관수(灌水)에 의(依)한 시비양분(施肥養分)의 토양중(土壤中) 이동(移動)에 관(關)한 연구(硏究) -2. 토양수분(土壤水分) 조건(條件)과 Cl와 P의 이동(移動)

류관식,유순호,송관철,Ryu, Kwan Shig,Yoo, Sun Ho,Song, Kwan Cheol 한국토양비료학회 1991 한국토양비료학회지 Vol.24 No.3

토양수분(土壤水分) 조건을 달리하였을 때 토양(土壤)에 시용한 양분(養分)이 작물(作物) 생육시기별(生育時期別)로 어떻게 이동(移動)하는가를 구명(究明)하기 위하여 본양(本良) 사양토(砂壤土) (Typic Udifluvents)에서 Ladino clover를 공시작물(供試作物)로 하여 microplot(D 20cm, L 85cm)시험(試驗)을 수행하였다. 토양수분장력(土壤水分張力)을 0.2, 1.0, 5.0 bar, 및 무관수의 4수준으로 하였을때 염소(鹽素) 이온의 하향(下向)이동은 토양수분(土壤水分) 조건이 좋을수록 빠르게 진행되어 관수점(灌水点) 0.2bar 처리구에서는 5.5개월후에는 모든 처리구에서 microplot 내 토층(土層)에서 Cl이온은 검출되지 않았다. 공시토양(供試土壤)은 유효인산(有效燐酸)함량이 매우높고 사질(砂質)임에도 인산비료(燐酸肥料)로 용과린을 사용하였기 때문에 인산(燐酸) 시용량이 많으며, 관수량이 많았으나 인산(燐酸)이 거의 이동(移動)되지 않아 시용 인산(燐酸)의 대부분이 시비지점(施肥地點)에 분포되어 있었다. 토양수분장력(土壤水分張力)이 낮게 유지된 구의 토양(土壤)일수록 유효태(有效態)로 침출되는 인산(燐酸)이 많고 식물체(植物體)에 의하여 흡수되는 양도 증가 하였다. 최종수확기(最終收穫期)에 무관계구에서는 시용(施用) 인산(燐酸)의 13%가 유효태(有效態)로 침출되고 14%가 작물(作物)에 흡수되었는데 비해 관수점(灌水点) 0.2bar 처리구에서는 24%가 침출되고 23%가 작물(作物)에 의해 흡수(吸收)되었다. A field microplot(D 20cm, L 85cm) experiment filled with Bonryang sandy loam soil (Typic Udifluvents) was conducted to obtain quantitative information on the movement of applied nutrients under diffetent soil moisture regimes and ladino clover cultivation. Chloride moved rapidly with soil water. When soil moisture tension was maintained at loer than 0.2 bar most of the Cl appeared to move outside the microplot 4 month after the microplot installation. Regardless of soil moisture condition, Cl was not detected in the soil due to the fast movement of the Cl beyond the microplot after 5.5 months Although large amount of P and water were applied to the soil of high available P during the field experiment, movement of P was negligible and most of P remained in thc place where applied due to the low solubility of the fused and superphosphate. Phosphate in the soil extracted by Bray No.1 solution and taken up by plant increased with soil moisture. Under the condition of irrigation at 0.2 bar, plant took up 23% of the applied P, and 24% of the P was extracted by Bray NO.1 solution, while plant took up 14% and 13% of the P was turned out to be Bray No.1 P. at thc nonirrigated condition after final harvest.

灌水條件이 砂壤土에서 채소作物의 生育에 미치는 影響

柳寬植(Kwan-Shig Ryu),嚴基哲(Ki-Cheol Eom) 한국토양비료학회 1986 한국토양비료학회지 Vol.19 No.1

土壤水分 條件에 따른 pH 變化와 無灌水 裸地區에서의 養分移動

柳寬植(Kwan-Shig Ryu) 한국토양비료학회 1994 한국토양비료학회지 Vol.27 No.4

灌漑水에 의한 施肥養分의 土壤中 移動에 關한 硏究

柳寬植(Kwan-Shig Ryu),柳順昊(Sun-Ho Yoo),宋寬哲(Kwan-Cheol Song) 한국토양비료학회 1991 한국토양비료학회지 Vol.24 No.2

土壤水分 條件에 따른 Ca, Mg과 K의 移動

柳寬植(Kwan-Shig Ryu),柳順昊(Sun-Ho Yoo),宋寬哲(Kwan-Cheol Song) 한국토양비료학회 1994 한국토양비료학회지 Vol.27 No.4

灌水에 依한 施肥養分의 土壤中 移動에 關한 硏究

柳寬植(Kwan-Shig Ryu),柳順昊(Sun-Ho Yoo),宋寬哲(Kwan-Cheol Song) 한국토양비료학회 1994 한국토양비료학회지 Vol.27 No.3

중성자 수분 측정기를 이용한 노상토의 함수량 측정에 관한 연구

류순호,류관식,송관철,이상모 한국응용생명화학회 1993 한국응용생명화학회 학술발표회 Vol.1993 No.-

우리나라 밭토양의 수분침투속도(水分浸透速度)에 관하여

정영상,류관식,임정남,Jung, Y.S.,Ryu, K.S.,Im, J.N. 한국토양비료학회 1980 한국토양비료학회지 Vol.13 No.1

강우강도가 100mm/hr인 인공강우기(人工降雨器)를 이용(利用)하여 밭토양의 강우침투성(降雨浸透性)을 조사(調査)하고, 침투수(浸透水)의 토양중재분포를 Youngs의 이론식(理論式)에 의(依)하여 추정(推定)한 것과 비교(比較)한 결과(結果)는 다음과 같았다. 1. 토양별 한계강우침투속도(限界降雨浸透速度)는 강우강도 100mm/hr 조건하(條件下)에서 식양토 내지(乃至) 식토(埴土)에서 10mm/hr 이하(以下), 양토에서 10~20mm/hr, 사양토에서 20~30mm/hr, 및 사토(砂土)에서 30mm/hr 이상(以上)으로 나타났으며, 한계강우침투속도(限界降雨浸透速度)에 도달(到達)하는 시간(時間)은 15~20분(分) 이었다. 2. 토양별 표토(表土)의 포화투수계수는 삼각사양토에서 0.47mm/min, 송정식양토에서 0.16mm/min, 그리고 전남미사질식양에서 0.14mm/min로 나타났다. 3. 강우후(降雨後) 토양수분의 재분포상양(再分布相樣)은 Youngs 이론식(理論式)에 의(依)하여 추정(推定)된 것과 거의 비슷한 경향이었다. The infiltration rates of the upland soils on hill side slope were investigated in situ using rainulator of which rainfall intensity was 100mm/hr. The soil moisture profile after the water infiltration was compared with that calculated from Youngs' equation. The results obtained are as follows: 1. Time required for infiltration rate to reach constant during rainfall was 15 to 25 min. The infiltration rate measured after 30 min was considered to be final infiltration rate. 2. The final infiltration rates of clay soils were lower than 10mm/hr., loamy soils 10 to 20., coarse loamy soils 20 to 30, and sandy soils higher than 30mm/hr., respectively. 3. The saturated hydraulic conductivity of the surface soil of Samgag sandy loam was 0.47mm/min., Songjeong clay loam0.16 mm/min., and Jeonnam silty clay loam 0.14mn/min., respectively. 4. The soil moisture profile calculated from Young's equation was in close agreement with measured in situ.

토양개량제(土壤改良劑) 처리(處理)가 토양(土壤)의 물리성(物理性)과 대두(大豆) 수량(收量)에 미치는 영향(影響)

조인상,허봉구,류관식,엄기태,조성진,Jo, In Sang,Hur, Bong Koo,Ryu, Kwan Shig,Um, Ki Tae,Cho, Seong Jin 한국토양비료학회 1987 한국토양비료학회지 Vol.20 No.1

This experiment was designed to find out the effects of soil conditioner, Polyacrylamide (PAM) and Bitumen, on the changes of soil aggregate properties and crop yields. The soil conditioners were treated at the rates of 0.5% and 1% to sandy loam and silty clay loam soils. The aggregate stability, wetting angle, mean weight diameter and air permeability were analyzed. Pot experiments were carried out to investigate the soybean growths and soil property changes after the soil conditioners were sprayed to surface soils. Soil aggregate stability was increased remarkably by the soil conditioner, PAM and Bitumen, treatments. PAM was more effective in sandy loam than silty clay loam, but Bitumen was better in silty clay loam. Wetting angle of the soil was changed slightly by PAM treatment, but it was greatly changed to hydrophobic by Bitumen treatment. Air permeability, water infiltration rate and moisture retention of the soils were increased by surface application of soil conditioners, PAM and Bitumen. The growths of soybean in conditioner applicated pots were better than those of untreated pots from early stage, and the yields were increased 6-13%. 토양개량제(土壤改良劑)가 토양(土壤) 입단형성(粒團形成)에 미치는 영향(影響)을 구명(究明)하고 토양(土壤) 입단(粒團)의 특성(特性)이 토양(土壤) 및 작물생육(作物生育)에 미치는 효과(效果)를 검토(檢討)하기 위하여 토양개량제(土壤改良劑) PAM 및 Bitumen 을 사양토(砂壤土) 및 미사질(微砂質) 식양토(埴壤土)에 각각(各各) 0.5%, 1%씩 처리(處理)하여 입단(粒團)의 안정성(安定性), 습윤각(濕潤角), 평균(平均) 중량직경(重量直徑), 통기성등(通氣性等)을 조사(調査)하고 토양개량제(土壤改良劑)를 미사질(微砂質) 식양토(埴壤土) pot에 각각(各各) 0.5%, 1%씩 표면(表面) 처리(處理)하여 대두(大豆) 생육(生育)과 토양(土壤) 특성(特性) 변화(變化)를 조사(調査)하였다. 1. 토양개량제(土壤改良劑) PAM 및 Bitumen 처리(處理)에 의(依)하여 토양입단(土壤粒團)의 안정성(安定性)은 현저(顯著)히 증대(增大)되었으며 동일농도(同一濃度)에서 PAM은 사양토(砂壤土)에서 Bitumen은 미사질(微砂質) 식양토(埴壤土)에서 더 효과적(效果的) 이었다. 2. PAM 처리(處理)에 의(依)하여 토양(土壤)의 습윤각(濕潤角)은 크게 변화(變化)되지 않았으나 Bitumen 처리(處理)에 의(依)하여 토양(土壤)의 소수성(疎水性)은 크게 증대(增大)되었다. 3. PAM 및 Bitumen 처리(處理)에 의(依)하여 통기성(通氣性) 및 수분(水分)의 침투속도(浸透速度)가 증대(增大)되고 수분함량(水分含量)이 많아졌다. 4. 대두(大豆)의 생육(生育)은 토양개량제(土壤改良劑) 처리(處理)에 의(依)하여 무처리(無處理)보다 초기(初期) 생육(生育)이 양호(良好)하고 수량(收量)은 6-13% 증수(增收) 되었다.

콩 생육시기별 증발산량의 추정모형 설정

孫膺龍,嚴基哲,柳寬植,金基駿 한국작물학회 1988 한국작물학회지 Vol.33 No.3

Lysimeter and field experiments were conducted in Sandy Loam to establish a simple estimation model for evapotranspiration (ET) of soybean for three years (l984-1986). Potential ET (PET) could be estimated by the eq.1 using Pan-evaporation (Eo) and was ranged from 1.1 to 4.6 mm/day during the experiments. PET (mm/day)=1.348+0.573 Eo …(1) Crop coefficient (Kc=maximum ET/PET) could be estimated by the eq.2 using Growth degree (G=days after planting/total growing days) and was ranged from 0.2 to 1.1 and from 0.6 to 1.4 for monoculture cropping and double cropping followed by barley, respectively, during the experiments. Monoculture : Kc=0.016+3.719 G-3.224 G2 …(2), Double cropping : Kc=0.609+2.014 G-2.120 G2 …(2). However, the maximum Kc was shown when G was about 50% and 40% for the monoculture and the double cropping, respectively. Soil water coefficient (f=AET/maximum ET) could be estimated by the eq.3 using soil water tension (Ψ) in 15cm depth. and it was decleased to 0.2 when Ψ was 10 bar. f=0.755-0.537 log │Ψ│…(3) Consequentially, the model to estimate the Actual ET (AET) of soybean was determined as eq.4 with the correction coefficient of -0.380. AET(mm/day)=PET·Kc·f -0.380 …(4) The estimated AET were compared with the measured AET to verify the model established above. The average deviation of the estimated ET(AET) was 0.5782~pm 0.338 (mm/day), and it would be within reasonable confidence range.