After examining the difference in the photosynthesis rate of corn according to the planting distance, the distance of 40 × 40 cm showed the lowest rate by 23 days after transplanting (May 31); however, there was no significant difference in the photosynthesis rate due to increased salt tolerance in the plant as time went by. As for the difference in growth features of a plant, the planting distance of 40×40cm showed a growing disorder due to the influence of salt by 23 days after transplantation (May 31); however, there was a desirable growth as time went by. For the difference in the salt content within a plant, the planting distance of 40×40cm tended to be higher than other planting distances, and the K⁺ content is much higher than other kinds of salt after examining the difference in salt absorption. As for the correlation between saline components within a plant, there was a significant negative correlation among K⁺, Ca²⁺, and Na⁺ while there was a significant positive correlation among Mg²⁺, Ca²⁺, and Na⁺. After examining the effectiveness of salt removal from soil according to corn cultivation, the planting distance of 30×30㎝ showed a remarkable decrease by 37 days, compared with 23 days, after transplantation in K⁺ by 28%, Ca²⁺ by 36.6 %, Mg²⁺ by 30.6 %, and Na⁺ by 22.9 %. And the salt content is higher in surface soil than in subsoil.
The PTDRT model as prediction techniques for desalinization in reclaimed tidelands was developed and verified whether it is applicable to reclaimed tidelands at the beginning stage. The changes of salt concentration during desalinization, the water requirements and period required for desalinization, were simulated according to soil properties and desalinization methods by repression analyses. The program was also designed to systematize input data and analysis data associated with desalinization, and to confirm the results by a graphic form. All input data and the results can be printed after the form of a typical report.
간척지에서의 제염에 따른 식생의 변화와 수도의 근모형성에 대한 염해의 영향을 알기 위하여 강화도, 남양 및 계화도 간척지를 중심으로 1982년 여름에 본 조사를 하여 다음과 같은 결과를 얻었다. 1. 간척후, 저습지에서는 퉁퉁마디와 칠면초가 최초로 우점종을 형성하는 고등식물이었으며, 제염이 됨에 따라 버들명아주가 출현했고, 또 이것에 이어 매자기와 갈대가 우점종의 자리를 차지하게 되며 매자기와 갈대가 우점종이 되는 염도의 토양에서는 수도재배에 대한 염해의 영향은 문제화되지 않았다. 2. 습지에서는 퉁퉁마디와 칠면초에 이어 사철쑥과 갯개미취가 우점종을 형성하게 되고, 이때에는 단자엽 화본료 잡초들의 이입이 시작되었다. 3. 건조지에서는 나문재와 해홍나물이 최초의 우점 고등식물로 등장하게 되고, 또 갯능쟁이도 있었지만 군락을 형성하지는 않았다. 4. 건조지에의 식물이입은 습지를 중심으로 이미 이입된 식물들이 제염이 진행됨에 따라 서서히 일어나게 된다. 5. 토양염도의 근모형성에 대한 형향은 고염도토양에서 생육된 것일수록 저염도 토양에서 생육된 것에 비하여 근모형성율은 낮추고, 또 근모장도 짧게 하는 것으로 나타났다.