ライフサイエンスコーパス: fresh water

1 ognized as a sustainable approach to harvest fresh water.

2 the water, and refilling the container with fresh water.

3 c diversity, whether terrestrial, marine, or fresh water.

4 nventional technologies for the treatment of fresh water.

5 monia acquired from aerosolized contaminated fresh water.

6 ther these stromatolites formed in marine or fresh water.

7 re is a valuable and omnipresent resource of fresh water.

8 kes that store 87% of Earth's liquid surface fresh water.

9 ed through contact with contaminated soil or fresh water.

10 own groups, with at least two transitions to fresh water.

11 estern Lake Erie, which is a vital source of fresh water.

12 e a different driver hierarchy from land and fresh water.

13 ection on this gene (and/or linked genes) in fresh water.

14 terstitial fluid with the external hypotonic fresh water.

15 about 25 per cent of the excess discharge to fresh water.

16 rmination of inorganic As species in natural fresh water.

17 pitation being the critical component of the fresh water.

18 iciency will likely become a vital source of fresh water.

19 s desalination that can turn salt water into fresh water.

20 ry or long-term decreases in availability of fresh water.

21 extend the bioassessment of MeHg to fishless fresh waters.

22 of heavy metals than are typically found in fresh waters.

23 fer a way to track and restore the health of fresh waters.

24 te that this odontocete was fully adapted to fresh waters.

25 eful tool for in situ monitoring of MC-LR in fresh waters.

26 long-term measurements of DIC in marine and fresh waters.

27 ects directly to availability and quality of fresh water, a major environmental issue of the 21st cen

28 Fully half of that additional fresh water-about 10,000 cubic kilometers-infiltrated th

29 sources matched the amount and rate at which fresh water accumulated in the North Atlantic during muc

30 vices that natural ecosystems provide (food, fresh water, air, climate, and medicine).

31 rics of monocultures and polycultures of six fresh-water algal species.

32 e cultured in the laboratory in a variety of fresh-water amoebae and macrophage-like cell lines.

33 lation on the transport pathways of Siberian fresh water and associated matter.

34 ranes are a highly efficient tool to provide fresh water and augment existing water supplies.

35 the Earth's climate system, among them heat, fresh water and carbon dioxide.

36 hich contains about one-third of the world's fresh water and covers a wide geographical area (1.5 and

37 e the design of policy to ensure security of fresh water and energy supply.

38 rctic climate and ecosystems by transporting fresh water and key substances, such as terrestrial nutr

39 approximately 0.1%) of HFFF in contaminated fresh water and likely be applied universally to trace H

40 in a variety of microbes that inhabit soil, fresh water and marine environments.

41 ability to transport large amounts of heat, fresh water and nutrients, the ocean is an essential reg

42 a multifaceted bacterium sans frontieres in fresh water and other ecosystems linked to the water cyc

43 nt of the wastewater can reduce the need for fresh water and potentially add to the environmental ben

44 yrene, and a bioplastic polylactic acid from fresh water and saltwater using three hydrophobic NADES.

45 gulation that maintain plasma homeostasis in fresh water and seawater fish are well known, the corres

46 e-water partition coefficients) measured for fresh water and seawater, and estimation of enhancement

47 These materials swell in fresh water and shrink in salt water, and thus the expan

48 n Baltic Sea, leading to a greater runoff of fresh water and terrestrial dissolved organic carbon (DO

49 s important for preventing eutrophication in fresh waters and maintaining water quality.

50 nisms that control switching between hyper- (fresh water) and hypo-osmoregulation (seawater) remain m

51 more constant and buffered environment than fresh water), and has evolved a unique type of swimming

52 ees C, 5-30min) through mixing with boiling, fresh water, and further to explore the effects of heat

53 matic osmolality changes between its vector, fresh water, and mammal host.

54 groundwater wells penetrate defined bases of fresh water, and nearly 16% of wells overlie it by no mo

55 e of the phages were capable of predation in fresh water, and only ICP1 was able to prey on V. choler

56 across the planet, including from air, soil, fresh water, and the oceans.

57 of E. faecalis as a reservoir of VGs in the fresh water aquatic environment.

58 Land plants evolved from fresh-water aquatic algae, and the transition to a terre

59 +/- 3.1 megatonnes of nitrogen per year) to fresh water are about 2.7 times the estimated 'safe' nit

60 availability and toxicity of trace metals in fresh water are known to be regulated by the complexatio

61 ee amino acids under sunlight irradiation in fresh waters are not fully understood.

62 n (OH)D insufficiency was 11 times higher in fresh water areas compared to high saline areas (AOR: 11

63 m-negative bacterium flourishes naturally in fresh water as a parasite of amoebae, but it can also re

64 c Ocean might have gained four times as much fresh water as comprised the Great Salinity Anomaly of t

65 The fresh-water Asian species Boesemania microlepis has an u

66 water, current policies informed by base of fresh water assessments may not be managing and protecti

67 on it automatically and continually releases fresh water at room temperature.

68 eenhouse-gas concentrations, and maintaining fresh-water availability.

69 In contrast, iron transport in the fresh water bacterium Aeromonas hydrophila is found to o

70 tive organism of Legionnaires' disease, is a fresh-water bacterium and intracellular parasite of amoe

71 sly, they were thought to have originated in fresh water before the breakup of Pangea, implying a nea

72 terrestrial water cycle with the majority of fresh water being used for agriculture.

73 ric deposition can be a major source of P to fresh water bodies and may strongly affect their biogeoc

74 y able to support large birds, especially in fresh water bodies such as those present in the Turonian

75 tant roles in nitrogen and carbon cycling in fresh waters but we do not know how these two processes

76 be determined, revealing a steady influx of fresh water, but with distinct spatiotemporal difference

77 rgy from salinity gradients between salt and fresh waters, but potential applications are currently l

78 ncing widespread encroachment on the base of fresh water by groundwater users.

79 Two commonly used algal strains, fresh-water Chlorella vulgaris and seawater Tetraselmis

80 e and one Fayetteville Shale HFWs diluted by fresh water collected from the Ohio and Allegheny Rivers

81 eguarded in some places and that the base-of-fresh-water concept needs to be reconsidered as a means

82 ortation fuel production, CO(2) utilization, fresh water conservation, and maintenance of a small clo

83 Climate change, biodiversity conservation, fresh water conservation, ecosystem productivity, and ca

84 ss of these differing circulations, heat and fresh water converge toward the equator, where the ice i

85 icient approach to converting sea water into fresh water could be of substantial benefit, but current

86 he four known globin genes that exist in the fresh-water crustacean Daphnia magna, several are indivi

87 r is found at depths deeper than the base of fresh water, current policies informed by base of fresh

88 mmodities, such as gases, fine chemicals and fresh water, currently represent around 15 per cent of g

89 asic circadian oscillator of the unicellular fresh water cyanobacterium Synechococcus elongatus PCC 7

90 n roadways and deicer use are now salinizing fresh waters, degrading habitat for aquatic organisms, a

91 ng water, and wastewater), and low priority (fresh water, demineralized water, waste gas, and electri

92 interlinked remains poorly characterized in fresh waters, despite the potential for chemical and mic

93 be utilized to determine changes in riverine fresh water discharge.

94 The fresh water discharged by large rivers such as the Amazo

95 Oceanic transports of heat, salt, fresh water, dissolved CO2, and other tracers regulate g

96 tigated materials, such as DOM isolated from fresh water, DOM in whole-water samples, and TiO2 and si

97 ies to escape from Mono Lake water than from fresh water, due to the high concentration of Na2CO3 whi

98 discharged thousands of cubic kilometres of fresh water each year into surrounding oceans, at times

99 Pb speciation under conditions relevant for fresh water ecosystems using resonant X-ray emission spe

100 arine particulates, and marine biofilms into fresh water environments.

101 ter from humidity to address the shortage of fresh water, especially in arid locations where other so

102 patially is needed to assess salinization of fresh water, establish reasonable thresholds and restora

103 d (FD-FPH) protein hydrolysates derived from fresh water fish (Cirrhinus mrigala) muscle, using papai

104 Arapaima gigas, a fresh water fish found in the Amazon Basin, resist preda

105 Aequorin-injected eggs of the medaka (a fresh water fish) show an explosive rise in free calcium

106 of petroleum, phosphate, agricultural land, fresh water, fish, and wood indicate that the growing hu

107 organisms co-exist in oceanic or fast moving fresh water flows.

108 adwater of 9 major Asian rivers that provide fresh water for 1.65 billion people and many ecosystems,

109 ght an alarming situation in the scarcity of fresh water for irrigation due to the present global wat

110 riven FO system for continuous production of fresh water from saline water or wastewaters.

111 's third-largest crude oil reserve, requires fresh water from the Athabasca River, an allocation of 4

112 reveals that the average annual discharge of fresh water from the six largest Eurasian rivers to the

113 Preventing and remedying fresh waters from chemical pollution is a fundamental so

114 mated tilapia (Oreochromis mossambicus) from fresh water (FW) to seawater (SW); performed suppression

115 pendent processes that could enable abundant fresh water generation.

116 applicable to Chlamydomonas, a biflagellate fresh water green alga, but intense autofluorescence fro

117 ines both functions and serves as an all-day fresh water harvester.

118 ing salinities signify that large amounts of fresh water have been added to the northern North Atlant

119 has an active resurfacing mechanism, or that fresh water-ice in the outer Solar System can persist fo

120 Scarcity of fresh water in arid and semi-arid regions means that we

121 However, the storage of fresh water in ice shelves and/or groundwater reserves i

122 depend on international cooperation, such as fresh water in international basins or large marine ecos

123 water is a resource equivalent to 10% of all fresh water in lakes on Earth.

124 Groundwater is a primary source of fresh water in many parts of the world.

125 Canthocamptidae, believed to have colonized fresh water in Pangaea during Carboniferous times.

126 s at low levels in adults, which emerge from fresh water in spring before the threat of freezing temp

127 at a rate that threatens the availability of fresh water in the northeastern United States.

128 The distribution of fresh water in the Southern Ocean and its partitioning b

129 ion-channel protein to sense the presence of fresh water in which they can lay their eggs.

130 xtremes and climatic impacts on food yields, fresh water, infectious diseases, conflict, and displace

131 these hydrological systems, the dynamics of fresh water input into marginal seas can be used to iden

132 il bivalve shells to reconstruct patterns of fresh water input into the paleo North Sea during the ea

133 ed (236)U contamination could be supplied by fresh water input.

134 coverage, probably as a result of increased fresh-water input.

135 ed such events by inserting large amounts of fresh water into the northern North Atlantic Ocean.

136 ransported large amounts of buoyant cold and fresh water into the northern North Atlantic Ocean.

137 tes in their urine, while subjects consuming fresh water-irrigated produce excreted undetectable or s

138 for uptake by cucumber plants as compared to fresh water irrigation.

139 Because fresh water is Ca2+-poor, our results suggest that one p

140 A shortage of fresh water is one of the acute challenges facing the wo

141 ition from fresh to more saline-the "base of fresh water"-is frequently used to determine the stringe

142 eral interrelated factors, including lack of fresh water, lack of drainage, the presence of high wate

143 al evidence for an associated deep, probably fresh-water, lake.

144 tood out, displaying a Hg cycling similar to fresh water lakes.

145 areas of the ocean floor and bottoms of many fresh-water lakes.

146 Population growth, arable land and fresh water limits, and climate change have profound imp

147 recent decades because of the huge amount of fresh water locked into the ice sheet and the impact tha

148 ere, we track the pathways and fate of these fresh water masses by initializing synthetic particles i

149 Fresh water may now be accumulating in the Arctic Ocean

150 ium limacinum and Tetraselmis chuii) and two fresh water microalgae (Chlorella vulgaris and Chlorella

151 equences of the two proteins from marine and fresh water mollusks exhibit the characteristic features

152 to provide the clean, reliable, and abundant fresh water necessary to support aquatic ecosystems and

153 ater types, secondary WW (positive control), fresh water (negative control), chlorinated WW, and HPC

154 ypothesis that most stickleback evolution in fresh water occurs within the first few decades after in

155 Groundwater comprises 95% of the liquid fresh water on Earth and contains a diverse mix of disso

156 city of the quantified organic compounds for fresh water organisms in recipient surface waters.

157 Renewable fresh water over continents has input from precipitation

158 would reduce the need to transport waste and fresh water over long distances.

159 tochemical processes taking place in surface fresh waters play an important role in the transformatio

160 shehri and Fazli) and prawn (Tiger prawn and Fresh water prawn) of different storage time and physiol

161 The rising use of seawater desalination for fresh water production is driving a parallel rise in the

162 made at depths deeper than defined bases of fresh water pump fresh groundwater (TDS < 2,000 mg/L).

163 quired of a CDI system with a total ocean-to-fresh water required energy input of ~1.45 Wh/L.

164 climate change but will face sea-level rise, fresh water resource degradation, and intensified storms

165 ct variability and availability of inputs to fresh water resources across the tropics.

166 The energy sector is a major user of fresh water resources in China.

167 cal discrepancy among fossil fuel resources, fresh water resources, and energy demand.

168 since they are continuously defiling limited fresh water resources, seriously affecting the terrestri

169 und the globe attempt to better-manage their fresh water resources.

170 o important controls on Tibetan Plateau (TP) fresh water resources.

171 as been used as target for monitoring of the fresh water resources.

172 ught to have been initiated by North America fresh water runoff that caused a sustained reduction of

173 500 mM or approximately 30,000 mg l(-1)) to fresh water (salinity <10 mM or <600 mg l(-1)) in which

174 Data were grouped by ecosystems (fresh water, salt water, terrestrial, and wetland) and r

175 Fresh water scarcity has led to increased use of reclaim

176 In addition, fresh water scarcity in dry regions or during periods of

177 Fresh water scarcity is one of the most threatening issu

178 entury the extensive clearing of forestland, fresh water scarcity, and sharp rises in the price of fo

179 other samples examined, including sea water, fresh water, sediment, terrestrial, extreme, metazoan-as

180 While extensive studies involving EET from a fresh water Shewanella microbe (S. oneidensis MR-1) to s

181 ies for providing reliable, safe, low-sodium fresh water should be developed alongside improvements i

182 In the giant dopamine neuron of the fresh water snail Planorbis corneus, bursting exocytotic

183 etylcholine binding protein (AChBP) from the fresh water snail, Lymnaea stagnalis, shows it to be a s

184 ariety of environments, including sea water, fresh water, soil, and air.

185 These fresh water sources facilitated human expansions into ar

186 Fresh water sources, including lakes, such as the Great

187 Antarctica contains most of Earth's fresh water stored in two large ice sheets.

188 Rising temperatures and lessening fresh water supplies are threatening agricultural produc

189 nology for treating saline waters to augment fresh water supply.

190 f considering a broad range of TPs of FLX in fresh water systems and in ecotoxicity tests and to incl

191 influence predator-prey interactions in the fresh water systems.

192 ink salmon (O. gorbuscha) spend less time in fresh water than any other species of Pacific salmon, an

193 sport large amounts of carbon, nutrients and fresh water through oceans and play an important role in

194 ish that tolerate a wide salinity range from fresh water to > 3x seawater.

195 ted approximately 20,000 cubic kilometers of fresh water to the Arctic and high-latitude North Atlant

196 he ice margin, thus affecting the routing of fresh water to the North Atlantic Ocean.

197 roundwater recharge feeds aquifers supplying fresh-water to a population over 80 million in Iran-a gl

198 s a large unicellular organism that swims in fresh water using cilia.

199 Cu activity for normal ranges encountered in fresh waters using WHAM VI.

200 Atmospheric water harvesting (AWH)-producing fresh water via collecting moisture from air-enables sus

201 g system, this hydrogel membrane can produce fresh water with a daily yield of ~34 L m(-2) in an outd

202 y distributions and compare defined bases of fresh water with salinity distributions and groundwater

203 orthern Sumatra, revealing recent release of fresh water within the deep sediments.

204 nly on more extensive use of arable land and fresh water would require clearing forests and exacerbat