Ideal Gas Law
n/V = P/(R*T) n= (P*V)/(R*T)
R for P = 8.314 J mol-1 K-1 , R for atm = 82.05 x 10-6 atm m3 mol-1 K-1 1.0 atm = 1.01325 x 105 PA
Air: 8.0 x 10-11 mol CHCl3/mol Air = 8.0 x 10-2 ppbv CHCl3
Water: 42 μg/L of something = 42 ppb and mg/L = ppm
Percent concentration of a gas in air is by pressure or moles (multiply PT by percentage in IGL to calculate moles)
Percent concentration in water is by mass typically
Hardness = TH = 2 * [Ca2+] + 2 * [Mg2+] + N of other multivalent Cations (answers in eq/L)
Carbonate Hardness = CH = [HCO3-] + 2 * [CO32-] up to the TH (answers in eq/L)
TDS = Σ mass concentrations of all ions (answers in mg/L)
Alkalinity = Kw/[H+] or [OH-] + [HCO3-] + 2 * [CO32-] - [H+]
Ionic Strength = I = 1/2 Σ cizi2 (molar concentration * the square of the charge for all ions)
pH = -log [H+], 10-5 M of [H+] has a pH of 5
TS = MB/VA TDS = MG/VD SS = ME/VD TVS = (MB-MC)/VA VSS = (ME-MF)/VD
VA w/o water = MB which burned = MC
VD filtered = ME on paper + MG still in solution, ME burned = MF (for the VSS)
Turbidity
concentration = particles/cm3 surface area concentration =
μm2/cm3
Volume of a sphere = 4/3πr3 Cross sectional area of a sphere = πr2
Volume of particles = density x mass total mass/mass of one particle = # of particles OR number per gram
If this is particles per L, be sure to change to particles per cm3 etc.
Total cross sectional area = cross sectional area of one particle x number of particles per cm3
Acid-Base Reactions & Acid Dissociation & Strong & Weak Acids
HA ↔ H+ + A-
KA = [H+][A-] pKA = -log10(KA) pKA = pH - log10[A-] + log10[HA]
[HA]
[HCO3-] typically balances natural waters for electroneutrality
(pKA) for HCO3- à
CO32- + H+ is 10.33, K = 10-10.33
K = [CO3-][H+]
[HCO3-]
Relative Humidity = Vapor Pressure/Saturation Vapor Pressure
Kinetics Rate Law R = k [A]a[B]b
YA = 100 ppb, YB = 50 ppb, YC = 1 ppb
A + B à C, k1 = 2 x 10-4ppb-1min-1, R1 = k1 [A][B]; C à A + B, k2 = 0.2 min-1 , R2 = -k2 [C] Therefore dYC/dt = k1 [A][B] - k2 [C]
A+ B à C & C à A + B τ = (C)/((k1*A*B)-(k2*C));
A + A à Products τ = Ao/(2k Ao2); A à products τ = Ao/(k1 Ao); A à Products τ = Ao/(ko)
Rate Law R = - 1/a (d[A]/dt) = -1/b (d[B]/dt) = 1/c (d[C]/dt) where A + B à C
dx/dt = production(x) - consumption (x) @ steady state dYx/dt = 0 = k1 YAYB - k2YC solve for YC
Henry's Law CW = KH,g Pg Pg = Hg CW KH,g is M/atm Hg is atm/M
CW is the species concentration in aqueous phase (M)
Pg is the partial pressure of the gaseous species (atm)
Material Balance Cx*VW + (Px*Va)/(R*T) = moles
Solubility Product & Solid Precipitation (solid must be present)
AxBy à xA + yB [A]x * [B]y = Ksp (T) e.g. [Ca+][F-]2 = 3 x 10-11 M3 for CaF2
Adsorption
Linear: qe
= Kads Ce Langmuir:
qe = qmax (b Ce)/(1 + b Ce) Freundlich: qe = Kf Ce1/n
qe = mass of sorbed contaminant (moles or mg per g of sorbant) Ce = concentration in fluid at equ. (moles or mg per liter)
qmax = max sorbtion Kads & b are L/g or moles
Freundlich linearized: log qe = 1/n log Ce + log Kf Langmuir linearized: Ce/qe = Ce/qmax + 1/(b * qmax) [plot Ce/qe on Y and Ce on X]
Uptake = contaminant on AC (mol or mmol)/grams AC = q; then plug in values of q to graph
Often, sorbed moles + Ct + gaseous moles = some total number of moles