Our research group is trying to estimate the quantity of sediment blowing off of cultivated fields during the winter in the Canadian Prairie region. It is a common-held belief that this sediment is a significant loss of soil from farm fields and a major source of sediment and associated nutrients being delivered to adjacent field boundaries, to roadside ditches in particular. It is a very conspicuous phenomenon, but the magnitude of sediment transport is being questioned. Our plan is to collect the dirty snow (referred to a “snirt” in this region) in one-meter-wide strips extending out from the field boundaries into the adjacent ditches. We have only found reference to one other study trying to make such measurements, and it was a small study carried out in this region about 15 years ago. Any information of advice would be appreciated.