산지토양(山地土壤)의 특성(特性)과 개량(改良)

류인수,Ryu, In-Soo 한국토양비료학회 1979 한국토양비료학회지 Vol.11 No.4

Majority of reclaimable soils in hillside lands in Korea are red yellow soils, with exception in Jeju island, where most of reclaimable hillside lands are composed of volcanic ash soils. Songjeong, Yesan and Samgag series are the major soil series of red yellow soils which are available for the reclamation. When observed in the fields, they are distinguished as reddish brown clay loam, red yellow sand loam and yellowish brown sand loam. They have moderately good physical properties but their chemical properties are generally poor for crop cultivations. The chemical properties of red yellow soils, as compared to long time cultivated (matured) soils, are characterized by very low pH, high in exchangeable Al content and phosphorus fixation capacity. Also extraodinary low available phosphorus and organic matter contents are generally observed. On the other, the chemical properties of volcanic ash soils are characterized by high armophous Fe and Al hydroxides and organic matter contents, which are the causative factors for the extremely high phosphorus fixation capacity of the soils. The phosphorus fixation capacity of volcanic acid soils are as high as 5-10 times of that of red yellow soils. Poor growth of crops on newly reclaimed red yellow soils are mainly caused by very low available P and pH and high exchangeable Al. Relatively high P fixation capacity renders the failure of effective use of applied P when the amount of application is not sufficient. Applications of lime to remove the exchangeable Al and relatively large quantity of P to lower the P fixation capacity and to increase the available P are the major recommendations for the increased crop production on red yellow hillside soils. Generally recommendable amounts of lime and P to meet the aforementioned requirements, are 200-250kg/10a of lime and $30-35kg\;P_2O_5/10a$. Over doses of lime. frequently induces the K, B, arid Zn deficiencies and lowers the uptake of P. In volcanic ash soils, it is difficult to alter the exchangeable Al and the P fixation capacity by liming and P application. This may be due to the peculiarity of volcanic ash soil in chemical properties. Because of this feature, the amelioration of volcanic ash soils is not as easy as in the case of red yellow soils. Application of P as high as $100kg\;P_2O_5/10a$ is needed to bring forth the significant yield response in barley. Combined applications of appropriate levels of P, lime, and organic matter, accompanied by deep plowing, results in around doubling of the yields of various crops on newly reclaimed red yellow soils.

제주도토양의 무기태인산(無機態燐酸) 조성(組成)과 유효인산의 정량법(定量法) 비교(比較)

신철우,류인수,윤정희,Shin, Cheol-Woo,Ryu, In-Soo,Yoon, Jung-Hui 한국토양비료학회 1981 한국토양비료학회지 Vol.13 No.3

4종(種)의 제주도 토양에 인산질비료(燐酸質肥料)를 시용(施用)한후 무기태인산(無機態燐酸)의 형태별(形態別) 함량변화와 수종 침출액(浸出液)에 의한 유효인산(有效燐酸) 침출량(浸出量)을 실내실험으로 조사(調査)하여 비교(比較) 검토한 결과(結果)는 다음과 같다. 1. 총인산에 대한 무기태인산(無機態燐酸)의 비율(比率)은 토양종류에 따라 달라 Al-P는 6.9-28.8%, Fe-P는 24.1~26.9%, Ca-P는 7.4~11.9% 범위이며 유효인산(有效燐酸)은 0.7-8.0%로 매우 낮았다. 2. 토양종류별로 인산(燐酸)을 시용(施用)한 후(後) 60일후(日後)에 조사(調査)한 토양인산의 형태별(形態別) 조성(組成)을 본 결과(結果) 흑색토(黑色土)에서는 Al-P>Fe-P> Ca-P, 농암갈색토(濃暗褐色土)에서는 Fe-P> Al-P> Ca-P, 암갈색토(暗褐色土)에서는 Fe-P> Ca-P> Al-P. 적황색토(赤黃色土)에서는 Fe-P> Al-P> Ca-P의 순(順)으로 나타나 토양별 차이(差異)가 있었다. 3. 5종(種)의 침출액(浸出液)으로 토양별 유효인산(有效燐酸)을 검정한 결과(結果) Bray No.2법(法)은 토양종류에 관계없이 어느 토양에서나 침출능(浸出能)이 컸으나 그 외의 방법(方法)들은 토양의 종류별(種類別)로 침출능(浸出能)이 상이(相異)하게 나타났다. 4. 유효인산(有效燐酸) 침출방법(浸出方法)과 무기태인산(無機態燐酸) 함량(含量)과의 관계에서 Bray No.2법(法)은 Ca-P와 5%수준에서, Olsen법(法)은 Al-P, Fe-P, Ca-P 및 Total-P와 각각 1%수준에서 유의(有意)한 관계를 보였다. Laboratory experiment was carried out to investigate the changes in the amount of inorganic phosphorus fractions of native and applied phosphorus and to compare the some analytical methods of soil phosphorus in volcanic ash. The rates of inorganic phosphorus to total-pP were varied with the kinds of soil in the ranges of 6.9 to 28.8% for Al-P, 24.1 to 26.9% for Fe-P, 7.4 to 11.9% for Ca-P and 0.7 to 8.0% for available phosphorus. The composition of inorganic phosphorus after incubation for 60 days was in the order of Al-P>Fe-P>Ca-P in Black soil, Fe-P>Al-P>Ca-P in Very dark brown soil, Fe-P>Ca-P>Al-P in Dark brown soil and Fe-P Al-P>Ca-P on Red yellow soil. The amounts of phosphorus extracted from soil varied with the methods for available phosphorus estimation. The magnitute of available P measured by Bray No. 2 method was the greatest. In relationship between inorganic phosphorus forms and available phophorus, Bray No. 2 method was closely related to Ca-P only and Olsen method correlated to Al-P, Fe-P, Ca-P and Total-P.

홍적태지(洪積台地)에 발달(發達)된 중점질(重粘質) 토양(土壤)(화동통(華東統))에 대(對)한 인산(燐酸) 규산(珪酸) 및 유기물(有機物)의 시용효과(施用效果)

안상배,류인수,Ahn, Sang-Bai,Ryu, In-Soo 한국토양비료학회 1978 한국토양비료학회지 Vol.10 No.4

담수하(湛水下)에서 환원발달(還元發達)이 극(極)히 부진(不進)한 적황색계중점질토양(화동통)((赤黃色系重粘質土壤)(華東統))의 개량방법(改良方法)으로서 인산(燐酸), 규산(珪酸) 및 유기물(有機物)의 효과를 기대(期待)하였던바 1. 인산(燐酸)의 효과는 매우 컸으며 인산(燐酸) 56kg/10a의 시용(施用)으로 약(約) 20%의 증수(增收)를 가져왔다. 2. 인산(燐酸)에 의(依)한 증수(增收)는 주(主)로 분벽수(分蘗數) 증가(增加)에 기인(起因)되었다. 인산(燐酸)에 대(對)한 품종간(品種間) 반응(反應)에서 주당경수(株當莖數)의 최고증가(最高增加)는 통일(統一) 3.6경(莖), 진흥(振興) 1.9경(莖)이었으나 등숙률(登熟率)은 반대(反對)로 통일(統一)에서 4% 감소(減少)되었고 진흥(振興)에서는 3% 증가(增加)되었다. 3. 유수형성기(幼穗形成期)와 출수기(出穗期)의 식물체중(植物體中) $P_2O_5$ 함량(含量)과 수량간(收量間)에는 1% 수준(水準)에서 높은 백관관계(栢關關係)가 있었으나, 출수기(出穗期)의 $P_2O_5$ 함량(含量)과 수량간(收量間)에는 유의적상관(有意的相關)이 없었다. 최고수량(最高收量)을 얻을 수 있는 유수형성기(幼穗形成期)의 인산함유률(燐酸含有率)은 0.8%이었다. 4. 규산(珪酸)의 효과는 통일(統一)에서는 인정(認定)되지 않았으나 진흥(振興)에서는 컸고 퇴비(堆肥) 및 왕겨의 시용효과도 진흥(振興)에서만이 현저하였다. 5. 규산(珪酸) 및 석회(石灰)의 시용(施用)은 경엽중(莖葉中)의 질소함유률(窒素含有率)을 저하(低下)시켰으며 특(特)히 통일(統一)에서 현저히 감소(減少)되었다. 이로 볼 때 이들 효과의 발현(發現)을 위(爲)하여는 특(特)히 통일(統一)의 경우 질소(窒素)의 증시(增施)가 수반되어야 할 것으로 보였다. A field experiment was conducted to confirm the effect of phosphorus, calcium silicate and different kinds of organic matter to a red-yellow heavy clay textured paddy soil, developed on alluvial terrace. 1. The yield response of phosphorus was very high in both Tongil (Indica x lap.) and Jinheung (Japonica type) varieties. Twenty percent of yield increase with 56kg $P_2O_5$ per 10a. 2. Yield increase by application of phosphorus was closely resulted from increase of tillers per plant. The increases of tillers per plant as observed at harvesting stage by phosphorus fertilization were 3.6 tillers in Tongil, 1.9 in Jinheung, while ripening ratio adversely was decreased 4% in Tongil and increased 3% in Jinheung. 3. High correlation between P content and yield was found at earformation and heading stages. The content of P in rice plant necessary to produce maximum yield in this soil was 0.8 percent at earformation stage. 4. The effect of silicate was not significant for Tongil but was obvious for Jinheung, and the effect of compost and rice husk was also significant for Jinheung. 5. Addition of silicate and lime to phoshorus treatment decreased the nitrogen content of rice plant, especially in Tongil. Accordingly, significant responses of silcate and lime seems be appeared by increasing the rate of nitrogen application.

수도재배기간중(水稻栽培期間中)의 저온(低溫) 및 이앙기(移秧期) 한발출현유형(旱魃出現類型)과 분포(分布)

이량수,정영상,류인수,한원식,김병찬,Lee, Yang-Soo,Jung, Yeong-Sang,Ryu, In-Soo,Han, Won-Shig,Kim, Byung-Chan 한국토양비료학회 1983 한국토양비료학회지 Vol.16 No.2

우리나라 수도작기간중(水稻作期間中)의 재해기상(災害氣象) 위험도(危險度)를 파악(把握)하기 위하여 냉해(冷害)와 한발(旱魃)과 출현빈해(出現頻害)와 역별분포등(域別分布等)에 대한 조사(調査)를 실시한 결과(結果) 다음과 같았다. 1. 1970년(年) 이후(以後) 한발(旱魃)과 저온출현(低溫出現)이 많아졌으며 침수해(浸水害)의 발생은 감소(減少)하였다. 2. 저온유형(低溫類型)의 출현빈도(出現頻度)는 전기저온형(前期低溫型)과 장기저온형(長期低溫型)이 많았으며 지역별(地域別)로는 수원(水原) > 대구(大邱) > 광주(光州)의 순(順)이었다. 3. 수도이앙기(水稻移秧期) (4~6월(月)) 강수량(降水量)의 년도별(年度別) 변화 주기(週期)는 약(約) 15년(年)으로 나타나며 최근년(最近年)은 소강우(少降雨) 주기(週期)에 해당하는 경향(傾向)이었다. 4. 이앙기(移秧期) 한발빈도(旱魃頻度)는 대구(大邱), 포항지역(浦項地域)에서 가장 많았고, '82년도(年度) 강수량(降水量)과 저수율(貯水率)을 기준(基準)한 한발극심(旱魃極甚) 지역(地域)은 영남내륙(嶺南內陸) 및 서남해안지대(西南海岸地帶)이었다. The occurrence and regional distribution of low temperature and drought during rice cropping period in Korea were studied to characterize the climatic impacts. The long term changes in rice yield, air temperature and precipitation were analyzed, and regional distributions were characterized. The significant climatic impacts on rice yield were heavy rain or flood, drought and low temperature. Since 1910, the occurrence of drought was 29 times, that of flood was 24 times and that of low temperature was 9 times; however, the drought and flood damages were decreased due to expansion of irrigation system since 1970 but low temperature damage was remarkedly increased. The long term changes in air temperature since 1908 in Suweon showed that the 5-year moving average from July to August decreased while that from May to June increased. The occurrence probability of the long term and early term low temperature types were the greatest in Korea and were in order of Suweon, Daegu and Kwangiu. The long term changes in 10-year moving average precipitation from April to June showed a 15 year cycle and recent years were in low precipitation period. The drought frequencies were the highest in Daegu and Pohang area. According to the precipitation from April to June and resevtoir storage at late June, the severest dry area were the Youngnam inland and the southwest coastal area.

主要 田作物에 對한 加里成分의 肥效

柳寅秀(In Soo Ryu) 한국토양비료학회 1977 한국토양비료학회지 Vol.10 No.3

置換性 A1 含量에 따른 石炭所要量 決定에 關한 硏究

柳寅秀(In Soo Ryu),趙成鎭(Seong Jin Cho),陸昌洙(Chang Soo Yuk) 한국토양비료학회 1974 한국토양비료학회지 Vol.7 No.3

土壤肥沃度 增進 및 諸 技術要因에 依한 肥料 消費趨勢 展望

柳寅秀(In-soo Ryu) 한국토양비료학회 1976 한국토양비료학회지 Vol.9 No.3

低丘陵 谷間地 畓土壤(芝山統과 龍池統)의 特性과 施肥反應에 關한 硏究

柳寅秀(In-Soo Ryu),愼鏞華(Yong-Hwa Shin),李炯兌(Dong-Tae Lee) 한국토양비료학회 1976 한국토양비료학회지 Vol.9 No.4

畓 類型別 生産力과 窒素反應

柳寅秀(In-Soo Ryu),李承宅(Sung-Tack Lee),朴天緖(Chon-Suh Park),愼鏞華(Yong-Hwa Shin) 한국토양비료학회 1977 한국토양비료학회지 Vol.10 No.1

火山灰土壤에서의 燐酸의 施用量과 施肥法 및 硅灰石의 効果

柳寅秀(In-Soo Ryu),尹禎熙(Jung-Hui Yoon),金仁卓(In-tak Kim) 한국토양비료학회 1978 한국토양비료학회지 Vol.11 No.1