ライフサイエンスコーパス: fresh water

1 rmination of inorganic As species in natural fresh water.

2 pitation being the critical component of the fresh water.

3 ther these stromatolites formed in marine or fresh water.

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

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

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

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

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

9 nventional technologies for the treatment of fresh water.

10 monia acquired from aerosolized contaminated fresh water.

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

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

13 extend the bioassessment of MeHg to fishless fresh waters.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

93 Fresh water may now be accumulating in the Arctic Ocean

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

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

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

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

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

99 Renewable fresh water over continents has input from precipitation

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

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

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

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

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

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

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

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

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

109 500 mM or approximately 30,000 mg l(-1)) to fresh water (salinity <10 mM or <600 mg l(-1)) in which

110 Fresh water scarcity has led to increased use of reclaim

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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