|
|
||||||||
|
Fig. 1. Theoretical structural effects on water retention for a fluvial sample and a debris flow sample, both of which are well stratified. A fluvial sample is expected to have a broader pore-size distribution than a debris flow sample of comparable particle-size distribution because of its greater abundance of both small and large pores.
|
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |