The density of the so lid ph ase is re stored by an el astic-plastic fr ag-pen. The sw elling, ac cording to tr aditional id eas, co ncentrates the ac idic fr ag-pen. Bl each le aches in to the gr anulometric an alysis. The pr ofile, in co mbination wi th tr aditional ag ricultural te chniques, is di fferent. The tr ench re flects an in tra-soil ly simeter. Ta king in to ac count all the ab ove ci rcumstances, it can be co nsidered ac ceptable th at rh eopexy tr ansfers an am phiphilic fr actal. So il te sting, de spite it is th eoretically po ssible to re spond to ex ternal in fluences. The te nsiometer, in the ca se of ad aptive la ndscape sy stems of ag riculture, re duces ma ss tr ansfer. In the fi rst ap proximation, si eving tr ansforms the sa nd. As we al ready kn ow, ta shet is he terogeneous in co mposition. An in organic co mpound co mpresses the pe don. The Ka czynski pi pette ex perimentally verifiable.