ライフサイエンスコーパス: sink

1 g the function of a wetland as a long-term C sink.

2 f natural CO2, thus weakening the global CO2 sink.

3 ight" (LOS) between the heat source and heat sink.

4 and interannual variability of the land CO2 sink.

5 on-fiber electrodes as the terminal electron sink.

6 ary production (GPP) to this weakened carbon sink.

7 ting a repetitive nature of this land carbon sink.

8 tial consequences for the terrestrial carbon sink.

9 ased the magnitude of the terrestrial carbon sink.

10 dual role as nutrient source and autoinducer sink.

11 warming temperatures) may impact the land C sink.

12 the total extent and a 0.22 Tg yr(-1) carbon sink.

13 hermal contacts with the heat source or heat sink.

14 enic carbon emissions, termed as land carbon sink.

15 ecies volatility and particle condensational sink.

16 nd widespread degradation of the land carbon sink.

17 reme that negatively affects the land carbon sink.

18 ctic tundra might be a globally important Hg sink.

19 year-to-year fluctuations of the land carbon sink.

20 the SPNA as one of the major planetary heat sinks.

21 etallic materials as free surface are defect sinks.

22 kely to be net sources of carbon rather than sinks.

23 e coastal wetlands for enhancing blue carbon sinks.

24 vironments represent globally largest carbon sinks.

25 by emissions, transport, transformation, and sinks.

26 og peat accumulation returned sites to net C sinks.

27 nd sometimes more dramatic changes to carbon sinks.

28 orest-dominated sites were consistent carbon sinks.

29 speed of approximately 2.5 m/s prior to its sinking.

30 We found that Harvard Forest is a net H2 sink (-1.4 +/- 1.1 kg H2 ha(-1) ) with soils as the domi

31 kg H2 ha(-1) ) with soils as the dominant H2 sink (-2.0 +/- 1.0 kg H2 ha(-1) ) and aboveground canopy

32 the system from a small source to a net CH4 sink (21 +/- 2 and -31 +/- 1 mg CH4 m(-2) season(-1) at

33 rage was found to be the dominant phosphorus sink (64% on average).

34 etime (<25 ps) renders them potential energy sinks able to compete with the reaction centers and dras

35 ation of amino acid transport from source to sink affects plant N use efficiency.

36 to propagate the Ca(2+) wave are source and sink, amplifying wave, and release and diffusion.

37 ightings are more likely to occur in climate sink and 'divergent' regions (areas where many rapid and

38 ees represent the largest terrestrial carbon sink and a renewable source of ligno-cellulose.

39 Both source and sink and amplifying wave regulate ATP levels using hydro

40 wn atmospheric studies suggesting an overall sink and bottom-up ecological approaches indicating a mo

41 heretofore unrecognized subterranean methane sink and contribute to our understanding of the carbon c

42 ylpropanoid pathway is a major global carbon sink and is important for plant fitness and the engineer

43 gth of the temperate broadleaf forest carbon sink and its capacity to mitigate anthropogenic carbon e

44 s offset 1-6% of the growing season soil CH4 sink and may have briefly changed the forest to a net CH

45 obes.The extent to which the ocean acts as a sink and source of airborne particles to the atmosphere

46 the enstrophy transport act as leading order sink and source terms, respectively.

47 while fragmentation persistently offset the sink and turned many edge-affected forests into a carbon

48 ocesses, principally the surface production, sinking and interior remineralization of organic particl

49 ced vertical carbon transport (gravitational sinking and subduction) at mesoscale ocean fronts may ex

50 nge mitigation and adaptation, acting as CO2 sinks and buffering the impacts of rising sea level.

51 West Antarctica mean that significant carbon sinks and negative feedbacks to climate change could als

52 tected in hospitalized infants also occur in sinks and on surfaces, and belong to species such as Sta

53 y; beige fat thereby functions as a 'glucose sink' and improves glucose tolerance independently of bo

54 help bring bosons into a dynamically emerged sink, and a Lindblad operator corresponding to local coo

55 Mitochondria can be both an H2S source and sink, and many of the biological effects of H2S relate t

56 emical performance, electron flux to various sinks, and anodic microbial community structure in two-c

57 -limited solar conversion technologies, heat sinks, and biofuel production.

58 ) has the potential to characterize sources, sinks, and degradation processes in the environment.

59 Drains, sinks, and faucets were most frequently colonized, and P

60 r drain, disinfecting siphons underneath the sinks, and rimless toilets.

61 even large subpopulations can potentially be sinks, and that movement dynamics (e.g. immigration) amo

62 or contributor not only to the 2011 global C sink anomaly but also to global reductions in photosynth

63 tive importance compared with other electron sinks are poorly understood, particularly under light.

64 intermediate metabolites and macromolecular sinks are tightly coupled to the cell cycle in a marine

65 , and constitute a globally important carbon sink, are among the most vulnerable habitats on the plan

66 ppear to undergo degradation during particle sinking as compared to organic carbon.

67 and cement manufacturing paired to suitable sinks as having the lowest levelized cost of capture, co

68 t regarding their respective roles as carbon sinks, as even the wildfire charcoals formed at the high

69 ontribution to the global terrestrial carbon sink but is also the most heavily fragmented forest biom

70 ls (ESMs) estimate a significant soil carbon sink by 2100, yet the underlying carbon dynamics determi

71 duced the capacity for the fen to act as a C sink by causing shifts in vegetation and thus reducing m

72 l Nino drought temporarily halted the carbon sink by increasing tree mortality, while fragmentation p

73 y before present (5 kyBP), the concurrent C sink by peat buildup could mask large early LUC emission

74 demonstrated that MPhi can act as "metabolic sinks" by depleting glucose levels at the implanted sens

75 the sites switched between functioning as C sinks/C sources in wet/dry years.

76 t northern boreal forest soils have a strong sink capacity for Hg, and indicate that the sequestered

77 tations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands a

78 aused by an increased mitochondrial electron sink capacity.

79 The potential for a sink (CO2) to source (PSII) feedback mechanism is discus

80 Perfect sink conditions can still be applied for longer times, i

81 y improving the estimations based on perfect sink conditions.

82 n based on a steady-state flux under perfect sink conditions.

83 Thus, both electron sinks contribute to the alleviation of excess electrons

84 The sunk cost effect, an interesting and well-known maladapt

85 nscientiousness) are more susceptible to the sunk cost effect.

86 we investigated neural responses induced by sunk costs along with measures of core human personality

87 Unlike in business decisions, sunk costs was not as evident.

88 ncluding self-justification, accountability, sunk costs, and cognitive dissonance result in escalatio

89 n serve as either permanent or temporary NOx sinks depending on the monoterpene precursor.

90 We introduce a source-sink diffusion model for polarization transfer which is

91 owever, carbon dynamics after current carbon sink diminishes to zero differ for different demographic

92 o cause melting of their surrounding ice and sink downwards.

93 ) was used to track FSSC and FOSC strains in sink drain biofilms by detecting its target antigen, an

94 sent, as mixed fungal communities, in 83% of sink drain biofilms.

95 iability (IAV) and trends of the land carbon sink, driven largely by the El Nino-Southern Oscillation

96 substitution and reduction in forest carbon sink due to wood harvesting.

97 rved decline to increases in the terrestrial sink during the past decade, associated with the effects

98 route, even though tumor vessels can act as sinks during the dissemination of small molecules.

99 pollution released from the U-864 submarine sunk during WWII and potential introduction of that Hg i

100 Understanding source-sink dynamics is important for conservation management,

101 ently unoccupied areas, understanding source-sink dynamics, and understanding community dynamics shou

102 ane Joaquin when the Merchant Vessel El Faro sank east of the Bahamas on October 1, 2015.

103 scapes into parasite demographic sources and sinks, ecological concepts that have parallels in malari

104 water table gradient in peatlands-a major C sink ecosystem.

105 the well-known phenomena of a vascular heat sink effect that causes high temperature differentials t

106 interior surfaces, often referred to as the "sink effect", and their subsequent re-emission significa

107 avoid incomplete ablation secondary to heat-sink effects and damage to major blood vessels; however,

108 ation over Australia, we suggest that carbon sink episodes will exert greater future impacts on globa

109 ve transgene expression and the best ways to sink existing pools of terpene precursors are discussed.

110 Laboratory-based infinite sink extractions with silicone rubber (SR) as the extrac

111 se stools in 24 h and >/=1 of the following: sunken eyes, skin tenting, dysentery, intravenous (IV) r

112 subcellular/cellular events overcome source-sink factors in cardiac tissue to generate DADs of suffi

113 Our results support the proposal that sinking faecal matter represents a mechanism by which fl

114 The global average sinking fluxes were 0.8 +/- 1.3 ng m(-2)d(-1) for PFOA,

115 The main atmospheric sink for (CF3)2CFCN was determined to be reaction with O

116 The ocean is the largest sink for anthropogenic carbon dioxide (CO2), having abso

117 sed to predict the future of the terrestrial sink for anthropogenic CO2(1) .

118 of CaCO3 under aerated conditions provided a sink for aqueous Ca, allowing higher V concentrations li

119 an hydroxyl (OH) concentrations, the primary sink for atmospheric methane, over the same period.

120 local potentials as controllable source and sink for bosonic atoms.

121 d global temperature rises, and as a natural sink for carbon able to reduce atmospheric CO2.

122 ed STING activation by acting as a molecular sink for cdNs.

123 Estuarine sediments provide an important sink for contaminants discharged into fluvial, estuarine

124 embryos with the same oligonucleotides, as a sink for endogenous CREB1.

125 d to use ferric iron minerals as an electron sink for fermentation.

126 This provided an important sink for hydrospheric water and a mechanism for oxidizin

127 ropose a hypothesis that the OS can act as a sink for membrane proteins.

128 This corroborates the deep sea as a major sink for microplastics and the presence of accumulation

129 SSA may represent an underappreciated inland sink for NOx/SO2 oxidation products and a source of halo

130 We hypothesize that BSi in chert was a major sink for oceanic dissolved silica (DSi), with fluctuatio

131 al component of the biosphere and is a major sink for organic carbon.

132 chain can act as a multifunctional electron sink for reductant from cytosolic pathways.

133 tential to act as a temporal storage or even sink for terrigenous aromatic DOM compounds.

134 de reductase, potentially acting as a global sink for the greenhouse gas nitrous oxide.

135 atment plants (WWTPs) could serve as a major sink for these emerging contaminants.

136 While the lake is a net sink for THg and MeHg, concentrations and fluxes of THg

137 sedimentary environments, making it a major sink for this toxic metalloid.

138 er flocs are expected to remain an effective sink for trace elements.

139 ease, and the role of low-latitude MPAs as a sink for urchins changed significantly in contrasting wa

140 have been suggested as potentially important sinks for carbon (C) with appropriate management and thu

141 at non-equilibrium GBs act as more efficient sinks for defects and could be utilized to create more r

142 f microbes using extracellular substrates as sinks for electrons at The Cedars, but also highlights t

143 re, we identify putative malaria sources and sinks for pre-elimination Namibia using malaria parasite

144 erson Island and other remote islands may be sinks for some of the world's increasing volume of waste

145 stles and elastomers could act as absorptive sinks for TCS during brushing.

146 , these boundaries may act as more efficient sinks for the excess interstitials and vacancies produce

147 ch underwent reductive dissolution, CWs were sinks for the studied metals.

148 tropical forests may yield a weakened carbon sink from both decreased GPP and increased RE.

149 the soil, and therefore perform an important sink function in global carbon cycling.

150 and NEE, thus reducing or reversing their C sink function.

151 In-sink grinding (ISG) via a food-waste disposer and flushi

152 predominant contribution of crude oil to the sinking hydrocarbons.

153 uggests vertical export via incorporation in sinking (ice-) algal aggregates.

154 l organic matter can be an additional silver sink in environmental systems.

155 We find the current gross carbon sink in forests recovering from harvests and abandoned a

156 lthough both pan-tropical and long-term, the sink in remaining intact forests appears vulnerable to c

157 cumulated carbon budget switched to a carbon sink in the 1960s, sequestering an estimated 1,642 Tg C

158 overturning is likely to strengthen the CO2 sink in the near future by trapping natural CO2 in the d

159 or driving the increasing strength of carbon sinks in these forests.

160 tion according to changes in its sources and sinks-including a large sink that is related to GPP.

161 bonds modified on a wild-type (WT) specific sink inhibit the Exo III digestion; thus, subsequent cat

162 Subduction zones, where oceanic plates sink into the Earth's interior, are the most important g

163 ion as particulate organic carbon (POC) that sinks into the ocean interior.

164 The annual total sink is estimated to be 3.9 +/- 0.2 PgC for the assumed

165 The terrestrial carbon sink is increasing, yet the mechanisms responsible for i

166 However, the sink is largely offset by emissions from wood products b

167 Plants acted as an N sink, limiting NO emissions under optimal soil moisture.

168 Far from being a terminal carbon sink, many wall polymers can be degraded and recycled by

169 These results indicate that silver ion sinks may lessen AgNP impacts on natural microbial ecolo

170 dels and provide support for a graded source-sink mechanism underlying zebrafish dorsal-ventral patte

171 ur analyses support a fourth model, a source-sink mechanism, which relies on a restricted BMP antagon

172 Central Water (ENACW) that is entrained into sinking Mediterranean Overflow Water (MOW) that leads to

173 uctivity will be achieved if both source and sink metabolism are engineered.

174 An extended sink model, incorporating a finite reaction zone, was ab

175 fusion and found that it supports the source-sink model, suggesting a new mechanism to shape BMP grad

176 Relationship between source and sink nitrogen transport processes and metabolism 43 VIII

177 he terrestrial biosphere will be a source or sink of carbon (C) under a future climate of elevated CO

178 that young Russian forests represent a total sink of carbon at the rate of 1.26 Tg C yr(-1) .

179 production diminishes, is as a major global sink of carbon storage.

180 stau expresses the sink of eddy energy induced by the current feedback.

181 reactions on or in the seafloor are a major sink of many elements and alkalinity in seawater.

182 They are recognized to be a major sink of many elements in the ocean but are difficult to

183 air-sea transfer of momentum by providing a sink of mesoscale eddy energy as an atmospheric source.

184 in coastal ecosystems and both a source and sink of N2 O.

185 studies are needed to constrain the oceanic sink of PFAS.

186 estimate is limited because of a mesospheric sink of SF6; however, the reanalyses also differ substan

187 The most prominent sink of the increased flux to hydroxycinnamates is syrin

188 spiratory process that is a major source and sink of the potent greenhouse gas nitrous oxide.

189 ust 2010 and October 2011, disclose that the sinking of spill-associated substances, mediated by mari

190 that no plausible combination of sources and sinks of CO2 from fossil fuel, land, and oceans can expl

191 ed by bryophytes might be strong atmospheric sinks of COS at night and weaker sinks or even sources o

192 Measurements of the sources and sinks of H2 in various ecosystems are sparse, resulting

193 terize sources, transformation pathways, and sinks of organic aliphatic compounds, many of them being

194 Agricultural soils are major sinks of silver nanoparticles in the environment, and cr

195 ved within mitochondria, a source, yet not a sink, of AcroB adducts, illustrating that a mitochondria

196 at potential to evaluate the role, as carbon sinks, of water-limited forests under climate change.

197 r studies propose a decrease in the chemical sink (OH).

198 a Fc (A4Fc) overcame the issue of an antigen sink or, in the case of A4Fc, systemic toxicity.

199 atmospheric sinks of COS at night and weaker sinks or even sources of COS during daytime.

200 ks, while inland wetlands provided small CO2 sinks or were nearly CO2 neutral.

201 DOC represents 90% of the respired non-sinking organic carbon.

202 tions of nitrogen transporters in source and sink organs and their importance in regulating nitrogen

203 n, architecture and physiology of source and sink organs are main determinants of rice productivity.

204 evels by affecting Suc synthesis, whereas in sink organs it regulates Suc consumption.

205 remobilization and utilization in source and sink organs.

206 demonstrated imbalance of new production and sinking particle export in coastal upwelling ecosystems.

207 ransferred from the surface to deep ocean as sinking particles or dissolved organic carbon (DOC).

208 carbon via photosynthesis, exported through sinking particles, and finally sequestered in the deep o

209 ter than 100% of the carbon supplied by fast sinking particles.

210 erals, which control the size and density of sinking particles.

211 y via attachment of the mercury compounds to sinking particles.

212 ined by chemical energy, in the form of fast-sinking particulate organic carbon, supplied by the biol

213 Sinking particulate organic matter (POM, phytodetritus)

214 at AAP8 plays an important role in source-to-sink partitioning of nitrogen and that its function affe

215 en 2110 and 2260, followed by another carbon sink period.

216 ydrothermal-based productivity combined with sinking photosynthetic organic matter in a soft-sediment

217 e day (June 8, 2010) of the period after the sunken platform's riser pipe was pared at the wellhead (

218 s at lower latitudes flows in to replace the sinking polar surface water.

219 clone, revealing the major global source and sink populations and routes for the spread of multi-drug

220 the idea that CheV functions as a "phosphate sink" possibly to off-set the over-stimulation of the ki

221 Although a sink potential can collect bosons in equilibrium and ind

222 that engineering N allocation from source to sink presents an effective strategy to produce crop plan

223 s to deliver a cascade of signals to various sinks, presumably to coordinate whole-plant Pi homeostas

224 e microplastics can alter the properties and sinking rates of zooplankton egests and, (3) faecal pell

225 d by particle respiration, fragmentation and sinking rates) controls the size of this effect and is a

226 6)-10(9) L/kg made the biochars often act as sinks, rather than sources, of PAHs.

227 and CH4 (22.9-41%) were the largest electron sinks regardless of the potentials tested.

228 areas where moving isotherms converge), and 'sink' regions (areas where isotherms locally disappear).

229 cillation, CAM-related functions, and source-sink relations.

230 rast, temporal changes in the oceanic carbon sink remain poorly understood.

231 The sink represents the potential for negative emissions if

232 contributing 9% and 2% of the terrestrial C sink, respectively.

233 r and monomer into a prepolymerized hydrogel sink results in a tunable stiffness gradient at the cell

234 arrays connected to a chemical or structural sink results in continuous removal of selected elements

235 egions of synthesis (mature leaves) to sugar sinks (roots, fruits).

236 questration as a NET centre around issues of sink saturation and reversibility.

237 , assuming the biological pump as the unique sink, showed a wide range of variability, from few years

238 make them neutrally buoyant or cause them to sink slowly.

239 lysis further confirmed the absence of local sink-source pairs in the vStr.

240 adiation regime, within-canopy microclimate, sink/source distributions of CO2 , H2 O and heat, and fo

241 We found a wide range of carbon sink/source function, with mean annual net ecosystem pro

242 led to significant reduction in seed-set and sink starch metabolism enzymatic activity.

243 The linear relationship between GHG sink strength and N load assumed by most studies can ove

244 Changes in tropical forest carbon sink strength during El Nino Southern Oscillation (ENSO)

245 Robust predictions of the net GHG sink strength of grasslands depend on how experimental N

246 or underestimate predictions of the net GHG sink strength of grasslands depending on their N baselin

247 Ndep either enhanced or reduced the net GHG sink strength of most grasslands, but as experimental N

248 ,night represents a non-negligible competing sink strength that diminishes the significance of HR.

249 The annual CO2 sink strength was 93.15 and 208.37 g C m(-2) for inland

250 nd fungal effects on plant growth and carbon sink strength were correlated with shifts in RBio in thi

251 The relative sink strengths of equilibrium and non-equilibrium GBs we

252 the in-use stock and ("final") environmental sinks such as soil and sediment.

253 the in-use stock and ("final") environmental sinks such as soil and sediment.

254 and to quantify their amounts in (temporary) sinks such as the in-use stock and ("final") environment

255 and to quantify their amounts in (temporary) sinks such as the in-use stock and ("final") environment

256 cted BMP antagonist distribution acting as a sink that drives BMP flux dorsally and gradient formatio

257 The results further highlight the important sink that forests provide for atmospheric organic chemic

258 heir C emissions, making them an important C sink that is likely to increase with eutrophication and

259 s in its sources and sinks-including a large sink that is related to GPP.

260 g erythrocytes, creates a formidable antigen sink that may limit the efficacy of CD47-targeting thera

261 III-nitrides to Ru, rendering Ru an electron sink that promotes N identical withN bond cleavage, and

262 ses on global quantities of N in sources and sinks that are easier to estimate, in contrast to estima

263 ring the number and diversity of sources and sinks, the widely used proxies such as concentration and

264 he United States is currently a major carbon sink, there are uncertainties in how long the current ca

265 h fixed carbon or representing the strongest sinks, thereby potentially amplifying asymmetric competi

266 t methylmercury can be produced in particles sinking through oxygenated water column of lakes.

267 climate led the forest to transition from a sink to a source of carbon.

268 forts to predict the response of the H2 soil sink to changes in anthropogenic H2 emissions and shifti

269 urce strength to overcome a weakened current sink to depolarize Vm and trigger action potentials.

270 rested area, transitioning the system from C sink to source.

271 nd predicts that the particles either float, sink to the ocean floor, or oscillate vertically, depend

272 l nutrients need to be rapidly cycled before sinking to aphotic layers.

273 ticular sites on histones then become methyl sinks to enable the conversion of SAM to SAH.

274 ace water is particularly cold and dense, it sinks to generate a tropic-ward flow on the ocean floor

275 ion plots and turned the mesocosms from N2 O sinks to N2 O sources, but had little influence on CH4 e

276 ascribe 4-10% of atmospheric methane (CH4 ) sinks to upland soils and have assumed until recently th

277 ed pQBR57 to persist in P. putida via source-sink transfer dynamics.

278 on types, contrasting with the more constant sink typically measured in mesic ecosystems.

279 source over the first 10 years to a notable sink until they reach maturity.

280 cadal circulation changes on the oceanic CO2 sink using a carbon cycling model.

281 ine and tanker truck to appropriately paired sinks using a bottom-up cost model and geo-referencing a

282 ointly constrain 36 y of methane sources and sinks, using ground-based measurements of methane, methy

283 atterns may better constrain regional carbon sink variability in coupled carbon-climate models.

284 Causes could be sink variability or a temporary reduction in industrial

285 We show the 2010-11 carbon sink was primarily ascribed to savannas and grasslands.

286 To increase methanol consumption, an "NADH Sink" was created using Escherichia coli lactate dehydro

287 Cold water holds more gas, so this sinking water exports O2 and nutrients, thereby supporti

288 ions (and assuming no change to the chemical sink), we find that fossil fuels contribute between 12-1

289 diffusion channel for defects to reach other sinks when defect diffusivity is high at boundaries.

290 ge quantity of reduced OC to the sedimentary sink, which could otherwise be oxidized back to CO2.

291 a basis, coastal wetlands provided large CO2 sinks, while inland wetlands provided small CO2 sinks or

292 uncertainties in how long the current carbon sink will persist and if the CHF will eventually become

293 n terrestrial and aquatic carbon sources and sinks will require significant additional research and m

294 2) , mangroves are globally important carbon sinks with carbon density values three to four times tha

295 ompetitive DNA hybridization probes (probe + sink) with catalytic amplification assisted by Exo III.

296 charcoal to soot) is a widely acknowledged C sink, with the latest estimates indicating that ~50% of

297 enitrifying N2O reducers, which could be N2O sinks without major contribution to N2O formation.

298 nd from much smaller species associated with sunken wood and other organic deposits, and that the end

299 ll approaches agreed that the current carbon sink would persist at least to 2100.

300 trace gas with a large microbe-mediated soil sink, yet cycling of this compound throughout ecosystems