Author(s): Alcides Pereira*
The frequency and intensity of heavy rains following long dry and warm spells are growing
Hardy, main to floor runoff, soil erosion, and irritating move water fine. In well dependent,
loamy and clayey soils, water and even reactive solutes, adsorbed on small soil particles, is
probably channeled through large pores macrospores without penetrating into the nice porous
matrix Edwards, Shipitalo, and Vogel.
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