Extract of bottom sediments
Radoslav Schügerl, +421(2)3229 3508, firstname.lastname@example.org
The bottom sediments arise by sedimentation of solid particles on the fluvial bottom, or their sedimentation in the adjacent areas. Typical areas for sedimentation are straight section of upwelled rivers, old river arms with full or partial flow, internal riversides of river bends, inundation area, and lateral river expansions. Sediments consist of organic and inorganic compounds. We offer extract of bottom sediments for determination of soil texture and determination of saturated hydraulic conductivity.