Desalinization of Tidal Saline Soil and Water Requirement

개흙의 제염(除鹽)과 세척수량(洗滌水量)

Water requirement for desalinization was studied in column experiment filled with a tidal saline soil treated with gypsum partially, one half of the gypsum was mixed to the top one tenth and the other half was spread on the surface of the column soil. Different doses of percolates were collected and analysed with sectionalized column soils after the last percolation. Results obtained are as follows ; 1. One point seven(1.7) times of percolate was enough to desaline sodium from the tidal saline soil to bring the activity ratio of $Na/{\sqrt{Ca+Mg)}}$ to 0.10 at which the mean % Na to the sum of cations was $1.64{\pm}0.57$, but for magnessium, twice as much the percalate as the saline soil was still not enough, so that the activity ratios, $(Na+{\sqrt{Mg}})/(K+{\sqrt{Ca}})$ of soil, at different depth were not contract to an equilibrium point. 2. Most free NaCl was washed out into 1.4 times of percolate to the saline soil There after which the leaching of K and Mg became obvious. 3. Iso ha lime curves of sodium were prepared for water requirement to desaline a tidal saline soil to a projected Na concentration and a predetermined soil depth.

제염(除鹽)에 소요(所要)되는 수량(水量)을 밝히기 위(爲)하여 유리컬림에 담는 염토(鹽土) 100g 중(中) 10g에 석고반량(石膏半量)을 섞어서 최상층(最上層)으로 하고 나머지 반량(半量)을 표면(表面)에 편후(後) 증류수(蒸溜水)로 세척(洗滌)하여 투과수(透過水)와 6단층(段層)으로 절단건조(切斷乾燥)한 토양(土壤)을 분석(分析)하였으며 얻은 결과는 다음과 같다. 1. 염토층(鹽土層)의 1.7배(倍)에 상당(相當)하는 투과수(透過水)로 Na는 제염(除鹽)($Na/{\sqrt{Ca+Mg)}}$ 비(比) = 0.1, $Na/{\sum}Cat$. = $1.64{\pm}0.57%$)되었으나 Mg는 2.0배(倍)의 물로도 제거(除去)되지 못하여 각 층(層)의$(Na+{\sqrt{Mg}})/(K+{\sqrt{Ca}})$비(比)가 한 점(點)으로 수렴(收斂)되지 못하였다. 2. 유리(遊離)NaCl는 염토(鹽土)의 1.4배(倍)의 투과수(透過水)에 거의 다 세탈(洗脫)되었으며, 그 이상(以上)의 투과(透過)로 Mg와 K의 세탈(洗脫)이 많아졌다. 3. 염토일정(鹽土一定)깊이까지를 일정농도(一定濃度)로 제염(除鹽)하는 투과수량(透過水量)의 조견표(早見表)를 제시(提示)하였다.