PMID-sentid Pub_year Sent_text comp_official_name comp_offsetprotein_name organism prot_offset 30933482-4 2019 During the sampling time, both high relative humidity (RH, ranged from 40% to 93%) and inorganic mass fraction in particles (62.6 +- 12.4% of dry particles, on average) resulted in abundant aerosol liquid water (43 +- 6% in the wet PM1, on average), which may liquefy the particles. Water 205-210 transmembrane protein 11 Homo sapiens 232-235 32052323-3 2020 Water-soluble ionic contents were also more distributed in PM1.1 with the great contents of secondary particles (NO3-, SO42-, and NH4+). Water 0-5 transmembrane protein 11 Homo sapiens 59-62 31377367-1 2019 The aerosol liquid water content (ALWC) of submicron particles (PM1) was calculated in this work by three methods based on the aerosol physical and chemical properties measurement campaigns in winter in Beijing, including (a) the PM1 volume difference between the ambient and dry states by applying the particle number size distribution and particle hygroscopicity measurement; (b) the thermodynamic equilibrium model (ISORROPIA II) based on the chemical composition; and (c) the kappa-Kohler theory of chemical composition with a volume mixing scheme. Water 19-24 transmembrane protein 11 Homo sapiens 64-67 32361437-0 2020 Characterization of atmospheric trace gases and water soluble inorganic chemical ions of PM1 and PM2.5 at Indira Gandhi International Airport, New Delhi during 2017-18 winter. Water 48-53 transmembrane protein 11 Homo sapiens 89-92 32361437-1 2020 Water soluble inorganic chemical ions of PM1 and PM2.5 and atmospheric trace gases were monitored simultaneously on hourly resolution at Indira Gandhi International Airport (IGIA), Delhi during 8 December 2017-10 February 2018. Water 0-5 transmembrane protein 11 Homo sapiens 41-44 30878926-0 2019 Characteristics and secondary formation of water-soluble organic acids in PM1, PM2.5 and PM10 in Beijing during haze episodes. Water 43-48 transmembrane protein 11 Homo sapiens 74-77 30878926-5 2019 Multiple linear regression was used to tentatively quantify the relative contributions of photochemical oxidation and aqueous-phase oxidation to the formation of total water-soluble organic acids in PM1, PM2.5 and PM10 during haze episodes. Water 168-173 transmembrane protein 11 Homo sapiens 199-202 30056622-1 2018 OBJECTIVES: Diffusion-weighted MRI provides information regarding body water movement following death, which may be an imaging marker of post-mortem interval (time since death; PMI) or maceration (degree of tissue degradation during intra-uterine retention) in perinatal deaths. Water 71-76 transmembrane protein 11 Homo sapiens 177-180 30366297-5 2019 Water-soluble inorganic ions and carbonaceous components were major chemical species in PM1.0 and PM2.5, accounting for 48.9%-54.1% and 25.6%-27.8% in PM1.0, 48.1%-52.3% and 22.7%-24.7% in PM2.5. Water 0-5 transmembrane protein 11 Homo sapiens 88-91 30366297-5 2019 Water-soluble inorganic ions and carbonaceous components were major chemical species in PM1.0 and PM2.5, accounting for 48.9%-54.1% and 25.6%-27.8% in PM1.0, 48.1%-52.3% and 22.7%-24.7% in PM2.5. Water 0-5 transmembrane protein 11 Homo sapiens 151-154 29522679-3 2018 In this Article, we present a detailed picture for the folding of the inhibitor peptide PMI into a helix during binding to the oncoprotein fragment 25-109Mdm2 obtained from atomistic, explicit-water simulations and Markov state modeling. Water 193-198 transmembrane protein 11 Homo sapiens 88-91 25079411-8 2014 The results of the back trajectory analysis imply that the high concentrations of PM1.0 and its water-soluble inorganic ions may be caused by stagnant weather conditions in Wuhan. Water 96-101 transmembrane protein 11 Homo sapiens 82-85 27572526-0 2016 Water soluble organic carbon in aerosols (PM1, PM2.5, PM10) and various precipitation forms (rain, snow, mixed) over the southern Baltic Sea station. Water 0-5 transmembrane protein 11 Homo sapiens 42-45 29964757-3 2016 The results showed that the total concentrations of measured water-soluble ions were (15.39+-9.91), (21.10+-15.49) and (36.34+-18.51) mug m-3 in PM1.1, PM2.1 and PM9, respectively. Water 61-66 transmembrane protein 11 Homo sapiens 145-148 29964757-4 2016 In PM1.1 and PM2.1, secondary water-soluble ions (SO42-, NO3- and NH4+) comprised 87.59% and 86.30% of all water-soluble ions, respectively, while in PM9, SO42- and Ca2+ comprised 32.78% and 28.54% of all water-soluble ions, respectively. Water 30-35 transmembrane protein 11 Homo sapiens 3-6 29964757-4 2016 In PM1.1 and PM2.1, secondary water-soluble ions (SO42-, NO3- and NH4+) comprised 87.59% and 86.30% of all water-soluble ions, respectively, while in PM9, SO42- and Ca2+ comprised 32.78% and 28.54% of all water-soluble ions, respectively. Water 107-112 transmembrane protein 11 Homo sapiens 3-6 29964757-4 2016 In PM1.1 and PM2.1, secondary water-soluble ions (SO42-, NO3- and NH4+) comprised 87.59% and 86.30% of all water-soluble ions, respectively, while in PM9, SO42- and Ca2+ comprised 32.78% and 28.54% of all water-soluble ions, respectively. Water 107-112 transmembrane protein 11 Homo sapiens 3-6 27017073-6 2016 Liquid water content (LWC) in both PM1 and PM2.5 had positive correlations with relative humidity (RH) but negative correlations with visibility, implying that hygroscopic growth might be a factor for visibility impairment, especially LWC in PM1. Water 7-12 transmembrane protein 11 Homo sapiens 35-38 27768907-5 2017 Water-soluble inorganic ions were the most abundant species in both PM1 and PM2.5, followed by organic mass (OM). Water 0-5 transmembrane protein 11 Homo sapiens 68-71 27768907-9 2017 The water content in PM1 and PM2.5 was enhanced by the water-soluble components, especially NH4NO3. Water 4-9 transmembrane protein 11 Homo sapiens 21-24 27768907-9 2017 The water content in PM1 and PM2.5 was enhanced by the water-soluble components, especially NH4NO3. Water 55-60 transmembrane protein 11 Homo sapiens 21-24 24370694-1 2014 Hourly mass concentrations of water-soluble ions in PM1 and gasses (NH3, HNO3, HCl) were on-line measured with a Monitor for AeRosols and Gases Analyzer (MARGA) in Shanghai from Oct. 1 to Nov. 16, 2012. Water 30-35 transmembrane protein 11 Homo sapiens 52-55 24370694-4 2014 The average mass concentration of PM1 and total water-soluble ions (TWSI) in PM1 in haze episodes were 78.9 +- 29.9 mug/m(3) and 47.2 +- 17.2 mug/m(3), 3.11 times (from 1.49 to 4.06 times) and 3.28 times (1.96 to 4.34 times) as those in non-haze periods, respectively. Water 48-53 transmembrane protein 11 Homo sapiens 77-80 24370694-17 2014 In addition, Strong NH3 and HNO3 reaction resulted in the enhancement of NH4NO3 mass fraction, therefore increased associated water content in PM1 under high RH condition and contributed to visibility degradation. Water 126-131 transmembrane protein 11 Homo sapiens 143-146 34217941-8 2021 Compared with micron-sized water droplets, PM1.0 removal efficiency improved by approximately two times higher. Water 27-32 transmembrane protein 11 Homo sapiens 43-46