ライフサイエンスコーパス: moisture

1 raits grain yield, number of ears, and grain moisture.

2 e system's sensitivity towards environmental moisture.

3 ted with bacterial diversity only under high moisture.

4 line under changing light intensity and soil moisture.

5 brid organic-inorganic perovskite devices by moisture.

6 water connections, a primary control on soil moisture.

7 es allowed us to disentangle temperature and moisture.

8 s it shows negligible sensitivity toward air/moisture.

9 ost of these materials is the sensitivity to moisture.

10 31%, predominantly driven by changes in soil moisture.

11 perovskite delta-CsPbI(3) in the presence of moisture.

12 an efficient plasticizer at least as high as moisture.

13 g, likely via an associated decrease in soil moisture.

14 eaction setup or equipment to exclude air or moisture.

15 edjaggery was found to equilibrate at higher moisture.

16 h dynamics during drought and return of soil moisture.

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

18 it showed high dietary fibre (36.9%) and low moisture (10.0%) contents which justify its hardness and

19 ar increase in the duration of elevated soil moisture (2-22 days) with increasing event size.

20 ntinuous illumination stability and improved moisture (55-60%) and thermal (85 degrees C) tolerances.

21 Here, a super moisture-absorbent gel, which is composed of hygroscopic

22 Moisture adsorption isotherms showed improved water adso

23 ctivity, which are an important mechanism of moisture advection from subtropical to extra-tropical re

24 s in the atmospheric vertical and horizontal moisture advections.

25 ug/kg) was observed at 200 degrees C and 5% moisture after 40 min.

26 ents and exhibit remarkable stability toward moisture, allowing for benchtop transformations without

27 Everywhere that moisture and a carbon source coexist in the terrestrial

28 ummer that corresponded to snow melt-derived moisture and a transition from winter dormancy to spring

29 11.8 g, firmness ranged from 7.3 to 20.1 N, moisture and ash contents ranged from 75.1 to 88.6% and

30 to be populated with protons as a result of moisture and carbon dioxide adsorption from the air.

31 was maximized under conditions of high soil moisture and evaporative demand, and may be reduced in s

32 n the laboratory with standard temperatures, moisture and excess carbon substrate, to allow physiolog

33 Our results suggest a regional increase in moisture and expansion of woody vegetation prior to mode

34 of the Asian monsoon, supporting a role for moisture and heat transport from low latitudes in North

35 commercialized because they are sensitive to moisture and heat.

36 anspiration, thereby reducing available soil moisture and impairing soil fertility.

37 en Arctic waters also increase the source of moisture and increase autumn snowfall over Siberia, insu

38 air temperature in winter and proceeding to moisture and leaf area during the summer.

39 damage of the enriched batches or affect the moisture and lipid content during processing and/or culi

40 soil microbiome responded to changes in soil moisture and nutrient conditions and to determine which

41 t only serve as thick and dense barriers for moisture and oxygen but also increase the crystal format

42 te a strong resistance to intercalation with moisture and oxygen.

43 (N(2)) in arable soils include high nitrate, moisture and plants; we investigate how differences in t

44 solubility of carbon dioxide (CO(2)) in the moisture and protein components of cheese matrices and t

45 that ground-nesting reptiles can assess soil moisture and respond by adjusting the depth of the nest,

46 from snowmelt peak streamflow, thus reducing moisture and safe sites for dominant tree recruitment.

47 e model was capable of predicting accurately moisture and temperature distributions along with heath

48 erimental set-up; direct measurement of soil moisture and temperature during the study period; amount

49 adient is likely due to the tradeoff between moisture and temperature with changing depth; most groun

50 e that strong negative coupling between soil moisture and vapor pressure deficit occurs globally, ind

51 In artistic oil paintings, ambient moisture and water and organic solvents used in conserva

52 tats varying in their exposure to radiation, moisture and wind (e.g. topography, radiative forcing or

53 t and possess limited richness in arid (< 5% moisture) and at high elevation sites, known drivers of

54 s such as cooccurring soil drought (low soil moisture) and atmospheric aridity (high vapor pressure d

55 turbulent transport of properties like heat, moisture, and carbon.

56 We continuously monitored soil temperature, moisture, and CO(2) for a three-year period (2015-2017),

57 conditions without precautions toward air or moisture, and is tolerant of nearly all common functiona

58 The impacts of sea-surface temperature, soil moisture, and leaf area index are quantified and found t

59 values, whereas it reduced b* and L* values, moisture, and linolenic acid content of sesame seeds fro

60 t no studies have examined Holocene sea ice, moisture, and ocean-atmosphere circulation in Arctic Ala

61 ompounds from harsh conditions (e.g., light, moisture, and oxygen) and biological destruction (enzyme

62 ochemical properties (bulk density, texture, moisture, and pH), plant and microbial characteristics (

63 specialized ligands, sensitivity to air and moisture, and so-called "transition-metal-residue issue"

64 cted by complex interactions of temperature, moisture, and substrate supply, which are further compli

65 ication costs, thermal drift, sensitivity to moisture, and the limited applicability for users with m

66 eaction rates (<4 h), compatibility with air moisture, and the use of inexpensive commercial reagents

67 ivity to carbon dioxide concentrations, soil moisture, and vapor pressure deficit, the impact of temp

68 ibution of isotopically heavy Arctic-derived moisture, and wetter climate.

69 ents of plant traits such as relative canopy moisture are providing early-warning signals that predic

70 primarily limited by current growing season moisture, as opposed to temperature or sunlight, but add

71 iWUE plateaued after 1975, driven by greater moisture availability and a changing soil biogeochemistr

72 ant c(a) - c(i)) in response to rising c(a), moisture availability and site conditions over 111 yr.

73 ecies-poor forests increased more as climate moisture availability decreased than it did in species-r

74 hat the reduction in GPP/SIF with decreasing moisture availability may be related to stomatal respons

75 precipitation seasonality and growing season moisture availability were correlated to aspects of root

76 PP responses to warming, leaf area index and moisture availability were the best predictors of annual

77 from stable isotopes did not vary with soil moisture availability, potentially indicating remobiliza

78 n abiotic conditions such as temperature and moisture availability.

79 idity because they are tightly controlled by moisture availability.

80 they each capture variation in WUE with soil moisture availability.

81 sponses to competition differed depending on moisture availability.

82 serve as following functions: (a) absorbing moisture; (b) uptaking water; (c) cleaning the body surf

83 However, existing moisture-based energy-harvesting technologies can produc

84 best explained as a plastic response to soil moisture, because differences in both the mean and varia

85 Soil moisture behaviour in most models is constrained by hydr

86 An atmospheric moisture budget analysis shows that these enhanced seaso

87 Existing earth system models represent soil moisture but simplify groundwater connections, a primary

88 Fat and moisture can be estimated with the global model in a wid

89 Soil moisture can feed back on rainfall through the impact of

90 lationships between temperature, atmospheric moisture capacity, and extreme precipitation intensity t

91 , fire weather conditions, ecozone, and soil moisture class.

92 without TLE addition were characterized for moisture, color, refractive index, fatty acid compositio

93 iotic factor) with different temperature and moisture conditions (abiotic factors) to manipulate micr

94 with increase in temperature and decrease in moisture conditions across the South-North gradient and

95 bacterial and fungal necromass under optimum moisture conditions at 10 degrees C, 15 degrees C, and 2

96 f carbon cycle sensitivity to temperature on moisture conditions, is emerging as key regulators of th

97 wth on wood and straw subjected to different moisture conditions.

98 ences in pore structure between genotypes or moisture conditions.

99 ivers shaping peatland community and surface moisture conditions.

100 tion of this response depended on antecedent moisture conditions.

101 reenness under droughts relative to baseline moisture conditions.

102 en carbon accumulation rate and peat surface moisture conditions: under dry conditions, less carbon w

103 0 degrees C), screw speed (SS: 200-300 rpm), moisture content (MC: 10-20%, wb), and defatted soy flou

104 A significant higher MEE and lower moisture content and hygroscopicity was observed in spra

105 Decrease in amylose and moisture content and increase in swelling index and solu

106 predictor of methanogen abundance, but wood moisture content and pH were also significant predictors

107 al changes of wood exposed to a variable air moisture content and potentially reduces wood biodegrada

108 clearly illustrate the impacts of substrate moisture content and prior history (e.g. whether germina

109 The moisture content and successful of molecular encapsulati

110 Moisture content and water activity values of SPI powder

111 act angle but decreased elongation at break, moisture content and water vapor permeability.

112 gates can be controlled by manipulating feed moisture content during extrusion, with 49.3% feed moist

113 d plant height, but negatively correlated to moisture content in fresh stalk and potential grain yiel

114 Moisture content in fresh stalk range from 33.7 to 74.4%

115 ty were determined to be 190 degrees C, leaf moisture content of 5%, and aqueous ethanol concentratio

116 anning calorimetry analyses reveals that the moisture content of CD/CNO complexes significantly decre

117 premature death; however, the effect of fuel moisture content on air pollutant emissions from solid-f

118 mpact of organic matter content, soil pH and moisture content on the dissolution rate and solubility

119 el forming behaviour, whereas 30.0 and 60.0% moisture content resulted in complete protein denaturati

120 The cheeses made using CpCP3 showed higher moisture content than those made with chymosin, but prot

121 oved, a close relationship of g(1) with soil moisture content was observed.

122 l under semiarid conditions with gravimetric moisture content ~12.5 +/- 2.4%.

123 Water activity, moisture content, and pH differences did not sufficientl

124 also evaluated for swelling, biodegradation, moisture content, in-vitro aerodynamic performance, and

125 inties (e.g., static GWP values, decay rate, moisture content, or gas collection efficiency) generall

126 dosed into standard LUFA soils with various moisture content, pH and organic carbon content.

127 with both increasing temperature and salt-in-moisture content, whereas solubility of CO(2) increased

128 d for the prediction of protein, gluten, and moisture content.

129 ructural rearrangement as a function of feed moisture content.

130 lled water or maltose solution to the native moisture content.

131 cess effectively improved dewatering of high moisture-content foods with positive impacts on process

132 ein isolate was texturized at different feed moisture contents (30.0, 49.3, and 60.0%) at a constant

133 ere applied to goosegrass maintained at soil moisture contents (VMC) of < 12%, 12 to 20%, or > 20%.

134 showed excellent powder characteristics with moisture contents ranging from 3 to 6%, water activity o

135 were realized after certain drying times and moisture contents.

136 tree density increased, but increasing fuel moisture contributed.

137 ature effects, we know little about how soil moisture contributes to successful hatching and particul

138 Soil moisture declined significantly in 8% of the area.

139 vere droughts and heatwaves because low soil moisture decreases both evaporation and plant transpirat

140 However, when soil moisture decreases, a higher proportion of old soil C is

141 tify a north-south dipole in annual climatic moisture deficit anomalies across the Interior West of t

142 re coupling, associated with persistent soil moisture deficit, appears to intensify surface warming a

143 following 15 years of experimentally imposed moisture deficit.

144 t-induced mortality following long-term soil moisture deficit.

145 dback acts to amplify precipitation and soil moisture deficits in most regions.

146 c changes that increase soil and atmospheric moisture deficits.

147 vskite/HTM interface helps in overcoming the moisture degradation of the hygroscopic perovskite layer

148 Moisture delivery in California is largely regulated by

149 gulated by stomatal responses to atmospheric moisture demand D and soil water availability W, but the

150 prediction maps demonstrated a more uniform moisture distribution in MVD ginger slices than that in

151 models can close the loop of satellite soil moisture downscaling for local applications such as agri

152 mulations needed to minimize the deleterious moisture effects on long-time deformations, cracking dam

153 much steeper than literature values for soil moisture effects on photosynthesis and stomatal conducta

154 lity for oceanographic applications and soil moisture estimation, microwave remote sensing observatio

155 rature in the presence of elevated levels of moisture expected with the use of membrane inlets or hea

156 the Sierra Nevada Mountains due to tropical moisture exports) and regions where multiple extreme flo

157 ntain their porosity and crystallinity after moisture exposure, important molecular-level structural

158 metal-organic framework that is stable after moisture exposure, what are the reversible, loading-depe

159 a systematic observational analysis of soil moisture feedbacks on propagating MCSs anywhere in the w

160 ironmental factors such as high temperature, moisture, flexibility and water resistivity has been inv

161 the present understanding, enhanced heat and moisture fluxes from high lead concentrations tend to pr

162 ution suggests the importance of pre-monsoon moisture for growth of the dominant vegetation, Himalaya

163 -based reconstructions of heatwaves and soil moisture for the past 260 years reveal an abrupt shift t

164 high fabrication cost (high temperature, air/moisture-free conditions), thereby limiting their device

165 with a control model with an empirical soil moisture function, the profit maximization model improve

166 nosZ showed a U-shape relationship with soil moisture; further insight into biotic mechanisms underly

167 ight old-growth forest sites across a strong moisture gradient in the western USA to retrospectively

168 is energy generation to be a self-maintained moisture gradient that forms within the film when the fi

169 This suggests that at the dry end of the moisture gradient, availability of water regulates carbo

170 2) exchange in winter and spring, while soil moisture has a primary control on net CO(2) exchange in

171 However, moisture hypersensitivity has made their manufacture com

172 aneous hydrolysis reactions of sulfides with moisture in air lead to the release of toxic hydrogen su

173 Moisture in materials can be a source of future outgassi

174 Thus, a 50% reduction of moisture in the grapes was observed after 10 min while s

175 ich decreased proportionally with increasing moisture in the HMT.

176 al scale and an asymmetric supply of oceanic moisture, in which the maximum values are located over t

177 We found that soil moisture increased under deepened winter snow in early g

178 parent, self-adhesive, breathable, flexible, moisture-insensitive, and able to maintain their accurac

179 olling environmental humidity level and thus moisture interaction with an electrospinning solution je

180 separate the impacts of temperature and soil moisture into direct effects and indirect effects throug

181 rd, extraction of the ubiquitous atmospheric moisture is a powerful strategy allowing for decentraliz

182 Atmospheric moisture is a ubiquitous water resource available at any

183 der two different conditions, where the fuel moisture is high and where it is low.

184 ason when vegetation is desiccated, and soil moisture is high.

185 moisture, shown here is that the presence of moisture is key in favoring formation of the target phen

186 rved that, AP helps to maintain temperature, moisture level and microbial and quality control of the

187 50-100 IJs cm(-2) in combination with 10-15% moisture level showed optimal results against C. capitat

188 individual ketones should be made at a fixed moisture level.

189 with increasing vegetation cover (NDVI) and moisture levels (NDWI), whereas the diversity of parasit

190 Moisture levels entering this DMS analyzer employed as a

191 Different soil textures and moisture levels resulted in a significant variation in E

192 nder naturally varying temperatures and soil moisture levels were remarkably insensitive in terms of

193 ng species at 0.06 and 0.042 m(3) m(-3) soil moisture levels.

194 t and restricted to species that experienced moisture limitations.

195 The net CO(2) exchange was generally more moisture limited in the boreal region than in the Arctic

196 cooking methods seemed mainly linked to the moisture loss increasing meat fat content and the culina

197 respiration rate [RR], colour and moisture loss) and biochemical profile (viz.

198 conditions), and improved technological (no moisture loss, lower proteolysis and organic acid conten

199 r,H,Cs,Na-X, shows superior stability toward moisture, maintaining its initial luminescence propertie

200 optoelectronic/photovoltaic devices against moisture, more interesting properties and device applica

201 position rate was negatively correlated with moisture niche width (an indicator of drought stress tol

202 ability, whereby fungi with wide thermal and moisture niches exhibit lower displacement ability.

203 is constantly changing due to shifts in soil moisture, nutrient availability and other conditions.

204 y were subjected to different levels of soil moisture, nutrient supply and intramorph and intermorph

205 t 170, 200 and 230 degrees C until the final moisture of 5%.

206 However, the contribution of recycled moisture of continental origin to I and Se to precipitat

207 The ubiquity of atmospheric moisture offers an alternative.

208 coordination when soil microbiomes cope with moisture or nutrient perturbations.

209 g to resolve whether ANPP(stem) is primarily moisture- or energy-limited and whether climate sensitiv

210 Soil moisture, organo-Al, and reactive Fe explained most of t

211 s of current and future temperature and soil moisture over decadal timescales.

212 ct as protective barriers against oxygen and moisture penetration.

213 ative recombination by 40%, while minimizing moisture permeation.

214 ause the hydrophobic DMIMPF(6) layer blocked moisture permeation.

215 Moisture, phenolic compounds, thiamin, niacin, and tocop

216 ifically, we found stem growth stops at soil moisture potentials of -0.47 MPa for larch and -0.66 MPa

217 In addition, the soil moisture-precipitation feedback acts to amplify precipit

218 of grey level co-occurrence matrix (GLCM) of moisture prediction maps demonstrated a more uniform moi

219 ection on textural structure of cake by high moisture preservation ability.

220 Extrusion at 49.3% feed moisture produced texturized mung bean protein (TMBP) wi

221 re content during extrusion, with 49.3% feed moisture prompting favourable partial denaturation to pr

222 AM were 51.89%, 15.62%, 20.21% and 2.47% for moisture, protein, fat and ash, respectively.

223 haracteristics (a*, b*, and L* values), ash, moisture, protein, oil, total phenolic, and antioxidant

224 esses are largely dependent on distinct soil moisture pulses.

225 if coupled to snow drought and earlier soil moisture recession, but summer precipitation changes rem

226 nd dried the lower atmosphere, which reduced moisture recycling and resulted in increased drought ext

227 ), restrict uptake of water to conserve soil moisture (reduced hydraulic conductance, narrow metaxyle

228 ety of ways (reduced precipitation, low soil moisture, reduced streamflow, etc.), but relatively few

229 f dried paprika was found to increase due to moisture reduction, inactivation of peroxidase, and the

230 This coordinated temperature and moisture regulation can be explained by "law of minimum,

231 l respond to variation in vegetation or soil moisture remains unknown.

232 n to flexibility (5 mm radius of curvature), moisture resistance (100 washing cycles), and strength (

233 vironmental stabilities (e.g., UV, heat, and moisture resistance).

234 This method also circumvents the use of moisture-sensitive organometallic reagents.

235 ast to literature reports suggesting general moisture sensitivity, a subset of Bcat products resultin

236 hium (Li)-ion batteries, but it suffers from moisture sensitivity, side reactions, and gas generation

237 erovskites show low phase stability and high moisture sensitivity.

238 ility of organolithium reagents with air and moisture, shown here is that the presence of moisture is

239 tified pre- and postdeluge responses in soil moisture, soil respiration, and canopy greenness, as wel

240 usive gas transport to explain observed soil moisture, soil temperature, and soil CO(2) concentration

241 e scale-independent physics and chemistry of moisture sorption and diffusion materials.

242 The ability to quantify moisture sorption and diffusion, independent of scale, u

243 Moisture sorption studies, Karl Fischer titration, and d

244 cycle in this region is driven by a shift in moisture source from the Indian Ocean to the South China

245 systems to simultaneously achieve desirable moisture stability and electrochemical stability, and pr

246 ace and/or grain boundaries, and enhance the moisture stability of the perovskite film.

247 ect of cations, anions, and Li/Na content on moisture stability.

248 The recent observation that the air- and moisture-stable amino-cyclophosph(V)azanes of the type [

249 rried out at room temperature using air- and moisture-stable forms of the catalyst, with loadings as

250 The isolated air- and moisture-stable Ru(II)-NHC-diamine complexes act as vers

251 Here we report an air- and moisture-stable, visible light-absorbing Zr(IV) photosen

252 rong link between dry line dynamics and soil moisture state.

253 und that plants transmit information on soil moisture status through their influence on the vapor pre

254 ptivity or runoff rate/amount, but increased moisture storage (+14%).

255 ion declined most (-56%) at fine scales, and moisture storage was greatest (+36%) at large scales.

256 me of runoff) and two hydrological outcomes (moisture storage, sediment production).

257 different environmental drivers (increase in moisture stress and atmospheric CO(2) concentrations): m

258 growth and reproduction under conditions of moisture stress and elevated CO(2) in the absence of her

259 plication on plant survival and growth under moisture stress and elevated CO(2) respectively.

260 of other environmental factors such as soil moisture stress are not fully understood and are therefo

261 mean LAI and LAI seasonality across the soil moisture stress gradient maximised NCE, and were therefo

262 rial ecosystem model to seven plots across a moisture stress gradient with detailed in situ measureme

263 ication of such small regulatory RNAs in low moisture stress hardy crops can help in cross species tr

264 miRNAs to demonstrate their role in deficit moisture stress tolerance mechanism of horsegram variety

265 response function, with an intercept at zero moisture stress, used in growth simulations reproduced 6

266 onal dynamics and leaf traits vary with soil moisture stress.

267 In low moisture substrates a steep increase in associated heter

268 Hydroclimate, the interplay of moisture supply and evaporative demand, is essential for

269 mechanism: physisorption, chemisorption, and moisture-swing sorption.

270 ear tree-ring reconstructions of summer soil moisture to demonstrate that the 2000-2018 SWNA drought

271 ear-independent gradients in temperature and moisture, to disentangle the effects of climate, soil pr

272 Different moisture-to-protein levels were achieved by freeze-dryin

273 as observed between CO(2) solubility and the moisture-to-protein ratio of experimental samples.

274 s methodology is general, simple, oxygen and moisture tolerant, high-yielding, totally chemo- and ste

275 analysis of finger millet genotypes revealed moisture, total carbohydrate, protein, fat, fiber and as

276 Protists are structured by moisture, total N and distance from the local coast and

277 more humid atmosphere will lead to enhanced moisture transport due to, among other factors, an inten

278 g of midlatitude Westerlies, while low-level moisture transport intensified by global warming has fav

279 e the effect of sample size and shape on the moisture transport phenomena through a combined experime

280 rier spring conditions resulting from weaker moisture transport.

281 can be explained by changes in both heat and moisture transport.

282 Functional properties of infrared heat-moisture treated (HMT) maize meal with stearic acid were

283 to two different modifications such as heat-moisture treatment (HMT) and citric acid treatment (CAT)

284 s study investigated the association of heat moisture treatment (HMT) with high hydrostatic pressure

285 The effect of heat moisture treatment (HMT), annealing (ANN), and dual retr

286 These anomalous moisture uptake (AMU) locations are identified on a glob

287 cipitation from central Vietnam by combining moisture uptake calculations with monthly stable isotope

288 However, the influence of soil-moisture variability and trends on the long-term carbon

289 Subseasonal and interannual soil-moisture variability generate CO(2) as a result of the n

290 hether the dominant driver is temperature or moisture variability, their interaction,that is, the dep

291 Soil moisture was computed in a thin upper layer and an under

292 egadrought-like trajectory of 2000-2018 soil moisture was driven by natural variability superimposed

293 ncreased to 2.54 km m(-2) degrees C(-1) Soil moisture was negatively correlated with fine-root growth

294 Increases in the level of moisture were accompanied by decreased quantitative resp

295 re significantly more stable when exposed to moisture when compared to the typical 3D perovskite meth

296 miting factor for land carbon uptake is soil moisture, which can reduce gross primary production thro

297 of gross primary productivity (GPP) to soil moisture, which improves the model agreement with observ

298 air temperature, soil temperature, and soil moisture, while browning occurred most often at cold sam

299 , the leaves revealed a very high content of moisture, with several beneficial compounds, including o

300 that range of depths to achieve higher soil moisture would also generally create cooler conditions f