특이산성토양(特異酸性土壤)에서 담수시(湛水時) 석회처리(石灰處理) 및 온도조절(溫度調節)이 토양(土壤)의 유효성분(有效成分) 변화(變化)에 미치는 영향(影響)

Effect of Lime and Temperature on the Changes of Available Soil Nutrients in Acid Sulfate Soil under Submergence

산성황산염토양(酸性黃酸鹽土壤)에서 담수시(湛水時) 석회(石灰) 처리량(處理量)과 온도(溫度) 조건(條件)에 따른 유효인산(有效燐酸)과 규산(珪酸)의 변화양상(變化樣相)과 함께 토양산도(土壤酸度)와 여러가지 화학성분(化學成分)과의 상관관계(相關關係)를 구명(究明)한 결과(結果)를 요약(要約)하면 다음과 같다. 1. 담수조건(湛水條件)은 토양(土壤)의 pH, 유효인산(有效燐酸) 유효규산(有效珪酸), 암모니아태(態) 질소(窒素), 제일철(第一鐵)의 증가(增加)와 알루미늄, 유효(有效)망간, 수용성(水溶性) 유황(硫黃)의 감소(減少)를 보였다. 2. 석회처리(石灰處理)는 토양(土壤)의 pH, 유효인산(有效燐酸), 유효규산(有效珪酸), 암모니아태(態) 질소(窒素), 수용성(水溶性) 유황(硫黃)의 증가(增加)와 알루미늄, 제일철(第一鐵), 유효(有效)망간의 감소(減少)를 보였다. 3. 석회(石灰) 12me/100gr 처리(處理)에서 pH 6.5 내외(內外)를 유지(維持)하였을 뿐만아니라 유효인산(有效燐酸), 암모니아태(態) 질소(窒素)의 증가(增加)와 알루미늄, 제일철(第一鐵)의 감소(減少)에도 효과(效果)가 컸다. 4. 온도간(溫度間)에는 $25^{\circ}C$보다 $35^{\circ}C$항온구(恒溫區)에서 유효인산(有效燐酸), 암모니아태(態) 질소(窒素), 그리고 환원태(還元態)인 제일철(第一鐵)의 생성(生成)이 많았다. 5. 담수기간(湛水期間) pH는 유효규산(有效珪酸)과 고도(高度)의 정상관(正相關)이 있었으며, 알루미늄, 제일철(第一鐵), 유효(有效)망간과는 부(負)의 상관관계(相關關係)를 보였다.

This experiment was conducted to investigate the changing patterns of the available elements by the control of lime addition amount and temperature in Acid Sulfate Soils under the submerged condition. The results obtained were summarized as follows: 1. pH and contents of available phosphate, soluble silicate, $NH_4-N$, and exchangeable iron in soils were decreased but exchangeable aluminium and manganese, and water soluble sulfur in soils increased after submergence. 2. Lime treatment increased pH, available phosphate, soluble silicate, $NH_4-N$, and water soluble sulfur, but that decreased exchangeable aluminium, iron, and manganese in soils. 3. Treatment with 12me/100gr of Ca as $CaCO_3$, showed the marked effect in increasing the exchangeable aluminium and iron, and increasing pH value to about 6.5 as well as available phosphate and $NH_4-N$. 4. Increases in available phosphate, $NH_4-N$, and exchangeable iron with aging of the soil flooded and lime treated were higher at $35^{\circ}C$ than those at $25^{\circ}C$. 5. Throughout submerged period a significant positive correlation was observed between pH and soluble silicate while the pH has negative correlation with exchangeable elements such as aluminium, iron, and manganese etc.