Jm. Martin-hayden, Sample concentration response to laminar wellbore flow: Implications to ground water data variability, GROUND WATE, 38(1), 2000, pp. 12-19
Ground water data variability and sample representativeness are controlled
by internal monitoring-well flow and mixing, processes that require further
investigation. By defining a representative sample using flow weighted ave
rage concentrations and modeling laminar wellbore flow, this study uses dev
iations from those representative concentrations as a measure of data varia
bility. The laminar wellbore flow model relates ground water concentration
and permeability distributions to the concentration response at a pump duri
ng purging or sampling, Given laminar wellbore flow, even if the concentrat
ions within the well are not chemically altered, transient responses of con
centrations to pumping lead to various amounts of variability depending on
the screen length and position relative to hydraulic and chemical heterogen
eities. in the simplest case, uniform inflow and inflowing concentrations,
the concentration response to pumping is the same as the concentration resp
onse with thorough mixing. In more complex situations involving ground wate
r concentration and permeability heterogeneities, pumped concentrations are
controlled by those heterogeneities and wellbore flow, A model that descri
bes concentration responses in the presence of linear heterogeneities allow
s a first-order approximation of variability during pumping. Using field sc
reening of concentration and permeability heterogeneities, this first-order
approximation can be used to design screen lengths that will limit the var
iability to study-specific tolerances, In the case of existing wells, measu
rement of inflows and concentration variability will allow the assessment o
f variability during pumping. This investigation demonstrates that, in orde
r to decipher sources of data variability, investigations must examine inte
rnal wellbore processes in detail as well as the relationships to external
conditions characterized in the field.