Calculate the flux of oxygen between the ocean and the atmosphere, given that: Temp = 18°C Salinity = 35 ppt Density = 1025 kg/m3 Oxygen concentration measured in bulk water = 263.84 mmol/m3 Wind speed = 7.4 m/s Oxygen is observed to be about 10% initially supersaturated
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Calculate the flux of oxygen between the ocean and the atmosphere, given that:
- Temp = 18°C
- Salinity = 35 ppt
- Density = 1025 kg/m3
- Oxygen concentration measured in bulk water = 263.84 mmol/m3
- Wind speed = 7.4 m/s
- Oxygen is observed to be about 10% initially supersaturated

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- If 30.0 mL of water that is 0.0500 M in Q is to be extracted with four 10.0-mL portions of an immiscible organic solvent, what is the minimum distribution coefficient that allows transfer of all but the following percentages of the solute to the organic layer: (a) 1.00 X10-24 (b) 1.00 X10-22A salt solution (30% Na2CO3) weighing 1ton iscooled to 20C where the salt crystallizes asdecahydrate. What will be the crystal yield ifthe solubility is 21.5 kg anhydrous Na2CO3/100kg water? (assume that 3% of the totalsolution is lost by evaporation)The distribution ratio D for an analyte is defined as the ratio of its analytical concentration in two immiscible solvents (organic versus aqueous): D = Corg/Caq Show that the fraction of analyte remained in the aqueous phase after the extraction (from aqueous to organic) is given by the following: Fraction remained = Vaq/(VorgD + Vaq) where Vaq and Vorg are the volume of water and organic solvent used in the extraction, respectively.
- (a) Water in vadose zone contains chlorobenzene of concentration 40 mg/L. What is the equilibrium concentration soil air in contact with this solution? (b) An aquifer with porosity 0.3 has distribution coefficient of TCE as 100 L/kg. What fraction of TCE is in aqueous phase and sorbed phase of the soil?The size of the ionic atmosphere, called the Debye radius, is 1/K, where k is given by e? NA" 1/2 Vi K = where e is the electronic charge, NA Avogadro's constant, ɛo the permittivity of vacuum (8.854×10-12 c2.N-1.m-2), ɛ the dielectric constant of the solvent, kg the Boltzmann constant, T the absolute temperature, and I the ionic strength. Calculate the Debye radius in a 0.036 m aqueous Na2S203 solution at 25°C. (Assume the density of the solution at 25°C is 1.0029 g•cm¬3.) 4.0 ÅHydroxyapatite, Ca₁0 (PO4) 6 (OH)2, has a solubility constant of Ksp = 2.34 x 10-59, and dissociates according to Ca10 (PO4)(OH)2(s) = 10 Ca²+(aq) + 6 PO¾-¯(aq) + 2 OH(aq) Solid hydroxyapatite is dissolved in water to form a saturated solution. What is the concentration of Ca²+ in this solution if [OH] is fixed at 3.60 × 10-4 M? [Ca2+] = M
- Allowable recovery from limiting salt calculations Determine the limiting sait and allowable recovery for a brackish water RO system containing the following solutes: calcium 74 mg/L. barium 0.008 mg/L. and sulfate 68 mg/L. Assume 100 percent rejection of all solutes and & polarization factor of 1.15 and ignore activity coeficients (i.e., activity = concentration).Suppose you have a soil that is made up of 10% organic matter with CEC = 200 cmol/kg, 40% kaolinitewith CEC = 10 cmol/kg, and 50% vermiculite with CEC = 100 cmol/kg.1- Calculate the overall CEC of the soil by taking a weighted average of the three soil components.2- What percentage of the overall CEC is contributed by the organic matter? How does that numbercompare to the 10% of the soil itself that is organic?> EL session.masteringchemistry.com MasteringChemistry ROSTER-2019-SPRI-PULLM-CHEM-101 blackboard wsu Google Search MasteringChemistry: HW 8 KHW 8 Applications for Dilution Calculations K8 of8 Dilution as a procedure in analysis We sometimes purposely dilute solutions if the analyte concentrations wavelengths in the visible (and sometimes uitraviolet) range. Based on the dissolved solute's properties, we can quantify that solute's concentration are too high to permit an accurate measurement. For example, a spectrophotometer can measure the amount of light that passes through a sample solution for If the solute's concentration is too high, a relatively small amount of incident light having the wavelength that corresponds to the solute's absorption behavior will less light is absorbed, and the detector in the spectrophotometer can generate more reliable data. reach the dete ctor, which results in an inaccurate measurement (consider the result if you blocked the light with an opaque…
- Calculate the masses of oxygen and nitrogen that are dissolved in 3.0 L of aqueous solution in equilibrium with air at 25 °C and 760 Torr. Assume that air is 21% oxygen and 78% nitrogen by volume. 0.55104 mass: Henry's law constants for gases in water at 25 °C Gas kn (bar-M-¹) He 2.7 x 10¹ N₂ 1.6 x 10' 0₂ 7.9 x 10² CO₂ 29 H₂S 10. 1.79 source: S, Rock, And Gallogly 46-General Chemistry | Publisher: University BooksDescribe the challenge of transporting oxygen and carbon dioxide in animals. In particular, discuss the polarity of oxygen and carbon dioxide gas, their consequence on solubility in the aqueous environment, and the inadequacy of passive diffusion in transporting these gases into cells and tissues.2.50 g of Na2CO3.xH2O crystals were dissolved in water and made up to 1000 cm³ of solution. 25 cm³ of this solution required 12.50 cm³ of 0.035 mol dm³ HNO3 for complete neutralisation. Calculate the value of x in Na2CO3.xH2O using the steps given below. Detailed working needs to be shown and where relevant answers must contain units. 2HNO₁₂ + Na2CO3 →2NaNO, + CO. + H.O (a) Calculate the number of moles of Na,CO, in 25 cm³ (b) Calculate the number of moles of Na,CO, in 1000 cm² (ej Calculate the mass of Na,CO, in 1000 cm³ (d) Calculate the mass of water of crystallisation associated with this mass of Na₂CO Calculate the moles of water of crystallisation associated with this mass of Na2CO3 (e) Calculate the value of x in Na2CO3.xH₂O