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yeah, im looking for best or easiest way to calculate recharge from rainfall. currently what in have done is that, i have divided domain in to polygons based on geology and rainfall stations using theissen polygon method.
is there any better way to assign recharge from rainfall data, such as, by using some kind of formula or something?
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how can i use scripts to devolope plugin?
suppose i attach vary bc plugin, how can i enter data for that?
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how to get it?
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If im considering recharge based on rainfall, which is the best method?
nb: ihave predicted rainfall data also
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what i he is considering density dependent condition?
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im doing groundwater modeling in a coastal region using feflow. i have some confusion regarding adding values in time series. in my case, if im getting 100, 50, 0, 100 mm of total rainfall in each month over an area, and i want to add it in time series as 30, 60, 90 days etc respectively . do i need to divide that monthly recharge by number of days in that month? . for example 100/30 for first month, 50/30 for second.. etc or can i put directly that value so that feflow will divide it in to missing days. how it works?
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IM DOING THE SAME AS HE SAID. BUT IT IS TAKING SO MUCH TIME TO RUN THE MODEL FOR THE FIRST TIME. I WAITED SO LONG, THEN CANCELED. IS THAT DUE TO ANY MISTAKE I HAV DONE?
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anyone pls expain step by step on how to calibrated boundary condition using IFM pilot points? since im new to programing i cant understand above code. but still iw ant to learn it
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i would like to know how to download ifm plugin
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I'm doing groundwater modeling in feflow. now it is in transient state calibration. i run with monthly recharge and daily time step. After high recharge time, during summer water level is not declining. graph is going straight and in next year it adds up more.
while changing porosity waterlevel fluctuation id getting high, but still it is not draining. Any suggestion on where i made mistake and wat make to drain water faster? may b because of not giving pupming rate? :-[
I'm using hydraulic conductivity, porosity, and inflow on top of slice as material property