ライフサイエンスコーパス: humid

1 e foraging activity when conditions are more humid.

2 y traversodont cynodonts are restricted to a humid 6 degrees equatorial swath that persisted for over

3 esence of water and can be subjected to 1000 humid adsorption/desorption cycles with minimal degradat

4 intain a high capacity of 1600 mA h g(-1) in humid air ( approximately 10% relative humidity).

5 tion layer also allows LixSi to be stable in humid air ( approximately 40% relative humidity).

6 tions of 1606 ppm, 15033 ppm, and 185 ppm in humid air (with 20% RH), respectively.

7 investigated the byproducts generated by the humid air discharge itself, which are the greenhouse gas

8 27(5) A, beta = 97.41(3) degrees), formed in humid air from the solid dimeric [Cu(CF(3)COO)(2) x (qui

9 Hyperventilation of hot humid air induces transient bronchoconstriction in patie

10 s is the tetranuclear blue product formed in humid air of the mu(4)-oxo tetramers.

11 y condensation of the water molecules of the humid air on the paper-sensor during the forced exhalati

12 Binary CO2/H2O adsorption measurements for humid air reveal that the presence of H2O at 2.55 kPa en

13 As expected, humid air samples are required for proper sensor functio

14 to collect water and promote nucleation from humid air(7-9).

15 eaction of Fe and O (causing iron to rust in humid air).

16 bonyls into imines mediated by NH3 vapors in humid air, resulted in selective browning of the LSOA sa

17 dsorbed than long chain alcohols, whereas in humid air, this preference is changed, and the sensitivi

18 Pseudomonas putida, i.e., biofilms grown in humid air, were analyzed by atomic force microscopy to d

19 lved in surface-adsorbed water reservoirs in humid air, with the signal strength being governed by th

20 rying concentrations of hydrogen fluoride in humid air.

21 cation of the destruction pathway in dry and humid air.

22 , ways when exposed to HCl and NH3 vapors in humid air.

23 chanically ventilated dogs (n = 8) with warm humid air.

24 chemistry with the participation of vapor in humid air.

25 sphere under an ultralow contact pressure in humid air.

26 iad" of neurons (with a dry-, a cold-, and a humid-air-responding cell [3]), IR40a expression include

27 oups can be explained by their hydrolysis in humid ambient conditions.

28 ine methane sensors for measuring methane in humid and condensing sewer air.

29 ng-term impact of NT/RT on N2 O emissions in humid and dry climatic zones with emissions expressed on

30 nvestigated at the gas/solid interface under humid and dry conditions, along with the nature of the h

31 margins smallest for species occupying both humid and dry tropical environments.

32 and storage in semiarid and arid, but not in humid and dry-subhumid, environments.

33 Flash droughts are most likely to occur over humid and semi-humid regions, such as southern and north

34 y of humidity swing driven air capture under humid and windy conditions is tested in the laboratory.

35 ver a wide range of climate conditions (arid-humid) and limiting factors (soil moisture, leaf area, e

36 ens are intensifying (becoming more warm and humid), and thus changes in synoptic meteorology may be

37 n soil moisture tended to be greater in more humid areas.

38 esponsive to decreased precipitation in more humid areas.

39 130 degrees C) and working conditions (i.e., humid) as well as in the presence of various interfering

40 A more humid atmosphere helps to explain PETM temperatures, but

41 ples were subjected to an oxygenated, highly humid atmosphere in a closed chamber for 4 to 5 months.

42 mechanism is revealed to differ for dry and humid atmospheres, changing from a site-specific binding

43 properties were not affected by exposure to humid atmospheres.

44 ter droplets and films on the leaf hair from humid atmospheres; collection of fog droplets on leaf ha

45 arid basin (the Tarim River Basin, TRB) and humid basin (the Yangtze River Basin, YRB) were evaluate

46 rt of Pangea and suggest that the equatorial humid belt in the Late Triassic was about as wide as it

47 prolonged residence in the austral temperate humid belt where a provincial vertebrate fauna with earl

48 ble Deccan Traps drifted into the equatorial humid belt where uptake of CO(2) by efficient silicate w

49 e onto continental crust within the tropical humid belt.

50 Humid biomes also respond to drought at short time-scale

51 Arid and humid biomes are both affected by drought, and we sugges

52 ed and brominated substances as observed for humid carrier gases.

53 r calculation remains large, particularly in humid catchments (for example, figure 2 in our paper).

54 0.51 kg C m(-2), lower than that observed in humid cities but much higher than that assumed in many r

55 d cities, which is stronger than that in the humid climate due to a stronger longwave radiative forci

56 cted rocks (mafic/ultramafic) and a tropical humid climate with high precipitation rate are needed to

57 te climate, hot and dry climate, and hot and humid climate) for at least 9 days simulating the period

58 , and for biofuels regions of a moderate and humid climate.

59 +/- 0.3 kelvin (mean and standard error) in humid climates but decreasing DeltaT by 1.5 +/- 0.2 kelv

60 t decrease in yield-scaled N2 O emissions in humid climates when fertilizer-N was placed at >/=5 cm d

61 Therefore, in humid climates, deep placement of fertilizer-N is recomm

62 cts the species range limits in both dry and humid climates, whereas SLA and longevity do not show cl

63 oses to produce ferric oxyhydroxides in more humid climates.

64 a-scaled N2 O emissions, in particular under humid climatic conditions.

65 s on the surface of an early Earth beneath a humid CO(2) atmosphere suffering electrical discharge.

66 Under humid conditions (50% RH), the major end products were 4

67 osity being retained after exposure to harsh humid conditions (90% relative humidity at 353 K).

68 n of atmospheric (CH3)2COO may survive under humid conditions and react with SO2, very different from

69 tilization models that already work well for humid conditions but still lack the mechanistically base

70 olumn breakthrough experiments under dry and humid conditions corroborate the excellent CO2 selectivi

71 ous and the subsequent onset of long-lasting humid conditions during the Late Cretaceous were driven

72 ly Holocene transition and increased as more humid conditions favored forest development after ca. 10

73 Humid conditions first occur at approximately 15 ka, and

74 ons at the interface of hybrid systems under humid conditions has the potential to reveal the local c

75 years ago, coincident with the onset of more humid conditions in central Africa at the beginning of t

76 Rapid changes towards more humid conditions in eastern South Africa as the Northern

77 The combination of warm, humid conditions in neonatal incubators, particularly in

78 ith NO being the major product under dry and humid conditions in the absence of molecular oxygen and

79 s at the polymer/metal oxide interface under humid conditions is vital to understand the long-term du

80 Exposure to humid conditions led to a significant increase in Zn bio

81 mined on bean leaf surfaces maintained under humid conditions or periodically exposed to desiccation

82 jor rise in water levels and a shift to more humid conditions over much of tropical Africa after appr

83 O)2(dobdc), steadily releases bound NO under humid conditions over the course of more than 10 days, s

84 million concentrations of ammonia even under humid conditions was observed.

85 trol experiments (RH < 1%, or no FeCl3 under humid conditions).

86 ZnO readily dissolved under humid conditions, whereas ZnS persisted in the dust.

87 African climate changed rapidly towards more humid conditions, while northern sub-Saharan Africa expe

88 ylene decreased PO2 and PCO2 both in dry and humid conditions.

89 y and selectivity, particularly under highly humid conditions.

90 y loses 7% of its maximum CO2 capacity under humid conditions.

91 er, glycerol, and squalane core phases under humid conditions.

92 of vocal fold vibration in desiccated versus humid contexts, arid and cold ecologies should be less a

93 of pedogenic carbonates provide evidence of humid cool woodlands with a grassy substrate.

94 accumulation of soil nitrate in Chinese semi-humid croplands based upon more than 7000 samples from 1

95 nitrate reservoir in the vadose-zone of semi-humid croplands, where the nitrate cannot be denitrified

96 nges from increased water content during the humid deposition.

97 is change may be related to fungal growth in humid dust.

98 th fermentation: fusty/muddy sediment, musty/humid/earthy, and winey/vinegary.

99 a transitional zone between the extremes of humid eastern and dry western forest types.

100 In the humid eastern United States, there is evidence of higher

101 e less amenable, when contrasted to warm and humid ecologies, to the development of languages with ph

102 mpling design includes many plots located in humid ecosystems and ignores critical areas for the cons

103 In humid ecosystems, the rate of methane (CH4 ) oxidation b

104 s that Eoanabas likewise lived in a warm and humid environment as suggested by the co-existing plant

105 ives the bodies would have decomposed in the humid environment of the tombs.

106 iscible, volatile solvent was deposited in a humid environment on a variety of substrates to achieve

107 , a mode of collective bacterial motility in humid environment through the depinning of bacterial dro

108 l coincides with paleoclimatic change from a humid environment to highly variable and much drier cond

109 At higher coverage and in a humid environment, adsorbate interchange was detected.

110 effect of water was more pronounced at high humid environment, while at low RH the matrix plasticiza

111 t role in the migration of microorganisms in humid environment.

112 Humid environments can serve as a reservoir and source o

113 occurring in agricultural workers in hot and humid environments may represent harbingers of the detri

114 In humid environments or biological systems, hydrolytic sta

115 Shrubs in humid environments tend to be hydraulically integrated,

116 We attribute this 'dry' behaviour in humid environments to the presence of curved S-Mo-S plan

117 ubsequent mud formation on solid surfaces in humid environments typically have adverse effects on sur

118 some MOFs can be structurally compromised in humid environments.

119 in designing better synthetic adhesives for humid environments.

120 northward dispersal likely occurred during a humid episode in the Sahara within Marine Isotope Stage

121 hern margin of Amazonia, which show that the humid evergreen rain forests of eastern Bolivia have bee

122 biomarkers (even at p.p.b. levels) in highly humid exhaled breath.

123 This work evaluated the humid extraction of barley beta-glucans and partially ch

124 vanna zones in the north gradually turn into humid forest zones in the south).

125 Sites in closed humid forests of northwest Madagascar and a montane eric

126 ozone recovery in a colder and possibly more humid future Arctic lower stratosphere.

127 limits of low proton affine analytes even in humid gas mixtures containing high proton affine compoun

128 Stability in both gaseous (such as humid gases) and aqueous media is considered.

129 ent with adjacent "hot," "cold," "dry," and "humid" glomeruli-an organization that allows for both un

130 In a temperate, humid grassland, we examined the seasonal impacts of cli

131 oss of kleaf and turgor loss point) than the humid-habitat Ranunculus lanuginosus Accordingly, water

132 These lineages originated in humid habitats and colonized dry/seasonally dry environm

133 ies living in tropical, densely forested and humid habitats in Africa have evolved darker faces.

134 V-1 DNA in dried blood spots (DBS) stored in humid heat and at -20 degrees C.

135 ) ] eumenorrheic women exercising in dry and humid heat, across their menstrual cycle.

136 d, flies avoided dry heat more robustly than humid heat, and this modulation was abolished by silenci

137 across the menstrual cycle, yet is lower in humid heat, in conjunction with reduced evaporative cool

138 associated with menstrual phase and dry vs. humid heat.

139 rual cycle phase, but differ between dry and humid heat.

140 and mid-luteal (ML) phases in dry (DRY) and humid (HUM) heat matched for wet bulb globe temperature

141 This study investigates the impact of humid indoor conditions on the bioaccessibility of Zn in

142 northern and southern hemispheres, producing humid intervals in one hemisphere matched to aridity in

143 It consists in exposing humid kernels to high steam pressure followed by a decom

144 ing, reveal that landslide frequency in many humid landscapes may be insensitive to projected changes

145 We show that humid, low-elevation communities are phylogenetically ov

146 the contemporary northern limit (colder and humid maritime regions; Denmark and Norway) will probabl

147 to the ecological opportunities provided by humid, megathermal forests, which were increasingly avai

148 radation upon exposure to dry air/oxygen and humid nitrogen/water environments, thus separating the e

149 Flies inhabiting the colder and more humid north-facing slope carried about 6% more transposa

150 C stocks in arid sites but decreased them in humid ones.

151 However, these membranes require humid operating conditions, which limit the temperature

152 Only when the overlying air is humid or droplet concentrations are very low does suffic

153 of the onset and termination of the African Humid Period are contested, with strong evidence for bot

154 nd termination of the Early Holocene African Humid Period are subjects of ongoing debate, with direct

155 strong terrestrial evidence that the African Humid Period ended abruptly, supporting the hypothesis t

156 rupt transitions into and out of the African Humid Period in northeast Africa.

157 suggests that the termination of the African Humid Period in the Horn of Africa occurred within centu

158 hemispheric coherence of this early African Humid Period is challenging due to opposing seasonal ins

159 deposition of F- and Na+ during the African Humid Period suggests rapidly fluctuating lake levels be

160 sal was possible because during the Holocene humid period the region contained a series of linked lak

161 ad timing of this period, termed the African Humid Period, is well known.

162 in this region, possibly during the Holocene humid period.

163 mong Near Eastern farmers during the African Humid Period.

164 anges in atmospheric wet deposition (arid vs humid periods).

165 Hominin occupations correspond with humid periods, particularly Marine Isotope Stages 7 and

166 animals and humans populated it during past humid phases.

167 These conditions led to humid pulses in South Africa and potentially to the crea

168 vegetation ranging from wooded savannahs to humid rainforest.

169 NE-II serotype was more common in hot, humid regions (P = .02) but was also present in other re

170 uggesting that any land cover changes in non-humid regions (P/PET<1) or in watersheds of low water re

171 ater-resource and land-use management in sub-humid regions of the world.

172 are most likely to occur over humid and semi-humid regions, such as southern and northeastern China.

173 e darkest flies were collected from the most humid regions.

174 to be a major cause of rock fracture in cold humid regions.

175 Here, we report the identification of the humid-responding neuron that completes the hygrosensory

176 n the Vaejovis vorhiesi group, restricted to humid rocky habitats in mountains across southwestern No

177 al closure) than conspecific plants from the humid site.

178 However, SOC losses in humid sites were counterbalanced by the effect of planta

179 Near room temperature, the humid source produces abundant gold-hydroxy cluster anio

180 he school term in late May-June 2009 in more humid southeastern states), school vacations (preventing

181 arlier societal disruption in the relatively humid southern Maya Lowlands.

182 outbreaks of pandemic influenza during more humid spring, summer, and autumn months might appear to

183 from a cold-dry polar-type climate to a warm-humid sub-Antarctic-type climate.

184 cal, predominantly deciduous), early Eocene (humid subtropical, mixed deciduous and evergreen), and m

185 cal patterns over topoclimate gradients in a humid temperate broadleaf forest in southern Appalachian

186 seful to enhance ecohydrological modeling in humid temperate forests.

187 ated human malaria, including P. vivax, into humid temperate or warm climate refuges around the Medit

188 ly show that the Tortonian Europe mainly had humid to subhumid summers and no arid climate has been c

189 of current agro-industrial scale clearing in humid tropical Africa.

190 Oxisol soils are widely distributed in the humid tropical and subtropical regions and are generally

191 Glaciation in the humid tropical Andes is a sensitive indicator of mean an

192 nated in the region, which formed a warm and humid tropical archipelago in the Early Triassic.

193 tion satellite datasets was used to quantify humid tropical forest clearing from 2000 to 2005.

194 ca contributes 5.4% to the estimated loss of humid tropical forest cover, reflecting the absence of c

195 We present a worldwide analysis of humid tropical forest dynamics and tree species richness

196 of redox fluctuations on lignin breakdown in humid tropical forest soils during ten-week laboratory i

197 and represents a 2.36% reduction in area of humid tropical forest.

198 Long-term monitoring of plots in mature humid tropical forests concentrated in South America rev

199 Humid tropical forests have the fastest rates of organic

200 Psychotria marginata, a shrub common to humid tropical forests in Central America, produces leav

201 ntributes to rapid rates of C cycling across humid tropical forests in spite of periodic O2 limitatio

202 constant proportion (9%) of biomass, but in humid tropical forests this ratio varies from 2% in undi

203 ions for understanding the global ecology of humid tropical forests, and their functional responses t

204 fference between the two models occurred for humid tropical forests, where the CLM-CN simulated a 62%

205 ional species pools and local assemblages in humid tropical forests.

206 crease the accuracy of ecological studies in humid tropical forests.

207 omote forest regeneration and restoration in humid tropical lowland areas with high biomass resilienc

208 ed the largest area of GFCL, followed by the humid tropical, dry tropical, and temperate biomes.

209 esculenta) is an important root crop in the humid tropics and a valuable source of essential mineral

210 However, every year vast areas of the humid tropics are disturbed by selective logging, unders

211 Extrapolation to perennial plants in the humid tropics is risky because functional relationships

212 Terrestrial ecosystems in the humid tropics play a potentially important but presently

213 rather unfavorable climate conditions of the humid tropics.

214 ighest in the boreal biome and lowest in the humid tropics.

215 tent estimates of forest clearing within the humid tropics.

216 uxes from land to water to atmosphere in the humid tropics.

217 ide food for over 800 million throughout the humid tropics.

218 nd 0.8 +/- 0.3 for rubber plantations in the humid tropics; and (ii) land use management policies sho

219 nd orders differently on both plastics under humid versus dry environments.

220 es and vegetation during the late Paleocene (humid, warm temperate to subtropical, predominantly deci

221 10(-6)s(-1) and 1.05x10(-6)s(-1) for dry and humid weather respectively.

222 urrence of disease is best predicted by wet, humid weather.

223 ace mixed layer was also observed to be more humid with higher relative humidity.

224 ly occur in hyper-arid zones and smallest in humid zones, highlighting the dependency on available su

225 cation of fossil-rich outcrops and temperate humid zones, indicating that climate change from arid to