Open AccessModeling flow pathways through pores and cracks in aerated soils
Author(s) -
Kumar Mohi
Publication year - 2011
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1029/2011eo340009
Subject(s) - macropore , environmental science , agriculture , groundwater , soil water , irrigation , leaching (pedology) , soil science , agronomy , ecology , geology , chemistry , biochemistry , catalysis , mesoporous material , geotechnical engineering , biology
Knowledge of how chemical contaminants spread through soil is of vital importance to those who manage groundwater and agricultural resources, superfund sites, landfills, and mines. Of particular interest to contaminant transport studies is crop management—though crops can be victims of pollution from elsewhere, fertilizers and other agricultural chemicals can leach through the soil and infiltrate groundwater. The spread of such contaminants from farmland not only is influenced by the amount of chemicals used for farming but also depends on how agriculture affects soil—activities such as mechanized farming, irrigation scheduling, swelling and shrinking properties, crop‐rooting characteristics, and earthworm or other biological activity can influence the amount and size of air pockets in the soil. These “macropores”—so named because they are typically about 1 millimeter or larger in diameter—can allow agricultural contaminants to move through the soil more rapidly, along preferential flow paths. ( Water Resources Research , doi:10.1029/2010WR009451, 2011)