토양용액 채취를 위한 토성별 한계수분함량 설정

Abstract

Soil moisture is an important factor for the availability and circulation of nutrients in arable soil. The purpose of this study was to set thresholds moisture content on soil nitrate concentration in the solution for real-time diagnosis. Sandy loam, silt loam, and sandy loam was filled with <TEX>$1.2g\;cm^{-3}$</TEX> at Wagner pots, 0, 100, and <TEX>$200mg\;L^{-1}$</TEX> of <TEX>$KNO_3$</TEX> was saturated. Nitrate in standard solution was recovered about 95% by passing the porous cup. Nitrate concentrations in sampling of soil solution were examined by using a porous cup. The soil solution was higher in accordance with sandy loam> silt loam> clay loam, limited water filled pore space for sampling soil solution was 33.7, 56.4, and 62.2%, respectively. Nitrate concentration in the soil solution was negligible at sandy loam and silt loam during sampling periods, which was decreased about 50~82% in clay loam compared to the initial <TEX>$NO_3$</TEX>-N concentration in the saturated <TEX>$KNO_3$</TEX> solution. Over limitation of soil solution sampling, soil EC and <TEX>$NO_3$</TEX>-N content were increased with the saturated <TEX>$NO_3$</TEX>-N concentration, regardless of soil texture (p<0.05). Conclusively, soil solution by using a porous cup was possible, regardless of the soil texture, which was useful for the diagnosis in nitrate concentration of soil solution. However, because nitrate concentration of soil solution in a clay loam changes, it was necessary for careful attention in order to take advantage for the real-time diagnosis of nitrogen management in soil.