SSSAJ Journal of Natural Resources and Life Sciences Education
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Fig. 1. Calculation of the MACRO exponent n* from hydraulic conductivity (K) and head (h) for the macropore region; (a) calculation of n* for various assumed boundary hb values between the macropore and micropore regions; (b) linear regression fitting for the assumed boundary hb of 30 mm, based on the n* values for the curves in (a).





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