The downward and upward movement of different rhizobia strains in soil
s with flowing water were investigated. In a leaching experiment using
saturated soil, the first appearance of cells in the leachate was sig
nificantly affected by the characteristics of rhizobia and soils. The
motility level of the rhizobia and movement aided by flagella did not
contribute to the downward movement of rhizobia. Indeed, the presence
of a high number of flagella impeded the movement of cells through por
e necks. The presence of a limited number of large water-filled pores
shortened the time of first appearance of flagellated cells. Compariso
n of the leaching of chloride ions and rhizobial cells suggested that
cells were being retained in soil by mechanical sieving. Retention of
rhizobia was also demonstrated in an experiment which studied the upwa
rd movement of rhizobia with flowing water into dry soil above a water
table. Retention was most evident for flagellated cells.