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사양토(砂壤土) 및 양토(壤土)에서 토양질소(土壤窒素) 무기화(無機化)에 미치는 석회(石灰)와 전분(澱粉)의 영향(影響)
윤순강,이석하,이명철,Yun, Sun-Gang,Lee, Suk-Ha,Lee, Myung-Cheol 한국토양비료학회 1991 한국토양비료학회지 Vol.24 No.3
토성(土性)을 달리하는 두 토양(土壤)(사양토(砂壤土), 양토(壤土))을 공시(供試)하여 무처리, 석회(3%, w/w), 전분(3% w/w), 및 석회+전분처리를 하고 토양수분을 포장용수량(圃場溶水量)의 80%로 조절(調節)한 뒤 항온(恒溫)($30+/-0.1^{\circ}C$, 6주간(周間)) 처리하여 pH와 무기태(無機態)질소함량 변화를 조사(調査)하였다. 양토(壤土)에서 항온에 따른 pH는 석회와 석회+전분처리에서 항온 1주 후에 급격히 pH가 증가(增加)되었고, 무처리에서는 항온 전보다 pH가 낮아졌다. 사양토에서는 석회처리시 양토에서와 유사(類似)한 pH증가를 보였으나 석회+전분처리에서는 항온 2주째부터 낮아졌다. 그리고 무처리와 전분처리에서는 항온(恒溫) 전(前)과 큰 차이가 없었다. 양토(壤土)에서 $NH_4-N$은 항온 후 3주부터 증가(增加)되기 시작하여 5주째 최대치(最大値)를 보였고 6주째는 다소 감소(減少)되었다. $NO_3-N$은 석회, 무처리에서 항온기간경과에 따라 pH상승(上昇)과 $NO_3-N$축적간에 정(正)의 상관관계(相關關係)를 보였으며, 전분, 석회+전분처리에서는 오히려 항온 전(前)보다 낮아졌다. 사양토(砂壤土)에서 $NH_4-N$은 양토에서와 유사(類似)하여 항온 3주째부터 증가되었으며, 처리별로는 양토에서와는 달리 석회+전분처리에서 매우 높았다. Effects of liming and starch application on the soil pH and mineralization of organic nitrogen were compared to control at $30+/10^{\circ}C$ incubation for six weeks in two soil types(loam, sandy loam) adjusted with 80% of field moisture capacity. 1. While soil pH was increased abruptyl one week after incubation in loam applied with lime and lime+starch, it tended to decrease at control during incubation period. Liming on sandy loam increased soil pH, and application of lime+starch together showed high pH at first week of incubation which was lowered slowly after wards. Significant changes in soil pH was not detected at control or starch application only. 2. The content of $NH_3-N$ in loam started to increse three weeks after incubation, and was maximized at fifth week. Positive correlation was shown at control during incubation period between soil pH and $NO_3-N$ content. Level of $NO_3-N$ content applied with starch or lime+starch was low compared to control. 3. The $NH_4-N$ content was high when sandy loam was applied with lime+starch together. At the first week of incubation, the $NO_3-N$ content was high at control or lime application.
Cd 안정동위체를 이용한 토양과 식물계에서 Cd의 거동해석
윤순강(Sun-Gang Yun),정구복(Gu-Bok Jung),김원일(Won-Il Kim),이종식(Jong-Sik Lee),김민경(Min-Kyeong Kim),김진호(Jin-Ho Kim),신중두(Joong-Du Shin),이덕배(Deog-Bae Lee),김삼권(Sam-Cwan Kim) 한국토양비료학회 2008 한국토양비료학회지 Vol.41 No.3
본 연구는 모재가 상이한 산지토양과 폐광인근 지역에 광미사 중 Cd 안정동위체의 분포와 토양 중에서 Cd 안정동위체 간의 관계를 해석하고, Cd 안정동위체 별 식물흡수 정도를 조사하기 위하여 광미사를 처리하고 고추와 콩을 재배하면서 식물체 지상부와 뿌리 중에 Cd의 안정동위체 분포에 대하여 조사하였다. 모재가 상이한 3가지(화강암, 변성암, 퇴적암) 토양에서 Cd의 8개 안정동위체(Cd<SUP>106, 108, 110, 111, 112, 113, 114, 116</SUP>)들의 토양 중 존재비는 토양별 차이가 없었다. 그러나 토양 모재차이에 관계없이 토양 중 Cd의 안정동위체 간에 관계는 크게 4가지의 분포특성을 나타내었다. Cd<SUP>106</SUP>/Cd<SUP>111</SUP> 간에는 직선형관계, Cd<SUP>114</SUP>/Cd<SUP>108 </SUP>간에는 2차식관계, Cd<SUP>110</SUP>/Cd<SUP>106</SUP> 간에는 역2차식 관계, Cd<SUP>110</SUP> / Cd<SUP>113</SUP> 간에는 클러스터형 관계를 보였다. 콩과 고추 중에 Cd은 안정동위체 중 Cd<SUP>116</SUP>, Cd<SUP>114</SUP>, Cd<SUP>112</SUP>이 주를 이루었고 존재비로는 Cd<SUP>116</SUP>이 가장 많았다. 반면 콩과 고추의 뿌리에서는 Cd<SUP>116</SUP>의 존재비가 감소하고 다른 7종류의 Cd 안정동위체 존재비가 상대적으로 증가하는 경향을 보였다. This experiment was conducted to describe the distribution of stable isotope Cd in the mine tailing and uncultivated soils derived from different parent rocks (Igneous rock, Metamorphic rock, and Sedimentary rock) as well as the movement of Cd isotopes from soil to plants, soybean and pepper. The results showed that there was no significant difference in isotopic ratios in soil among the eight kinds of stable isotope of Cd. However the relationship among isotopic ratios of stable isotope of Cd in soils were classified to four types, linear type between Cd<SUP>106</SUP>/Cd<SUP>111</SUP> and Cd<SUP>108</SUP>/Cd<SUP>111</SUP>, quadratic type between Cd<SUP>114</SUP> / Cd<SUP>108</SUP> and Cd<SUP>111</SUP>/Cd<SUP>110</SUP>, reverse quadratic type between Cd<SUP>110</SUP>/Cd<SUP>106</SUP> and Cd<SUP>108</SUP> / Cd<SUP>116</SUP>, and cluster type between Cd<SUP>110</SUP>/Cd<SUP>113</SUP> and Cd<SUP>116</SUP>/Cd<SUP>113</SUP>. While the individual stable isotopes of Cd in root were remained except on the plot of pepper without mine tailing application. Cd<SUP>116</SUP>, Cd<SUP>114</SUP>, and Cd<SUP>112</SUP> played active roles among other stable isotopic Cds in bean and red pepper, and Cd<SUP>116</SUP> was ranked the highest abundance ratio. Contrary to crop itself, the abundance ratios of Cd116 in bean and read pepper roots were decreased, and the ones of other Cds were relatively increased.
요소(尿素)(Urea)를 시용(施用)한 초지(草地)의 토양단면(土壤斷面)에서 무기태질소(無機態窒素) 함량(含量)의 계절적(季節的) 변화
윤순강,유순호,Yun, Sun-Gang,Yoo, Sun-Ho 한국토양비료학회 1991 한국토양비료학회지 Vol.24 No.3
요소(urea)를 시용한 초지의 토양단면에서 무기태질소의 계절적 함량변화를 조사하기 위하여 질소 시용수준(施用水準)을 0, 14, 28 kg/10a로 하고 목초를 재배하면서 봄(5.26), 여름(7.27), 가을(10.18)철에 토양시료를 토양깊이 100cm 까지 20cm 간격으로 채취하여 분석(分析), 검토(檢討)한 결과는 다음과 같다. 1. 봄 철에 질소 무시용구에서는 $NH_4-N$ 함량이 높았으나 14, 28 kg N/10a 처리에서는 $NO_3-N$ 함량이 증가(增加)되었고 $NH_4-N$, $NO_3-N$ 함량은 토양깊이가 깊을수록 모두 감소되는 경향을 보였다. 2. 여름 철 토양 중 $NO_3-N$ 함량(含量)은 0 N < 14 N <28 N 순으로 증가되었고 28 N 처리에서는 토양중 평균 $NO_3-N$ 함량이 42 ppm였다. 3. 가을 철에는 $NH_4-N$ 함량은 전 처리에서 여름 철과 큰 차이가 없었으나 $NO_3-N$ 함량은 여름 철에 비하여 크게 감소(減少)되어서 14 N, 28 N 처리에서 각각 7, 14 ppm 이하로 낮아졌다. 4. 토양 중 전질소 함량은 봄 철에 토양깊이 0~20cm에서 0 N에 비하여 28 N 처리에서 0.042% 낮았으며 전체적으로는 0 N과 28 N 처리 사이에 차이가 적었다. 그러나 토양 전질소(全窒素) 함량에 대한 무기태질소(無機態窒素) 함량 비율은 0 N과 28 N 처리 간에 차이가 컸는데 여름 철에 28 N 처리의 토양깊이 40~100cm에서 무기태질소(無機態窒素) 함량비율은 0 N 처리에 비하여 크게 증가(增加)되었으며 특히 토양깊이 80~100cm에서는 0 N에 비하여 2배 이상 증가되었다. Field experiment was conducted to investigate the seasonal change in inorganic nitrogen content in grassland soil profile after urea application. Urea was applied at the levels of 0 (0N), 14 (14N), and 28 (28N) Kg N per 10a. Soil samples were taken at every 20 cm interval upto 100 cm soil depth in spring (May 26), summer (July 27), and autumn (October 18) and analysed for total and inorganic nitrogen ($NH_4-N$ and $NO_3-N$). The results obtained are as follows ; 1. In spring, the $NH_4-N$ content of ON treatment was higher than $NO_3-N$ content both in surface and subsoil. The urea application increasing both $NH_4-N$ and $NO_3-N$ contents in the surface soils and these contents decreased with soil depth. 2. In summer, increase in urea application rate elevated the $NO_3-N$ content in soil profile of 0 to 100cm and the content reached upto 42 ppm in the 28N treatment. 3. The seasonal difference in $NH_4-N$ content between summer and autumn was insignificant throughout soil profile. Soil $NO_3-N$ content in autumn were 7 and 14 ppm for 14N and 28N respectively, showing very low values compared with that of summer. 4. The ratio of inorganic nitrogen to total nitrogen increased with soil depth and with urea application rates.
윤순강 ( Sun Gang Yun ),김원일 ( Won Il Kim ),김진호 ( Jin Ho Kim ),김선종 ( Seon Jong Kim ),고문환 ( Mun Hwan Koh ),엄기철 ( Ki Cheol Eom ) 한국환경농학회 2002 한국환경농학회지 Vol.21 No.4
Irrigation water quality along Donjin river watershed was monitored to find a possible pollutants, for maintaining water quality to achieve food safety through water quality preservation of river. As a pollution indicators, such as Biological Oxygen Demand(BOD), Chemical Oxygen Demand(COD), Total Nitrogen(T-N), and Total Phosphate(T-P) in Dongjin river were examined from May to November in 2001. The results were as follows : The BOD level of Dongji n river ranged from 2.84 to 6.45 mg/L, which would be in a Ⅱ~Ⅳ grade of the potable water criteria by Ministry of Environment. Averaged BOD level of downstream DJ6(After Jeongupcheon confluence) was 4.07 mg/L. The average COD level of Dongjin river ranged from 11.20 to 32.96 mg/L. COD level of DJ6 rapidly increased rapidly after the junction of Dongjin river and Jungupcheon because it showed the latter had relatively high pollution level. T-N content were significantly high in all sites of Dongjin river ranged through 4.16 to 5.84 mg/L. T-P examined high concentration than another thing point by 0.19 mg/L after Jeongupcheon confluence as BOD and COD. COD of main stream was expressed high concentration to dry season after rainy season. In case of T-P, pollution degree of dry season before rainy season appeared and examined that quality of water was worsened go by dry season after rainy season. The water quality of Dongjin river was deteriorated with inflow of Jungupcheon polluted by municipal and industrial sites near Jungup city.