integral to aqu

60 bon dioxide-equivalent (CO(2)-eq) basis, and dissolved oxygen availability rapidly decreased.

61 A large region of low-dissolved-oxygen bottom waters (hypoxia) forms nearly ev

62 ger of the generated nitric oxide is not the dissolved oxygen but rather superoxide anion radical gen

63 n its spatial relationship with bottom-water dissolved oxygen (BWDO) concentration using a geostatist

64 re, pH and seawater carbonate chemistry, and dissolved oxygen, can exceed the changes expected with c

65 to overlying water PCBs, lipid fraction, and dissolved oxygen concentration (regulating gill ventilat

66 rs on performance (Anammox biofilm activity, dissolved oxygen concentration and fraction of solids wa

67 We show that the dissolved oxygen concentration does not appear to affect

68 induced fluctuations in temperature, pH, and dissolved oxygen concentration following the variation i

69 Dissolved oxygen concentration in the wine immediately p

70 e estimated by use of the Microtox assay and dissolved oxygen concentration measurements.

71 thin sediments, equivalent to an increase in dissolved oxygen concentration of 15-20 micromoles per l

72 Low dissolved oxygen concentration of subsurface environment

73 xperimental conditions, such as temperature, dissolved oxygen concentration, and viscosity.

74 the path of both Steps due to the increasing dissolved oxygen concentration.

75 ieve real-time measurements of intracellular dissolved oxygen concentration.

76 h corresponds to a 90% reduction in terms of dissolved oxygen concentration.

77 hase, the rate of which responds linearly to dissolved oxygen concentration.

78 akly controlled by pH, and not controlled by dissolved oxygen concentration.

79 of cold temperatures (<6 degrees C) and low dissolved oxygen concentrations (<1-3 ml l(-1)).

80 t various temperatures (25-70 degrees C) and dissolved oxygen concentrations (0-100% O2 in the gas ph

81 plot (r(2) = 0.999) over the whole range of dissolved oxygen concentrations (0-43 ppm).

82 n pathways in the AlS-IACW system under high dissolved oxygen concentrations (3-6 mg L(-1)) without s

83 environmental conditions and can survive low dissolved oxygen concentrations and high water temperatu

84 Dissolved oxygen concentrations dropped from approximate

85 Furthermore, dissolved oxygen concentrations in streambed pore water

86 Here we apply this proxy to estimate past dissolved oxygen concentrations in the near surface wate

87 uction was observed at higher EBCT where low dissolved oxygen concentrations may have limited biologi

88 itro into EMT6 cells was investigated at the dissolved oxygen concentrations of 0, 1 x 10(3), 5 x 10(

89 ucoid derivative of strain PAO1 each grew at dissolved oxygen concentrations of less than 3 microM.

90 pplied a biogeochemical model that simulates dissolved oxygen concentrations on the shelf in response

91 Exposure to temperature, pH, and dissolved oxygen concentrations projected by the year 20

92 Dissolved oxygen concentrations suggest that microbial r

93 r standardized conditions, we observed lower dissolved oxygen concentrations with the protocatechuic

94 he dark, when microbial respiration depleted dissolved oxygen concentrations within the biomat.

95 Here, we show that, at high dissolved oxygen concentrations, FeS accelerates NCU(IV)

96 oups on the OMZ margin are abundant at lower dissolved oxygen concentrations, including sulphur-cycli

97 n is accompanied by corresponding changes in dissolved oxygen concentrations, proxy data reflecting o

98 strong dependence on both organic carbon and dissolved oxygen concentrations.

99 d during periods of low water table and high dissolved oxygen concentrations.

100 -the-art machine learning model, to forecast dissolved oxygen concentrations.

101 aining sustained limiting extant nitrite and dissolved oxygen concentrations.

102 also exhibited ethanol production under low dissolved oxygen conditions, underscoring their utility

103 mimicked current and projected future pH and dissolved oxygen conditions.

104 studying the kinetics of dissolved oxygen consumption in the presence of suspende

105 Dissolved oxygen content, rather than temperature, exerc

106 id photoreaction of GO is insensitive to the dissolved oxygen content.

107 ent pressure, and it significantly increases dissolved oxygen content.

108 inks, reducing nearby acidity and increasing dissolved oxygen; creating conditions conducive to calci

109 Results indicate that dissolved oxygen, crops and irrigated cropland, fertiliz

110 peratures increased twice as fast and bottom dissolved oxygen declined >180% faster than average tren

111 Those WW components, as well as limited dissolved oxygen, decreased dissolution in WW.

112 Although the solubility of dissolved oxygen decreases with increasing water tempera

113 d their increased presence resulted in lower dissolved oxygen deficiency and higher proportions of sw

114 sh kills occurred in association with severe dissolved oxygen deficits and high contaminant loadings

115 Seasonal development of dissolved-oxygen deficits (hypoxia) represents an acute

116 n wastewater system (UWS) by targeting river dissolved oxygen depletion and ammonia peaks, reducing c

117 Nutrient enrichment and dissolved oxygen depletion that occur following these ev

118 Full-scale experiments at different dissolved oxygen (DO = 2 - 6 mg/L) setpoints indicated p

119 M solution through the center inlet port and dissolved oxygen (DO) above and below, strong transverse

120 (ETNP), we captured systematic variations in dissolved oxygen (DO) and associated variables (nitrite,

121 ical models based on in situ observations of dissolved oxygen (DO) and mechanistic models based on a

122 well the dynamic ammonium, nitrite, nitrate, dissolved oxygen (DO) and N2O data collected from both a

123 is seasonal trend is opposite to that of the dissolved oxygen (DO) and nitrate concentrations.

124 owmelt-driven water table peaking transports dissolved oxygen (DO) and nitrate from the vadose zone i

125 shifts of the dominating pathway at various dissolved oxygen (DO) and nitrite levels, consistent wit

126 Changes in dissolved oxygen (DO) and undigested BSA concentration w

127 s where diel fluctuations of temperature and dissolved oxygen (DO) are substantial.

128 reased due to combined effects of decreasing dissolved oxygen (DO) at depth, high sea surface tempera

129 SND under high dissolved oxygen (DO) brings high nitrogen conversion ra

130 f Mexico imparted a significant reduction in dissolved oxygen (DO) concentration and stimulated a blo

131 ted sludge process, reducing the operational dissolved oxygen (DO) concentration can improve oxygen t

132 of the oxygen and nitrogen input gases, the dissolved oxygen (DO) concentration in proximal microcha

133 As an important hydrological parameter, dissolved oxygen (DO) concentration is a well-accepted i

134 At dissolved oxygen (DO) concentration of 0.55 mg O2/L, fur

135 and nanoparticulate FeS as a function of pH, dissolved oxygen (DO) concentration, and FeS content.

136 tform capable of simultaneous measurement of dissolved oxygen (DO) concentration, glucose and lactate

137 Hypoxic conditions, defined as dissolved oxygen (DO) concentrations below 2 mg/L, are a

138 Dissolved oxygen (DO) concentrations followed the same t

139 a continuous system, very high and very low dissolved oxygen (DO) concentrations resulted in lower e

140 Dissolved oxygen (DO) concentrations shape the biogeoche

141 ncentrations, solid retention time (SRT) and dissolved oxygen (DO) concentrations), two full-scale mu

142 Exposure to low dissolved oxygen (DO) conditions may have deleterious ef

143 bstantial natural fluctuations in pCO(2) and dissolved oxygen (DO) conditions on diel, tidal, seasona

144 Low dissolved oxygen (DO) conditions selected for and high a

145 Dissolved oxygen (DO) did not observably inhibit Cr(VI)

146 ignificantly reduced operational bulk liquid dissolved oxygen (DO) from above 2 mg/L to at or below 0

147 icroelectrode measurements demonstrated that dissolved oxygen (DO) in biofilm-free dermal tissue was

148 nsor for in situ and real time monitoring of dissolved oxygen (DO) in environmental waters.

149 which integrate diffusion and consumption of dissolved oxygen (DO) in sediments, usually assume a dow

150 xidation of biogenic noncrystalline U(IV) by dissolved oxygen (DO) in the presence of mackinawite (Fe

151 Dissolved oxygen (DO) is an essential resource in ice-co

152 ormation of organic chemicals into OM, while dissolved oxygen (DO) is considered a minor or negligibl

153 sitive optical detection of oxygen including dissolved oxygen (DO) is of great interest in various ap

154 The influent dissolved oxygen (DO) level was increased stepwise to 6.

155 was significantly related to differences in dissolved oxygen (DO) level, and it was not explained by

156 idized and depleted, giving rise to elevated dissolved oxygen (DO) levels and remobilization of U(IV)

157 A decline in dissolved oxygen (DO) levels in many waterbodies have be

158 Under dissolved oxygen (DO) levels of 2.5-3.0 mg/L, N2O emissi

159 Dissolved oxygen (DO) reflects river metabolic pulses an

160 c-susceptible population, as a small drop in dissolved oxygen (DO) saturation (20%) allows for their

161 Dissolved oxygen (DO) sustains river ecosystems, but the

162 proteome analyses showed that at restricted dissolved oxygen (DO) the numbers of differentially expr

163 le, which can deliver significant amounts of dissolved oxygen (DO) to the shallow groundwater.

164 mplistic approach for producing gradients of dissolved oxygen (DO) within a lab-on-a-chip platform.

165 On the basis of dissolved oxygen (DO), ammonium, nitrite, and nitrate pr

166 t high frequency variability in temperature, dissolved oxygen (DO), and pH increases as pCO(2) increa

167 The monitored variables were pH and dissolved oxygen (DO), and soft sensors were used to pre

168 nite dissolution is profoundly influenced by dissolved oxygen (DO), carbonate, and solutes such as Ca

169 ver-enrichment since World War II, e.g., low dissolved oxygen (DO), decreased water clarity, and harm

170 Dissolved oxygen (DO), nitrate, and dissolved organic ca

171 oped when a simulated groundwater containing dissolved oxygen (DO), nitrate, arsenate, and sulfate wa

172 Temporal monochloramine, free chlorine, dissolved oxygen (DO), pH, ammonium, nitrite, and nitrat

173 Changes in dissolved oxygen (DO), pH, and other variables were simi

174 ements of water quality parameters including dissolved oxygen (DO), phosphate (PO(4)-P), ammonium (NH

175 the relationships between N2O flux and NO3-, dissolved oxygen (DO), temperature, land use and surfici

176 reased chl-a, reduced water clarity, and low dissolved oxygen (DO), while decreased N loadings from 1

177 f OMZs where they experience fluctuations in dissolved oxygen (DO).

178 (IV) stability in the presence of nitrite or dissolved oxygen (DO).

179 s techniques rely on pretreatments to remove dissolved oxygen (DO).

180 ing is driven mainly by the concentration of dissolved oxygen (DO).

181 er were subjected to cyclic perturbations of dissolved oxygen (DO).

182 mposition rate leads to rapid consumption of dissolved oxygen (DO).

183 Short-term (1.7 mg/L dissolved oxygen, DO for 3 days to 1 week) and long-term

184 In vitro intracellular changes of dissolved oxygen due to cell respiration were monitored,

185 trophication will affect metabolic rates and dissolved oxygen dynamics in the future are needed to el

186 duce the magnitude of FPV impacts on GHG and dissolved oxygen dynamics.

187 arks indicates they were able to exploit low dissolved oxygen environments (<1-3 ml l(-1)), occasiona

188 addition, quenching of the excited state by dissolved oxygen exhibits a pH dependence that parallels

189 as monitored during UV-A illumination with a dissolved oxygen fiberoptic microsensor.

190 ending, the probability density functions of dissolved oxygen fluctuations exhibit heavy tails that a

191 that estuaries are characterized by dynamic dissolved oxygen fluctuations that potentially favour PA

192 Both HABs and low dissolved oxygen followed similar patterns, increasing f

193 on of mediator sensitivity to reoxidation by dissolved oxygen for improvement of microbial solar cell

194 It is shown here that the elimination of dissolved oxygen from samples is critical when covalentl

195 filter is described that removes efficiently dissolved oxygen from the surface of an electrochemical

196 gh singlet oxygen, a highly reactive form of dissolved oxygen generated by sunlight irradiation of di

197 microbial community along a hypoxic to oxic dissolved oxygen gradient revealed that the relative abu

198 Here we sample across dissolved oxygen gradients in the oceans' largest OMZ an

199 Bottom dissolved oxygen has increased (0.48 mg L(-1) per decade

200 Surface water characteristics (e.g., high dissolved oxygen, high pH, and enrichment of (13)C in CO

201 This study shows that dissolved oxygen, hitherto an interferent purposefully r

202 f how operational parameters, in particular, dissolved oxygen, impact their activity and synergistic

203 es microbial activity and the consumption of dissolved oxygen in bottom waters.

204 genian ocean basins (>635 Myr ago) contained dissolved oxygen in concentrations sufficient to support

205 Declines in dissolved oxygen in freshwater are 2.75 to 9.3 times gre

206 For example, the concentration of dissolved oxygen in Pacific intermediate waters was cons

207 However, precise measurement of dissolved oxygen in real time remains difficult.

208 al method (Winkler titrations) for measuring dissolved oxygen in seawater, however, is much too high

209 was inversely proportional to the amount of dissolved oxygen in solution.

210 ic vegetation that restricted the flow, less dissolved oxygen in surface water, and greater organic m

211 Concentrations of dissolved oxygen in the ocean seem to correlate well wit

212 ith the heterogeneous oxidation of Fe(II) by dissolved oxygen in the presence of goethite (1.9 x 10(-

213 Dissolved organic carbon and dissolved oxygen in the water column, as well as SigmaRE

214 also is sensitive to selective quenching by dissolved oxygen, in which only cis stereoisomers are pr

215 Dissolved oxygen increased the rate at pH 0.

216 However, dissolved oxygen interference and electroactive interfer

217 Importantly, dissolved oxygen is available at least at the lake surfa

218 Dissolved oxygen is completely consumed within the upper

219 Calculations suggest that food, not dissolved oxygen is the limiting factor for eukaryal pop

220 hate buffer, pH 6.5, 4 to 23 degrees C), and dissolved oxygen is the only oxidant required.

221 ies, such as Na+, K+, Li+, NH4+, Ca2+, Mg2+, dissolved oxygen, lactate, ascorbate, and urate, which a

222 dation, to 16) and bimolecular reaction with dissolved oxygen (leading to 4 and 17 in a 1:1 ratio).

223 longer time points (>10 h), the presence of dissolved oxygen led to a greater production of CO2 than

224 A mid-shelf ribbon with near-bottom, dissolved oxygen less than 50 umol kg(-1) extended for 4

225 of coastal water quality in the form of low dissolved oxygen levels (hypoxia) can harm biodiversity,

226 Dissolved oxygen levels fell below the 9.0 ppm standard

227 Dissolved oxygen levels were measured at weekly or longe

228 ting the greater diversity; redox regime and dissolved oxygen levels were the main environmental driv

229 River Basin were monitored for temperature, dissolved oxygen levels, and fecal bacterial concentrati

230 metal concentrations, as well as decreasing dissolved oxygen levels.

231 reduced the water temperature, salinity and dissolved oxygen levels.

232 s revealed the development of abnormally low dissolved-oxygen levels as a response to anomalously str

233 Dissolved oxygen limitation did not govern NOB suppressi

234 reased while napA expression decreased under dissolved-oxygen-limiting conditions, whereas flaB was n

235 Coastal hypoxia (dissolved oxygen </= 2 mg/L) is a growing problem worldw

236 ace oxygen mass balance model and continuous dissolved oxygen measurements from four locations to pro

237 bundance, oxidation-reduction potential, and dissolved oxygen measurements indicated that microbial g

238 These results indicate that dissolved oxygen modulates gene expression in B. burgdor

239 To test the possibility that dissolved oxygen modulates gene expression in B. burgdor

240 Oxidants (e.g., dissolved oxygen, nitrate) flowing in from upgradient ap

241 -reactant accelerator to directly reduce the dissolved oxygen (O(2) ) to reactive oxygen species (ROS

242 ggests a model describing the consumption of dissolved oxygen (O(2)) in the hypolimnia of eutrophic l

243 Dissolved oxygen (O(2)) is essential for most ocean ecos

244 competitively take oxygen from H(2)O(2) and dissolved oxygen (O(2)), whereas the remaining residues

245 surements of bacterial sulfate reduction and dissolved oxygen (O2) in hypersaline bacterial mats from

246 Warming of the oceans and consequent loss of dissolved oxygen (O2) will alter marine ecosystems, but

247 In unfed controls, the concentration of dissolved oxygen ([O2]) in all replicates exhibited regu

248 e important for assessing the impacts of low dissolved oxygen on aquatic ecosystems at large spatial

249 kely to enable new studies on the effects of dissolved oxygen on cellular behavior.

250 rfaces did not influence the rate of loss of dissolved oxygen or oxidation of ascorbic acid.

251 with cells grown with 20 microM or 3 microM dissolved oxygen, or anaerobically with nitrate, reveale

252 tions that the complex is indeed tolerant to dissolved oxygen over timescales long enough for practic

253 emained relatively unchanged with respect to dissolved oxygen, pH, and ammonia-nitrogen, although tem

254 e variables related to ecosystem metabolism (dissolved oxygen, pH, and chlorophyll-a concentration) a

255 Directly measured variables (dissolved oxygen, pH, and chlorophyll-a concentration) r

256 concentrations and their ratios, as well as dissolved oxygen, played important roles in promoting th

257 , the sensors did not require the removal of dissolved oxygen prior to successful pH measurements.

258 Dimensionless parameters were used to model dissolved oxygen profiles and establish that mass transf

259 goals of the study were to measure and model dissolved oxygen profiles within high-temperature (65-75

260 displays a unimodal pattern with decreasing dissolved oxygen, reaching maximum values on the edge of

261 We employ dissolved oxygen regimes that represent natural aquatic

262 Electrochemical sensors for pH and dissolved oxygen remain the most commonly used in biopro

263 hotodissociation and was inhibited 2-fold by dissolved oxygen removal, suggesting the importance of b

264 activates the protease; recycling of PTH2 by dissolved oxygen results in complete inhibition of the p

265 Dissolved oxygen, riboflavin and other flavins, proteoly

266 (3) physical and chemical stressors such as dissolved oxygen, salinity, and upwelling; and (4) adapt

267 Dissolved oxygen saturation (%DO) decreased by -0.24 +/-

268 Concentrations of algal pigments, dissolved oxygen saturation, and pH rapidly declined fol

269 on between reefs with distinct pH, salinity, dissolved oxygen, sedimentation, and flow dynamics to de

270 utilizes 96-well-type electrodes array (DOX-dissolved oxygen sensor) with principal component analys

271 We eliminated interference from dissolved oxygen, separated xylose and mannose along wit

272 ng not only verified the efficacy of reduced dissolved oxygen set-point in reducing N(2)O emission by

273 Temperature, sulfide, As and dissolved oxygen significantly shaped the microbial comm

274 (2 mM and 10 mM) of K2S2O8 and 8.2 mg L(-1) dissolved oxygen suggested that monomeric U(IV) species

275 The flavin radical is affected by dissolved oxygen, suggesting that its binding site withi

276 the model are chlorophyll a, sediment type, dissolved oxygen, temperature, and depth.

277 Dissolved oxygen/temperature probes and septa for inject

278 the transition from a high oxygen level (10% dissolved oxygen tension or DOT) to a low oxygen level (

279 The CaO2 shells could quickly increase dissolved oxygen to extremely anaerobic water in the ini

280 wed by oxidation of the Fe(II)-TC complex by dissolved oxygen to generate a Fe(III)-TC complex and re

281 ogenerated electrons and their reaction with dissolved oxygen to produce superoxide anions.

282 The algal growth provided dissolved oxygen to the cathode reaction of the MFC, whe

283 rates might produce enough fixed carbon and dissolved oxygen to yield net production as an average o

284 howed 92% to >=99% removal efficiency, while dissolved oxygen, total dissolved solids, pH, and electr

285 bedding) nanosensors have been developed for dissolved oxygen using organically modified silicate (or

286 parent aerobic conditions by first consuming dissolved oxygen via aerobic respiration, and then direc

287 -defined free Fe(II) was lost on exposure to dissolved oxygen was also enhanced by the more mature OC

288 The evolution of dissolved oxygen was found to be similar in all bottles,

289 the arsenite/goethite under conditions where dissolved oxygen was present in solution led to the pres

290 How much dissolved oxygen was present in the mid-Proterozoic ocea

291 In addition, dissolved oxygen was produced in the anode, resulting in

292 Dissolved oxygen was selectively depleted (2- to 3-fold)

293 on oxidation in the presence of goethite and dissolved oxygen was the primary reason for the higher A

294 revealed a continuous, shelfwide band of low dissolved oxygen waters that were dominated by Thaumarch

295 and underwater glider-based measurements of dissolved oxygen were made in this region.

296 e well predicted by redox indicators (Eh and dissolved oxygen) whereas Mn shows no significant relati

297 same depth as a nutrient maximum with lower dissolved oxygen, which is consistent with the recent fi

298 attenuation and increasing concentrations of dissolved oxygen, while the same analysis found a negati

299 s grown under aerobic conditions (185 microM dissolved oxygen) with cells grown with 20 microM or 3 m

300 We mapped the distribution of dissolved oxygen within isolated bovine lenses and also