WebQ = [SO 3] 2 [SO 2] 2 [O 2] Q = \dfrac{[\text{SO}_3]^2}{[\text{SO}_2]^2[\text O_2]} Q = [SO 2 ] 2 [O 2 ] [SO 3 ] 2 Q, equals, start fraction, open bracket, start text, S, O, end text, start … WebThe first law of thermodynamics applies the conservation of energy principle to systems where heat transfer and doing work are the methods of transferring energy into and out of the system. The first law of thermodynamics states that the change in internal energy of a system \Delta U ΔU equals the net heat transfer into the system Q Q, plus ...
The equilibrium constant K (article) Khan Academy
WebQc = [SO3]2 [SO2]2[O2] = 02 [SO2]2[O2] = 0. As the reaction proceeds toward equilibrium in the forward direction, reactant concentrations decrease (as does the denominator of Qc ), … WebThe rate of discharge of water Q is given by Q = v A Therefore v = Q A = k i from equation (5.5) But the water is actually flowing through an area A v with a velocity which will be indicated by v s. The rate of discharge Q is Q = v s A v which also = v A Therefore vs = v A Av = v V Vv where V is the total internal volume of the pipe = v n (5.10) taujihad
Heat Transfer Formula - Definition, Formula And Solved Examples
WebDec 6, 2011 · Answer: Δ H = 462 kJ/mol Use the Δ H and the balanced chemical equation below and calculate the Δ Hf of F–(g). H+(g) + F–(g) —-> HF(g)Δ H = – 150 kJ/mol Answer: Δ Hf of F–(g) = -120 kJ/mol Use the Δ H and balanced chemical equation below and calculate the Δ Hf of CN(s). 2 HCN(g) + AgCN(s) —-> Ag(s) + H2 (g) + 3 CN(s)Δ H = -113 kJ/mol WebMar 13, 2024 · Add together the heats of formation for the products, CO + H2, which is –110.53 kJ/mol + 0 kJ/mol = –110.53 kJ/mol. Subtract the sum of the heats of formation … Webq = ka(Δh/Δl) where K is a constant of proportionality that defines the water flux for a given hydraulic gradient (Δh/ΔL). The above equation can also be recast in terms of the water volume flux per unit area, Q/A (also called "Darcy flux" or "Darcy velocity" with units of … The thick sedimentary sequence has formed a vast expanse of flat topography o… Unit 2: Physical Hydrology Overview. This section of the course outlines the distri… Regional Aquifer Systems: Examples. Ground water flow systems extend over a w… Unit 1: Fresh Water: Scarcity or Surfeit? Overview. Water is often called the “Elixir … Module 3: Rivers and Watersheds Overview. In this module, we will investigate th… a1 掲示用