Dual Porosity Craig M. Bethke and Brian Farrell1 Task 1: Dual porosity model of Pb transport We’ll model Pb transport as before, except we’ll take 40% of the aquifer to be stagnant. Water is stationary there, but the - Porosity - Document - PDFSEARCH.IO

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	Dual Porosity Craig M. Bethke and Brian Farrell1 Task 1: Dual porosity model of Pb transport We’ll model Pb transport as before, except we’ll take 40% of the aquifer to be stagnant. Water is stationary there, but the Add to Reading List Document Date: 2016-03-18 09:04:10 Open Document File Size: 332,45 KB Share Result on Facebook

Dual Porosity Craig M. Bethke and Brian Farrell1 Task 1: Dual porosity model of Pb transport We’ll model Pb transport as before, except we’ll take 40% of the aquifer to be stagnant. Water is stationary there, but theAdd to Reading List