“…,Olson and Miller 2010, Lin andAshlock 2014b) and soils (e.g., Ashlock 2011, 2014a). It has several advantages compared to the multi-receiver methods such as MASW, including: (1) greatly reduced instrumentation costs, since only one sensor and a two-channel data acquisition system are required; (2) increased portability, as a multichannel seismograph with external battery source and string of geophones are not required; (3) enabling minimally invasive measurement of higher modes using a single borehole for downhole receiver measurements with moving impacts at the surface (Lin and Ashlock 2014a, Ashlock and Lin 2014); (4) the potential to be faster than MASW if a movable servo-electric impact source is used, as the set-up time for a string of geophones and cables is eliminated; and (5) ease in obtaining 3-D stiffness profiles, as the source can readily be moved along different horizontal lines, compared to reinstalling an entire string of geophones multiple times to cover the entire testing area for MASW, as shown inFigure 6.4 in Chapter 6.…”