• 한국토양비료학회지
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• 제31권3호
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• pp.266-270
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• 1998

밭토양의 수용성 인산농도의 예측방법을 개발 할 목적으로 토양특성이 다양한 40개 토양에 대하여 0.01 M $CaC1_2-P$와 유효인산 및 인산흡수능 등과의 관계를 검토한 결과, 직선회귀관계에서 0.01 M $CaC1_2-P$와의 결정계수는 유효인산이 $0.479^{**}$, 부영양화인산이 $0.281^{**}$이었으며 토양의 인산흡수능중에는 인산흡수량이 $-0.465^{**}$, 인산흡수계수가 -$-0.056^{NS}$이었다. 0.01 M $CaC1_2-P$와 독립 변수인 유효인산과 인산흡수능을 함께 고려한 2차 다항 회귀관계로 보면 결정계수가 $0.745^{**}$로 향상되었고 독립변수로 유효인산과 인산흡수계수를 함께 고려하면 결정계수가 $0.566^{**}$ 이었으며 유효인산/인산흡수량의비를 독립변수로 하여 만든 지수함수식(指數函數式)에서는 결정계수가 0.818로 크게 향상되었다.

• Advances in concrete construction
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• 제7권3호
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• pp.143-150
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• 2019

This study presents the fracture properties of nano modified medium strength concrete (MSC). The nano particle used in this study is nano silica which replaces cement about 1 and 2% by weight, and the micro steel fibers are added about 0.4% volume of concrete. In addition to fracture properties, mechanical properties, namely, compressive strength, split tensile strength, and flexural strength of nano modified MSC are studied. To ensure the durability of the MSC, durability studies such as rapid chloride penetration test, sorptivity test, and water absorption test have been carried out for the nano modified MSC. From the study, it is observed that significant performance improvement in nano modified MSC in terms of strength and durability which could be attributed due to the addition pozzolanic reaction and the filler effect of nano silica. The incorporation of nano silica increases the fracture energy about 30% for mix without nano silica. Also, size independent fracture energy is arrived using two popular methods, namely, RILEM work of fracture method with $P-{\delta}$ tail correction and boundary effect method. Both the methods resulted in nearly the same size-independent $G_F$ irrespective of the notch to depth ratio of the same specimen. This shows evidence that either of the two procedures could be used in practice for analysis of cracked concrete structures.

• 한국토양비료학회지
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• 제19권3호
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• pp.251-268
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• 1986

Selecting a site for the safe disposal of radioactive waste requires the evaluation of a wide range of geologic, mineralogic, hydrologic, and physicochemical properties. Although highly diverse, these properties are in fact interrelated. Site requirements are also diverse because they are influenced by the nature of the radionuclides in the waste, for example, their half-lives, specific energy, and chemistry. A fundamental consideration in site selection is the mineralogy of the host rock, and one of the most ubiquitous mineral groups is clay minerals. Clays and clay minerals as in situ lithologic components and engineered barriers may playa significant role in retarding the migration of radionuclides. Their high sorptivity, longevity (stability), low permeability, and other physical factors should make them a very effective retainer of most radionuclides in nuclear wastes. There are, however, some unanswered questions. For example, how will their longevity and physicochemical properties be influenced by such factors as radionuclide concentration, radiation intensity, elevated temperatures, changes in redox condition, pH, and formation fluids for extended periods of time? Understanding of mechanisms affecting clay mineral-radionuclide interactions under prevailing geochemical conditions is important; however, the utilization of experimental geochemical information related to physicochemical properties of clays and clay-bearing materials with geohydrologic models presents a uniquely challenging problem in that many assessments have to be based on model predictions rather than on experiments. These are high-priority research investigations that need to be addressed before complete reliance for disposal area performance is made on clays and clay minerals.

• 한국토양비료학회지
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• 제36권6호
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• pp.384-390
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• 2003

논토양의 환경기준 인산지표 예측기술개발을 위하여 논토양 35점을 $25{\pm}1^{\circ}C$ 에서 1, 2, 4주간 담수 항온한 결과 담수 항온 전 풍건 토양의 $0.01M\;CaCl_2$ 가용인산 함량과 유효인산 함량 및 인산흡수능의 관계는 습토로 분석할 경우 상관계수의 크기는 유효인산/인산흡수량>유효인산>유효인산/인산흡수계수>인산흡수량>총인산>인산흡수계수 순이었고, 항온기간별 상관계수 크기는 습토로 분석할 경우 항온이 길어질수록 상관계수는 점점 낮아 졌으나, 건토로 분석할 경우는 이와 반대 경향이었다. 토양의 유효인산 함량과 인산흡수량을 활용하여 $0.01M\;CaCl_2$ 가용인산 농도를 추정할 수 있는 관계식 $0.01M\;CaCl_2-P=0.0828$ (유효인산/인산흡수량) + 0.0374을 얻었으며, 이러한 관계식은 토양의 인산 함량과 인산흡수 특성을 고려하여 작물재배에 필요한 적정 유효인산 함량의 추정과 토양 인산의 유실 가능성 등을 예측하는데 활용될 수 있을 것이다.