논토양(土壤)의 탈질작용(脫窒作用)에 관(關)한 연구(硏究) -제(第) 1 보(報). 사질답토양(砂質畓土壤)에서 질소시비량(窒素施肥量) 차이(差異)가 탈질(脫窒)에 미치는 영향(影響)

Studies on the Denitrification in the Submerged Paddy Soil -1. The Denitrification Rates Upon the Different Levels of Nitrogen Fertilizer in Sandy Soil

담수토양조건(湛水土壤條件)에서 질소시비량(窒素施肥量)이 상이(相異)했을때 아산화질소(亞酸化窒素)($N_2O$) 생성(生成)에 의한 시비질소(施肥窒素)의 탈질(脫窒)과 관계(關係)한 몇가지 결과(結果)를 요약(要約)하면 다음과 같다. 1. 담수항온기간중(湛水恒溫期間中) $N_2O$ gas의 생성량(生成量)은 항온(恒溫) 20일경(日傾)에 가장 많았으며 시비량(施肥量)이 증가(增加)할수록 $N_2O$ gas의 생성량(生成量)도 증가(增加)하여 최고(最高) $1830{\mu}g/100g$을 나타내었다. 2. 토양중(土壤中) 질소시비량(窒素施肥量)이 증가(增加)할수록 Ammonia 화성율(化成率) 및 초산화성율(硝酸化成率)이 증가(增加)하였다. 3. Mitchaelis-Mentene의 효소반응공식(酵素反應公式)에 의한 초산태질소(硝酸態窒素)로부터 탈질량(脫窒量) 산출결과(算出結果)는 실제(實際) 아산화질소측정(亞酸化窒素測定)에 의한 탈질량(脫窒量)과 높은 상관관계(相關關係)가 있었으며 계산식(計算式)에 의한 탈질량(脫窒量)이 다소(多少) 많았다. 그리고 본시험결과(本試驗結果) 탈질반응(脫窒反應)은 Zero Order Kinetic으로 밝혀졌다.

A laboratory experiment was conducted to find out the denitrification rate upon the different levels of nitrogen fertilizer in submerged sandy soil. The results obtained were summarized as follows: 1. The highest denitrification rate was observed at 25 days after incubation. The amount was reached at 1830 ug/100g soil for 20mg nitrogen was applied in 100g soil. 2. Increases of fertilizer nitrogen was enhanced the rate of ammonification and nitrification during the incubation time. 3. Deep correlation was observed between the denitrification capacities which was determined as nitrous oxide and Mitchaelis-Menten kinetic with relation to nitrate concentration. More higher denitrification rates were observed in Mitchaelis-Menten kinetic than dentrification rate with determined as nitrous oxide. 4. A Zero order (with relation to nitrate concentration) kinetic model for denitrification was presented in this experiment condition to illustrate the variability of nitrous oxide concentrations in the submerged soil atmosphere.