ライフサイエンスコーパス: moisture

1 g(-1) (expressed as sodium nitrate at 12% of moisture).

2 s, with resulting indirect feedbacks on soil moisture.

3 convergence of low-level, externally sourced moisture.

4 ortality by 40% compared to LSM-modeled soil moisture.

5 chanism for C destabilization under elevated moisture.

6 face temperature, available soil N, and soil moisture.

7 xhibiting surprisingly high stability toward moisture.

8 response of photosynthesis to changing soil moisture.

9 ure and is tolerant towards oxygen and trace moisture.

10 vanadia and tungsta sites, temperature, and moisture.

11 and positive or nonlinear responses to soil moisture.

12 d organic cultivars (in %), were: 72 and 72 (moisture); 0.87 and 0.90 (ashes); 1.5 and 1.4 (proteins)

13 ows: barrel temperature, 129 degrees C; feed moisture, 15%; and screw speed, 299 rpm.

14 Goldenberry waste powder, contained 5.87% moisture, 15.89% protein, 13.72% fat, 3.52% ash, 16.74%

15 (0.64-7.36g/100g rice) was extruded under 5 moisture (16.64-23.36g/100g) and 5 temperature (106.36-1

16 results indicated that seeds contained 5.30% moisture, 3.99% ash, 9.19% fat, 14.31% fiber, 27.21% pro

17 GAB model was chosen to describe the moisture adsorption isotherm behaviours.

18 alone presented higher hygroscopicity in the moisture adsorption isotherms at 25 degrees C and lower

19 a high-emission scenario, as only over-lake moisture advection is high enough to sustain Clausius-Cl

20 There is anomalous moisture advection over the upstream of the TP caused by

21 d nanoplatelets appear to be quite stable in moisture, allowing out-of-glovebox device fabrication.

22 Increased moisture and anaerobiosis initially suppress soil C mine

23 hat C mineralization declines under elevated moisture and associated anaerobic conditions, leading to

24 and after 12months of storage, at 12 and 15% moisture and at temperatures of 11, 18, 25, and 32 degre

25 ce grains were adjusted to 13%, 16%, and 18% moisture and autoclaved at 121 degrees C for 30 and 60mi

26 Spatial heterogeneity in soil moisture and conspecific density were the predominant an

27 er concentrations, FPH minimized expressible moisture and cook loss, while maximizing salt extractabl

28 constraining the immediate increase in soil moisture and drying out over the following months, as we

29 ummer monsoon which is the primary source of moisture and dynamic forcing conducive for warm-season s

30 l drylands is well constrained, whereas soil moisture and ecological droughts, which drive vegetation

31 as much as mean precipitation and less than moisture and extreme precipitation for most models, regi

32 ookies made with maple syrup had the highest moisture and greening corresponding with lowest free chl

33 Qc-5-Cu-sql-beta is stable to moisture and its separation performance is unaffected by

34 loss in the early decomposition stages, soil moisture and legacy effects of initial differences in li

35 lace lead and improve their stability toward moisture and light.

36 i-dry foods, but is highly sensitive to high moisture and liquid foods.

37 netite in forest soils due to increased soil moisture and lower pH.

38 on, alpha-bis-PCBM resists the ingression of moisture and passivates voids or pinholes generated in t

39 h relative humidity storage, and use of high moisture and pH ingredients.

40 sissippi basin that gradually builds up soil moisture and reduces the basin's infiltration capacity,

41 the amount of precipitation reduced the soil moisture and Rs by -12% and -6%, respectively, but did n

42 zed to 28% below the ambient level, the soil moisture and Rs values decreased by an average of -14% a

43 ing a twin screw extruder with constant feed moisture and screw speed.

44 models; however, within certain biomes soil moisture and soil carbon emerge as dominant predictors o

45 ve of this study was evaluate the effects of moisture and temperature during grain storage on the fun

46 Feed moisture and temperature increased density and total vol

47 ence of whey protein concentrate (WPC), feed moisture and temperature on the physicochemical properti

48 g monsoon circulation, the locally available moisture and the frequency of moisture-laden depressions

49 trast, films with 30% glycerol lost the most moisture and their elongation was reduced significantly,

50 t were performed without exclusion of air or moisture and through applications in stereoselective ole

51 Moisture and tocopherol contents were more closely corre

52 breathability in response to temperature and moisture and window shutters that automatically open and

53 e) were investigated in HMF-amino acid (high moisture) and Coffee-amino acid (low moisture) model sys

54 ased emulsifying capacity (52.2% with 12% of moisture) and foam formation, compared with sample obtai

55 ecreased extraction yield (51.6% with 15% of moisture) and protein solubility (24.8% with 15% of mois

56 ired, the reaction is insensitive to air and moisture, and it proceeds at room temperature.

57 s of plant photosynthesis, soil temperature, moisture, and nitrogen.

58 environmental factors (i.e. soil nutrients, moisture, and phenolics) and geographical distance, both

59 l stability, phase stability, sensitivity to moisture, and potential issues due to the toxicity of le

60 oxidant activity to the cheeses, reduced the moisture, and preserved the unsaturated fatty acids and

61 lotting properties, leading to higher yield, moisture, and texture parameters of curd.

62 ata to observations of water potential, soil moisture, and vapor pressure deficit over 2 yr in the No

63 f monthly meteorological, hydrological, soil moisture, and vegetation droughts from 1981 to 2013 were

64 Metal catalysts and moisture- and air-free conditions are not required.

65 urrence and concentration of macronutrients, moisture, ash, dietary fiber, fatty acids, minerals, car

66 Some nutritional and antinutritional (moisture, ash, protein, fructans, dietary fibers, phenol

67 creasing knowledge about the role that wind, moisture availability and vegetation cover play in shapi

68 sts is largely controlled by agriculture and moisture availability from irrigation, but further analy

69 heir typically high solar absorption and low moisture availability generates the urban heat island ef

70 peratures interact with other key drivers of moisture availability to determine the sustainability of

71 that growth of both species is sensitive to moisture availability, yet show limited evidence of decl

72 biomass change as well as the feedbacks with moisture balance and CO2 in individual models.

73 incorporated emulsion coatings with improved moisture barrier, wettability and surface adhesion onto

74 The values of moisture, betalains content, and retention were 3.33-4.2

75 Moisture budget analysis indicates that on multi-year ti

76 udoacacia seedlings under the same mean soil moisture, but with different drought frequency caused by

77 ABSTARCT: Constraints on soil moisture can guide agricultural practices, act as input

78 While temperature, moisture, carbon supply, and other site characteristics

79 he Arctic N2O budget will depend strongly on moisture changes, and that a gradual deepening of the ac

80 nge on vegetation when assessing future soil moisture conditions in water-limited ecosystems.

81 Arginine and kLysine increased under the low moisture conditions of Coffee-amino acid model systems.

82 may be more directly linked to environmental moisture conditions than might otherwise be expected.

83 ercus robur) saplings under wet and dry soil moisture conditions to (18) O-depleted water vapour (c.

84 tting patterns interact with antecedent soil moisture conditions to alter pore-scale, core-scale, and

85 ge of 5-50 degrees C under both low and high moisture conditions.

86 sed with increasing frequency (27-2450 MHz), moisture content (4.2-19.6% w.b.) and temperature (20-90

87 gnocellulosic (bamboo) fiber cell walls with moisture content (MC).

88 mol/mol (a 37.5 +/- 7.4% reduction) with 20% moisture content and 0.9 water activity.

89 A site-specific relationship between moisture content and electrical conductivity data was de

90 d interesting physical properties with lower moisture content and higher spread factor than those mad

91 of this study was to evaluate the effects of moisture content and storage temperature on the percenta

92 acetylated high amylose starches had higher moisture content and water solubility than the native hi

93 All rice genotypes were stored at 13% moisture content at temperatures of 16, 24, 32, and 40 d

94 ainly through circulation change rather than moisture content change.

95 Moisture content decreased as the size of the granules d

96 hort-term C mineralization than current soil moisture content in these soils.

97 Moisture content increased (6-11% dmo), while soluble so

98 gst all treatments, conditioning grains to a moisture content of 14% for 30min was found to be optimu

99 The moisture content of beta-cyclodextrin/Danube fish oils c

100 The equilibrium moisture content of bulgur increased both with decreasin

101 time, number of freeze-thaw cycles, and the moisture content of coal were studied using combined uni

102 Higher moisture content of food matrices did not substantially

103 ali of the waste from 0.66 to <0.01M and the moisture content of the pulp increased from 93% to 97% (

104 Finally the effect of the moisture content on furfuryl alcohol formation was found

105 sorbitol solution for 24h and adjusting the moisture content to 25% before HMT (100 degrees C, 1h).

106 e DW periods and they ranged from a constant moisture content treatment, to a one day drying (low-dry

107 Results showed that (a) change in soil moisture content was linearly correlated to change in el

108 The moisture content was significantly lowered after beta-CD

109 ourdough technology allowed increasing crumb moisture content with no significant variations during s

110 , 40, 915 or 2450 MHz and sample temperature/moisture content with R(2) greater than 0.967.

111 coefficient), water status (water activity, moisture content) and molecular mobility by (1)H Nuclear

112 Particles (77-83% moisture content) were conditioned in acidified solution

113 ls increased with increasing temperature and moisture content, and largely enhanced at higher tempera

114 acteristics of the obtained powder including moisture content, bulk density, wettability, morphology,

115 ion pretreatment substantially decreased the moisture content, duration of the drying process, and th

116 D (5-20%) concentration on product recovery, moisture content, hygroscopicity, curcuminoids encapsula

117 as followed by the addition of water (13-17% moisture content, MC) or absolute ethanol (1:1, 1:2, 1:3

118 ences in the total running time, equilibrium moisture content, sorption hysteresis and sorption kinet

119 died, freeze-thaw damage resulting from high moisture content, was restricted by the coal's moisture

120 tion of drying process in terms of physical (moisture content, water activity, total color change, fi

121 all of the three powders exhibited increased moisture content, which was consistent with an increase

122 sing with increasing storage temperature and moisture content.

123 torical maples exhibited reduced equilibrium moisture content.

124 ned by gas chromatography and the decline in moisture content.

125 s produced from amorphous alpha-CD powder at moisture contents (MC) close to or higher than the criti

126 yzer at frequencies between 10 and 3000 MHz, moisture contents between 4.2% to 19.6% w.b. and tempera

127 ce condensed systems that covered a range of moisture contents from 7.34% w/w (23% relative humidity)

128 I, CNC II, CNF I, and CNF II had equilibrium moisture contents of 21.4, 28.6, 33.2, and 38.9%, respec

129 hts can guide the optimal selection of final moisture contents to advance dry preservation methods.

130 GPLLJs transport heat and moisture, contribute to thunderstorm and severe weather

131 framework (MOF), with dual functionality for moisture control within the recommended range of relativ

132 cutoff scale, controlled by the interplay of moisture convergence variance and precipitation loss, te

133 the fermented and malted biscuits had higher moisture, crude protein, crude fiber and energy value wi

134 Moisture decreased with darker roast color, while the to

135 Annual moisture deficits were significantly greater from 2000 t

136 Changes in moisture delivery are driven by complex interactions bet

137 d that historical rainfall controls both the moisture dependence and sensitivity of respiration.

138 roximately 153 ppm was found to be extremely moisture dependent.

139 ink degree/gradient of the film to allow for moisture-dependent changes of modulus and swelling degre

140 the presence of clouds, of proxies for soil moisture derived from the amplitude and phase content of

141 bes the primary differences between the soil moisture desorption and the adsorption processes by the

142 Effective moisture diffusion coefficients (Deff) were calculated b

143 experimental procedure to accurately measure moisture diffusivity based on thermogravimetric approach

144 Accurate description of moisture diffusivity is key to precisely understand and

145 Unfortunately, measuring moisture diffusivity is not trivial, especially at low m

146 n to a point where the available atmospheric moisture does not suffice anymore to release the latent

147 r CO2 efflux was largely explained by litter moisture driving microbial degradation and ultraviolet r

148 to the extreme snowfall inducing higher soil moisture during spring thaw.

149 int toward a sustained increase in effective moisture during the event, however the magnitude of chan

150 ivity imaging (ERI) was used to monitor soil moisture dynamics to a depth of 9 m in a grassland, a gr

151 effect of climate change in regulating fuel moisture (e.g. warmer conditions increasing fuel dryness

152 ependent mortality as well as soil or litter moisture effects on leaf turnover or fire.

153 The screw profile and moisture feed content had the most significant impact on

154 Fuel moisture, firepower and MCE fluctuation effects on stove

155 due to the superposition of slowly-changing moisture fluxes, mainly supported by increased hygrometr

156 Although it is a low-moisture food, raw flour can be a vehicle for foodborne

157 semi-dry foods (aw approximately 0.5), high moisture foods (aw approximately 1) and liquid foods (aw

158 nherently hygroscopic, that is, they take-up moisture from the air, which affects the extent to which

159 This process was driven by the secretion of moisture from the sweat glands, since increased hydratio

160 that calibrating models with parabolic soil moisture functions can improve predictive power over sim

161 ctions and biomass while manipulating a soil moisture gradient and reducing consumer pressure.

162 from three forest dynamics plots spanning a moisture gradient in Panama that have experienced El Nin

163 tions did not vary systematically across the moisture gradient under nondrought conditions, woody mor

164 ssociated with high rates of evolution along moisture gradients and between the evergreen and deciduo

165 nditions, and that their distributions along moisture gradients can be used to predict their drought

166 profile of roots monitored at control and 4 moisture gradients regimes showed the up-regulation of 1

167 drolase gene (XET) up-regulated at different moisture gradients, was cloned and expressed in tobacco.

168 ifornia with severely reduced snowpack, soil moisture, ground water, and reservoir stocks, but the im

169 Predicted soil moisture, groundwater depth and leaf area index agreed w

170 y the time of the second peak, however, soil moisture had dropped to anomalously low levels in the co

171 Global warming increases the moisture holding capacity of the atmosphere and conseque

172 allowed to obtain a dried material with 12% moisture in 43min when 550g of broccoli by-products were

173 mplement under industrial conditions because moisture in combustion exhaust streams blocks oxidation

174 pressure deficit, and increased surface soil moisture in higher diversity communities.

175 n of both oceanic and terrestrial sources of moisture in models for simulating the intraseasonal vari

176 dendroecology to elucidate the role of soil moisture in modifying the relationship between climate a

177 that UCI is caused by lack of vegetation and moisture in non-urban areas relative to cities.

178 odels is that soil microorganisms respond to moisture in the same way, regardless of location or clim

179 n on the spatio-temporal variability of soil moisture in the vadose zone is important to assess groun

180 of a series of optical devices triggered by moisture, including anticounterfeit tabs, encryption dev

181 WPC and moisture increased crystallinity, but only WPC increased

182 Increasing bean flour and processing moisture increased density and hardness while decreasing

183 WPC and feed moisture increased redness, yellowness and decreased lum

184 ity, defined as the slope of respiration vs. moisture, increased fourfold across a 480-mm rainfall gr

185 These direct and indirect effects of moisture indicate that future changes in precipitation a

186 main stability failure routes related to the moisture-induced poly(3,4-ethylenedioxythiophene) aggreg

187 nforest, which strongly enhances atmospheric moisture inflow from the Atlantic.

188 Because soil moisture integrates temperature and precipitation dynami

189 The inferred temporal evolution of soil moisture is remarkably consistent between independent, o

190 ally available moisture and the frequency of moisture-laden depressions from the Bay of Bengal have a

191 ication, offering the desired control of the moisture level at room temperature, have yet to be explo

192 showed similar proton distributions at a 44% moisture level, although the chemical composition of coa

193 om ecosystems under C3/C4 plant rotations at moisture levels at and above field capacity over 5 month

194 iles of RF heated almond kernels under three moisture levels were made using experiment and computer

195 d largely enhanced at higher temperature and moisture levels.

196 possibly due to lack of temperature-induced moisture limitation in mesic habitats.

197 However, it retarded the increase in moisture loss and maintained both flesh and pulp colour

198 crobial growth, reducing lipid oxidation and moisture loss, and functioning as a carrier of food addi

199 generally reported for bread staling (crumb moisture loss, decrease in frozen water content, formati

200 of the Mediterranean coast; and earlier soil moisture maxima have led to earlier winter floods in wes

201 Counter to theory, elevated moisture may significantly accelerate C losses from mine

202 inimalist plant hydraulics model with a soil moisture model and, for the first time, translate rainfa

203 tively with amino acids in both high and low moisture model systems.

204 order; kCysteine>kArginine>kLysine for high moisture model systems.

205 d (high moisture) and Coffee-amino acid (low moisture) model systems at 5, 25 and 50 degrees C.

206 We find that the oceanic sources of moisture, namely western and central Indian Oceans (WIO

207 ironmental factors, including levels of soil moisture, nitrate, chloride, and labile organic carbon,

208 assware without rigorous exclusion of either moisture or oxygen, and use trifluoroacetic acid as a st

209 physicochemical parameters of honey samples (moisture, pH, total acidity, ash, dry matter, and qualit

210 Moisture-powered potential switching is achieved by esta

211 riven responses are further mediated by soil moisture, precipitation, and carbon supply and regions i

212 nd influenced the temporal evolution of soil moisture profiles; and (c) juniper encroachment lowered

213 act (6%) had a significant effect on the pH, moisture, protein, fat, fiber, instrumental color values

214 The moisture pulse experiment showed that high N soils had h

215 tability is regulated by shifting low-energy moisture reactions to high-energy ones due to As.

216 important in facilitating continental-scale moisture recycling but are poorly understood at regional

217 scale, and find that it is associated with a moisture recycling mechanism, rather than the classic al

218 tivity and rainfall, indicative of amplified moisture recycling.

219 ly determined by the recycling rate of local moisture, regulated by planetary circulation patterns as

220 The respiration-moisture relationship was resistant to environmental cha

221 and indirect climate change effects on soil moisture requires better understanding.

222 ing LSM-modeled and topography-mediated soil moisture, respectively.

223 Moisture response functions for soil microbial carbon (C

224 d by these tunable responses, three types of moisture-responsive wrinkle dynamics are achieved, for t

225 tional standard of care protocols, involving moisture-retentive occlusive dressing, or standard of ca

226 isture content, was restricted by the coal's moisture saturation limit.

227 ological responses (evapotranspiration, soil moisture, seasonal and annual streamflow, and water stre

228 uction of fluorinated amines rely on air and moisture sensitive reagents that require special handlin

229 ver, these have required the use of air- and moisture-sensitive catalysts and reagents, limiting both

230 -) salts were isolated for the first time as moisture-sensitive solids that decompose at temperatures

231 Moisture sensitivity, defined as the slope of respiratio

232 Watering increased season-average soil moisture similarly across sites.

233 ly positively correlated with rainfall, soil moisture (SM), the carbon to nitrogen ratio (C/N ratio),

234 relevant to diffusion into soils (i.e., soil moisture, snow depth, snow density).

235 bal scale by linking global datasets of soil moisture, soil temperature, primary productivity, and so

236 that realistic land conditions such as soil moisture/soil temperature (SM/ST) can significantly impr

237 At least 66% of gross high moisture solids and 23% of gross low moisture solids can

238 , and this fraction increases to 99% of high moisture solids and 55% of low moisture solids if waste

239 ss high moisture solids and 23% of gross low moisture solids can be treated using existing county inf

240 o 99% of high moisture solids and 55% of low moisture solids if waste can be shipped anywhere within

241 Changes in carbohydrate composition, moisture, soluble solids, acidity, total polyphenol cont

242 isotherm experiments to investigate dynamic moisture sorption and desorption in markedly different m

243 umn through early winter air temperature and moisture source changes in East-Central Europe for the H

244 l as a temperature change, but as a shift in moisture source, suggesting weaker westerlies and increa

245 Changes in the proportion of moisture sourced from the Arctic with sea ice change in

246 driven by complex interactions between ocean moisture sources and atmospheric circulation modes, maki

247 articularly interesting due to their air and moisture stability and high functional group tolerance.

248 Improved moisture stability is regulated by shifting low-energy m

249 diazolium perchlorate salts showed excellent moisture stability, an unusual feature in compounds of t

250 significantly improved chemical, thermal and moisture stability, and excellent solution processabilit

251 arenes and alkynes-along with their air and moisture stability, has established them as an important

252 1.46 mS cm(-1) at 25 degrees C and enhanced moisture stability.

253 th 1, 2, and 3 phenylene rings, we construct moisture-stable Ni-MOF-74 members with adjustable pore a

254 Using only robust air- and moisture-stable reagents and pre-catalysts, both known a

255 hod for the synthesis of POEs using air- and moisture-stable vinyl acetal precursors is presented.

256 ading the contact, regardless of the initial moisture state of the finger and of the normal force app

257 However, after 25 days, elevated moisture stimulates cumulative gaseous C-loss as CO2 and

258 activity, warming temperatures and increased moisture stress on plants.

259 e, ER increases year-round in the absence of moisture stress resulting in net CO2 uptake increases in

260 Thus, even without moisture stress, net CO2 uptake of boreal forest-wetland

261 neotropical forests suggests that increasing moisture-stress is indeed likely to drive significant ch

262 iments with changed inputs, temperature, and moisture suggest that uncertainty associated with freeze

263 explained by a critical balance between soil moisture supply and atmospheric demand representing rela

264 rly in the northwestern United States, where moisture supply and ecosystem processes are highly sensi

265 Cool-season moisture supply and snowpack responded strongly to storm

266 lies over the Arabian Sea, driving surges of moisture supply, leading to extreme rainfall episodes ac

267 annual plant community at all levels of soil moisture through reductions in microclimatic stress in b

268 e South American Low Level Jet that delivers moisture to southeastern South America.

269 er the tropical Pacific that transports less moisture to the ASM region and subsequently reduces ASM

270 on of aldehydes and ketones, and for related moisture-tolerant hydrogenation.

271 Moisture, total phenolics, reducing sugar and B vitamins

272 y is key to precisely understand and predict moisture transfer behaviour in a matrix.

273 ch can be crucial to ensure good accuracy of moisture transfer description/prediction especially when

274 en the Amazon rainforest and the atmospheric moisture transport from the Atlantic to the South Americ

275 during the active periods results in a high moisture transport from the Bay of Bengal and GB into th

276 We suggest that changes in eastward moisture transport from the North Atlantic are the prima

277 Here, we study moisture transport from the oceanic and terrestrial sour

278 Despite the importance of precipitation and moisture transport over the Tibetan Plateau for glacier

279 Changes in the pasting profiles of heat-moisture treated starches were more obvious when glycero

280 tudy was to evaluate the effects of the heat-moisture treatment (HMT) applied to paddy rice grains on

281 ntration of plasticizers applied during heat-moisture treatment (HMT) on the properties of canna star

282 acorn starch were mostly influenced by Heat-moisture treatment (HMT).

283 ogeneity in three environmental factors-soil moisture, understory light, and conspecific neighborhood

284 Moisture uptake and outgassing can be detrimental to a s

285 levated temperatures (>70 degrees C) and low moisture values (>1%).

286 iffusivity is not trivial, especially at low moisture values and/or elevated temperatures.

287 geneity by aggregating factors that increase moisture variability within and across biomes.

288 ographic tradeoffs driven by short-term soil moisture variation act as a mechanism to allow multiple

289 ics and topographic convergence-induced soil moisture variation to land surface models (LSM) can help

290 Texture, aw and bread moisture varied according to a first-order kinetic model

291 icting plant hydraulic safety loss from soil moisture was developed using field measurements and a pl

292 dfires disproportionally occurred where fuel moisture was higher than lightning-started fires, thereb

293 age when nonnative biomass was high and soil moisture was low.

294 ic anthocyanin, antioxidant activity, color, moisture, water activity (aw), solubility, hygroscopicit

295 The minimal changes observed in moisture, water activity and texture of the samples, cou

296 pret this as being related to an increase in moisture which is partially mitigated by weakening circu

297 We focus on respiration responses to soil moisture, which remain unresolved in ecosystem models.

298 vels and lipid content and thus reduced skin moisture with an increase in archaeal signatures.

299 e) and protein solubility (24.8% with 15% of moisture) with increased emulsifying capacity (52.2% wit

300 We argue that models should treat soil moisture within a three-dimensional framework emphasizin