[논문]염류집적토양에서 규산질 비료가 인산의 유효도 증진에 미치는 영향

이용복; 김필주

염류집적토양에서 규산질 비료가 인산의 유효도 증진에 미치는 영향
Effects of Silicate Fertilizer on Increasing Phosphorus Availability in Salt Accumulated Soil during Chinese Cabbage Cultivation 원문보기

韓國土壤肥料學會誌 = Korean journal of soil science & fertilizer, v.39 no.1, 2006년, pp.8 - 14

이용복 (School of Environment and Natural Resources, The Ohio State University) , 김필주 (Dept. Agricultural Chemistry, Division of Applied Life Science, Graduate school, Gyeongsang National University)

초록
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시설재배지내 염류와 인산이 집적된 토양(Total-P; $2140mg\;kg^{-1}$)에서 이온간 경쟁에 의한 인산의 유효도를 증진효과 조사하기 위해 현장 작물재배시험을 실시하였다. 규산의 인산유효도 증진효과를 알아보기 위해 규산을 처리하지 않은 삼요소구(NPK)를 대비구로 하여, 인산무시용 조건에서 규산질비료를 세수준(0, 2, $4Mg\;ha^{-1}$) 처리하여 비교하였다. 인산을 시용한 삼요소구에 비해 인산을 무처리하고 규산을 처리시 배추의 생육과 수량은 크게 증대되었다. 특히 인산을 무처리하고 규산을 $4Mg\;ha^{-1}$ 처리시 삼요구에 비해 약 25%의 수량증대가 확인되었다. 식물체내 인산함량은 처리간 유의적인 차이는 없었으나 규산 처리량 증가에 따른 수량증대로 인산 흡수량이 유의적으로 증가하였다. 규산질비료 시용량 증가에 따라 토양 중 유효인산함량의 유의적 증가가 하였으며, 토양의 유효규산과 식물체의 규산함량간($r=0.76^{**}$), 그리고 식물체 규산함량과 배추 수량간($r=0.78^{**}$)에는 고도의 정의 상관관계가 확인되어 시용규산이 토양 내 인산의 유효도 증진과 작물의 인산흡수량 증가에 직접적 효과가 있는 것으로 조사되었다. 규산질비료 처리량이 증가함에 따라 식물체의 인산 흡수량 증가로 인해 시험 후 토양 중 Total-P 함량은 다소 감소하였으나, 유효인산 함량에는 큰 차이를 발견할 수 없었다. 시험 전 토양과 비교할 때 배추수확 후 토양 내 전 인산 함량 감소는 주로 Ca-P 함량 감소로부터 기인된 것으로 조사되었다. 결과적으로 인산 집적지 토양에 규산질비료의 적절한 시용은 인산의 유효도를 증진시켜 작물의 수량을 증대시키고, 인산시비량 감축에 따른 인산집적을 크게 감소시킬 수 있을 것으로 평가되었다.

Abstract ▼ AI-Helper

High phosphate accumulations in greenhouse soils have been considered as a new agricultural problem in Korea. The effects of silicate on changes in phosphate fractions and on the yield of Chinese cabbage without P fertilization were investigated by pot experiment. For this experiment, P-accumulated soil was selected (Total-P; $2140mg\;kg^{-1}$). Three levels of silicate (0, 2, and $4Mg\;ha^{-1}$) without P fertilization and P fertilizer without silicate application (Si0+NPK) were applied in 1/2000a pots. The same amount of nitrogen and potassium fertilizers were applied to the all pots. The application of $4Mg\;ha^{-1}$ of silicate greatly increased the yield of Chinese cabbage by 25% compared to Si0+NPK treatment. Although there is no significant difference in plant P absorption among all the treatments, the uptake of P in the $4Mg\;ha^{-1}$ silicate application was significantly higher than Si0+NPK treatment due to increase in yield. The content of available $SiO_2$ in soil increased with increasing silicate application rates. The Si concentration of plant showed a positive correlation with available $SiO_2$ contents in soil and the yield of Chinese cabbage. Total P greatly decreased with increasing rates of silicate application, yet the change in available P content was not significant. The Si0+NPK treatment increased the content of Ca-P by 11%, however, which was decreased by 27% in the $4Mg\;ha^{-1}$ silicate application. Therefore, the effect of silicate on reducing total-P was mainly attributed to the change in concentration of Ca-P. Our results suggest that the application of silicate in P-accumulated soils not only increase the crops yield but also reduces phosphate accumulation.

주제어

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문제 정의

The objective of this study were to investigate the effects of silicate application on the growth and yield of Chinese cabbage, and on the changes in phosphate fractional forms in a P-accumulated greenhouse soil.

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