Although nitrate (NO
3-) contamination of groundwater has been broadly detected, determinig NO
3- pathways to the groundwater still remains a challenge. In unsaturated soil, where NO
3- moves through, sitting over the groundwater table, soil water content always changes due to rainfall and evapotranspiration. Thus, it is speculated that behaviors of NO
3- dissolved in soil water might be complex in unsaturated soil. Using time domain reflectometry (TDR) we
in situ measured temporal changes in water and NO
3- contents in Andisol applied with animal manure. On a rainfall event, water infiltrated into greater than 40 cm deep whereas NO
3- just reached as deep as 10 cm from the soil surface.
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