산성(酸性) 유산염(硫酸鹽) 토양(土壤)에 관(關)한 연구(硏究) - 투수(透水)에 의(依)한 석회(石灰) 시용량(施用量)이 수도생육(水稻生育)에 미치는 영향(影響) -

Studies on the Acid Sulphate Soils - Effect of the Rice Plant Growth by Amounts of Lime Application on No-Percolation and Percolation -

산성(酸性) 류산염(硫酸鹽) 토양(土壤)에 석회시용(石灰施用)과 투수(透水) 무투수(無透水)가 수도생육(水稻生育)에 미치는 영향과 토양(土壤) 성분변화(成分變化)를 본바 다음 몇가지 결과(結果)를 얻었다. 1. 분얼 및 초장(草長)은 생육초(生育初)에는 별차이가 없으나 8월이후(月以後) 석회(石灰)의 효과가 나타남과 아울러 투수구(透水區)가 무투수구(無透水區)에 비(比)하여 효과적이었다. 2. 수수(穗數) 및 수당립수(穗當粒數), 임실률(稔實率)도 석회시용증가(石灰施用增加)에 따라 효과가 좋으며 무투수(無透水)에 비(比)하여 투수구(透水區)가 좋은 결과(結果)를 가져왔다. 3. 정조수량(精粗收量)은 표준구(標準區) 100에 비(比)하여 무투수(無透水) Ca 12me/100gr가 194% 투수구(透水區)의 Ca 4me/100gr가 268%, Ca 8me/100gr가 315% 증수(增收)되었다. 4. 석회시용(石灰施用)에 따라 호마엽고병(胡麻葉枯病) 병반(病斑)도 감소(減少)되었다. 5. 석회시용(石灰施用)에 따라 토양내(土壤內) 성분변화(成分變化)는 유효인산, 가용성(可溶性) $SiO_2$ 함량이 증가(增加)되었고 $Fe^{{+}{+}}$의 함량(含量)이 감소(減少)되었다.

This experiment was conducted to investigate the influence of amounts of lime dressed on the growth of rice by the treatment of percolation and nonpercolation in the acid sulphate soil. And also analysis of soil chemical components after treatment was carried out. The results obtained were summarized as follows: 1. In the initial stage of growth, number of tillers and plant length showed no distinct differences between the treatments of percolation and nonpercolation, but after August the effect of lime appeared and the percolation treatment was more effective than the nonpercolation. 2. Lime dressing affected good influence on the panicles, grain per panicles and the rate of grain formation, and the treatment of percolation showed better results than nonpercolation. 3. If the yield of rough rice in the control (nonpercolation and lime dressing) was 100, it was 194 in the treatment of nonpercolation 12me/100gr of lime dressed, 268 in the treatment of percolation-4me/100gr of lime and 315 in the 8me/100gr-percolation. 4. Lime dressing affected good influence on the control of Helminthosporium leaf spots. 5. In the case of lime dressing, amounts of available phosphate and soluble silicon dioxide were increased, but ferrous ion ($Fe^{{+}{+}}$) were decreased.