seismic surveying within the upper few meters of the Earth's shallow subsur
face requires a high-frequency source. To ascertain the important features
of such sources, experiments were conducted at test sites in central and ea
stern Kansas using various impulsive seismic sources (4.5-kg hammer, 30.06
rifle, and .22-caliber rifle) to examine the effects of minimizing source e
nergy on the frequency content of reflection data. Results indicate that th
e higher energy near-surface seismic-reflection sources (e.g., sledgehammer
, large-caliber projectiles) lack some of the high-frequency energy exhibit
ed by smaller sources, precluding the detection of reflection signal from u
ltrashallow depths (<3 m) at the sites tested. At the test site in eastern
Kansas, the .22-caliber rifle yielded more energy above 250 Hz than either
the sledgehammer or 30.06 rifle. At the test site in central Kansas, where
three reflective interfaces shallower than 3 m exist, the .22-caliber rifle
with subsonic ammunition yielded the largest amount of energy at frequenci
es above 300 Hz and produced the best data.