• Title/Summary/Keyword: Granite soil

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Effects of Soil Physical properties on Growth in Wasabia japonica Matsum (토양 배지조성이 고추냉이 생육에 미치는 영향)

  • Byeon, Hak-Soo;Seo, Jeong-Sik;Lim, Soo-Jeong;Heo, Su-Jeong;Seo, Sang-Myung
    • Korean Journal of Medicinal Crop Science
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    • v.9 no.1
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    • pp.76-82
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    • 2001
  • This study was conducted to find out the optimum ranges of soil physical properties for wasabi growth by the relationship of soil physical properties and plant growth. Soil bulk density and hardness were higher in decomposition of granite and river sand than hydroball. This root distribution of surface layer was higher in decomposition of granite and river sand than hydroball. Growth characteristics and yield were higher in hydroball than decomposition of granite and river sand. In inlet site, the marketable rhizome weight in decompasition of granite, river sand, hydroball were 298kg/10a, 401kg/10a, 766kg/10a, respectively. But outlet, the weight in three soils were 251kg/10a, 256kg/10a, 633kg/10a, respectively.

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A Study on the Reinforcement Effects of Decomposed Granite Soils according to the Spacing Intensity of Non-woven Geotextile (부직포 배치간격에 따른 화강풍화토의 보강효과에 관한 연구)

  • Cho, Yong-Sung;Lee, Myung-Ho;Kim, Kyeong-Shin
    • Journal of the Korean Geosynthetics Society
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    • v.7 no.1
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    • pp.1-6
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    • 2008
  • In this study, the deformation and strength characteristics for non-woven geotextile-reinforced decomposed granite soil on the triaxial compression test under the same condition as the underground. The specimen of reinforced earth was made of the decomposed granite soil imbedded horizontal in a given space with non-woven geotextile. Four different type of specimen was used in this experimental programme; UR for unreinforced, R-1 for a single non-woven geotextile sheet, R-2 for two sheets, and R-3 for three sheets. According to the testing results, it was found that the strength of the reinforced soil increased when the non-woven geotextile sheets were more used. These results would be applied to the design of reinforced earth structure through the theoretical interpretation method.

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The Influence of Freeze-Thaw Process on the Physical Properties of Weathered Granite Soils (2) (동결.융해반복작용이 화강암풍화토의 물리적성질에 미치는 영향(II))

  • 유능환;유연택
    • Magazine of the Korean Society of Agricultural Engineers
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    • v.31 no.3
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    • pp.70-80
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    • 1989
  • In this research program special triaxial compression tests and dehydration-swelling tests under the condition of freeze-thaw process were conducted to show the effects of freezethaw process on the physical properties of weathered granite soil, and their results as follows; 1.Consolidation settlement of weathered granite soil mass was increased due to freeze-thaw process, and the initial tangent coefficient of dense state was higher than that of loose state. 2.Compression behaviour of soil was increased according to the decrease of freezing temperature, and when the freezing temperature was reached under - 10$^{\circ}$C, the compression rate was not influenced by change of freezing temperature. 3.The experiments showed that the void ratio and permeability of soil were converged into their values of shrinkage limit, and the permeability was higher due to the freeze-thaw process and as the lower the freezing temperature. 4.The decrease of liquid limit was indicated as the lower the freezing temperature, and as more the freeze4haw cycles, the moisture content was shown the lower side. 5.It was shown that the shrinkage was decreased by freeze-thaw process and not influenced by way of freezing temperature, but dehydration rate was higher.

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Assessment of radon potential in the areas covered with granite and gneiss in Korea

  • Je Hyun-Kuk;Chon Hyo-Taek
    • 한국지구물리탐사학회:학술대회논문집
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    • 2003.11a
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    • pp.501-503
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    • 2003
  • Soil-gas radon level and other atmospheric factors have been measured at residual soil profiles that overlie granite bedrock which consists of major geology in Korea for 6 months from November, 2000 to April, 2001. Seasonal variations of soil-gas radon concentration are generally of greater magnitude than day-to-day fluctuations. The highest radon concentrations of 5,131 pCi/L measured during winter season and the lowest radon concentrations of 107 pCi/L during spring season. Two study areas, Bongcheon-dong(granite bedrock) and Seongnam-Yongin(gneiss bedrock) were investigated to assess the radon potential according to their field survey and emanation tests. The mean values of radon decrease in sequentially from Suji-A(813 pCi/L)>Suji-B(757 pCi/L)>Bundang-B(691 pCi/L)>Bundang-A(643 pCi/L)>Bongcheon-dong(513 pCi/L). Estimated soil-gas radon potential using maximum radon emanation ratios of each study area decreases in the order of Bongcheondong(950 pCi/L)>Suji-B(524 pCi/L)>Bundang-A(437 pCi/)>Bundang-B(259 pCi/L)>Suji-A(230 pCi/L) areas. The values of indoor radon and its daughter product concentrations in Bongcheon-dong area show that indoor basement rooms in poor ventilation condition could be classified as extremely high radon risk location of more than 4 pCi/L Rn and 0.02 WL.

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Numerical Investigation of Freezing and Thawing Process in Buried Chilled Gas Pipeline (매설 냉각가스관의 동결-융해에 대한 수치해석 연구)

  • Shin, Hosung;Park, Heungrock
    • Journal of the Korean Geotechnical Society
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    • v.32 no.6
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    • pp.17-26
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    • 2016
  • Characteristic behaviors of geo-structure during freezing and thawing process have to be understood based on fundamental knowledge on phase change in porous soil and interaction between soil and structure. Inversion analysis using published one-dimensional soil freezing tests was conducted to suggest a mechanical model to consider an effect of the ice saturation on Young's modulus. Silty soil was more sensitive to temperature than weathered granite soil and sand, and weathered granite soil was more affected by initial water saturation in stiffness decrease than silty soil. Numerical simulations on chilled gas pipeline showed that shielding effect from surrounding frozen zone around the pipe decreases impact from external load onto the pipe. And a pipe installed in sand backfill showed more heaving due to relatively low stiffness of sand during freezing than that of surrounding in-situ weather granite soil. However, it had more stable stress condition due to effective stress redistribution from external load.

Experimental Study of the Weight Increase of the Oven Dried Weathered Granite Soil due to Moisture Absorbed during Air Exposure (노건조된 화강풍화토의 공기 중 노출시 습윤무게 증가에 관한 실험적 연구)

  • Kim, Suk-Joo
    • The Journal of Engineering Geology
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    • v.32 no.3
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    • pp.401-410
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    • 2022
  • This work reports an oven drying test performed on weathered granite soil from Yecheon, Korea, in order to find an effective method for measuring the weight of pure soil particles. After samples were oven dried, weights measured following desiccation using the method specified by the Korean Industrial Standard (KS F) were compared with weights measured without prior desiccation. Soil samples exposed to air for 45 min after oven drying absorbed moisture from the air and gradually increased in weight. When a desiccator was used, results measured 30 s after exposure to air indicated weight increases of 0.103-0.735% (depending on the particle size of the soil) relative to equivalent samples measured without desiccation. Using a desiccator after oven drying leads to overestimation of the pure soil weight. Therefore, measuring the weight of a soil sample immediately after oven drying without using a desiccator can reduce the error of weight measurement.

Soil-Water Characteristic Curves for Drying and Wetting Processes in Granite-Weathered Soil Based on Variations in Fine Contents (세립분 함량을 고려한 국내 화강풍화토의 건조 및 습윤 함수특성곡선 분석)

  • Lee, Sangbeen;Ryou, Jae-Eun;Seo, Jinuk;Jung, Jongwon
    • Journal of the Korean Geotechnical Society
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    • v.40 no.1
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    • pp.47-54
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    • 2024
  • In current slope stability analysis techniques, slope stability is evaluated based on the saturated-soil theory. However, soil-water characteristics change frequently depending on the climate. Therefore, because the saturated soil theory has limitations, the application of the unsaturated soil theory is necessary for slope stability. It is also important to evaluate the engineering properties of unsaturated soil because the capillary absorption capacity is reduced due to heavy rain, thereby causing a reduction in slope stability. In this study, soil-water characteristic tests were performed using four samples with different fine contents (0%, 10%, 20%, and 30%) using granite-weathered soil in domestic production areas. In particular, to consider the previously conducted drying process as well as the evaluation of stability due to heavy rain on the actual slope, a wetting process was conducted, in which the water content was increased. In addition, the van Genuchten (1980) model, which is the most consistent theoretical equation for the experiment, was used with various theoretical equations, and the parameters were analyzed according to the fine content of the granite-weathered soil for the drying and wetting processes.

Frost Heaving Pressure and Physical Characteristics of the Railway Roadbed Materials (철도노반재료의 동상팽창압 및 물리적 특성 평가)

  • Shin Eun-Chul;Park Jeong-Jun;Kim Jong-In
    • Journal of the Korean Society for Railway
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    • v.8 no.1
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    • pp.57-62
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    • 2005
  • The frost heaving pressure can be a problem for weakening of the railway roadbed material. This study was initiated to investigate the soils frost heaving pressure and physical characteristics(Liquid limit, permeability, SEM analysis) resulting from freezing and freezing-thawing cycle process. Therefore, upon freezing a saturated soil in a closed-system from the top, a considerable pressure was developed. Weathered granite soils, sandy soil were used in the laboratory freezing test which sometimes subjected to thermal gradients under closed-systems. The frost heaving pressure arising within the soil samples and the temperature of the samples inside were monitored with elapsed time. The degree of saturation versus heaving pressure curve is also presented for weathered granite soil and the maximum pressure is closely related to this curve. Based on the laboratory test results, fine-grained soils with strong attractive forces between soil grains md water molecules, and additional water is attracted into the pores leading to further volume changes and ice segregation.

Comparison of the Structure of Grassland Communities and the Performance of Galcicoles and Calcifuges on the Limiestone and the Granite Areas (石灰岩과 花崗岩地帶에서 草地群落의 構造 및 好石灰植物과 嫌石灰植物의 成就度 比校)

  • Kwak, Young-Se;Chin, Kuk-Jeong;Min, Kuem-Suk;Kim, Joon-Ho;Choung, Yeon-Sook
    • The Korean Journal of Ecology
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    • v.17 no.2
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    • pp.105-112
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    • 1994
  • Structure of grassland communities was investigated, and performance of populations of Themeda triandra var. japonica and Miscanthus sinensis were compared on limestone and granite soils. Forty three and forty taxa occurred on the limestone and granite grasslands, respectively, but their similarity was very low. Shoot height and number of hills per patch, as a measure of performance, of Themeda on the limestone grassland were higherthan those on the granite grassland. In contrast, shoot height and number on hills per patch of Miscanthus were higher on limestone than granite grassland. Evidence shows that poor growth of Micanthus population on the limestone soil was associated with higher content of insoluble divalent cations than soluble ones in shoot tissue.

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Estimation of Chemical Forms of Phosphate Released from the Paddy Soils with Different Effect of Phosphate Application (인산비옥도(燐酸肥沃度)가 상이(相異)한 답토양(畓土壤)에서 환원용출(還元溶出)되는 인산형태(燐酸形態)의 추정(推定))

  • Hong, Jung-Kuck
    • Korean Journal of Soil Science and Fertilizer
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    • v.15 no.2
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    • pp.89-94
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    • 1982
  • 1. Solubility diagram was used to estimate Chemical form of the Soil phosphates which supply phosphorus into soil solutions under submerged condition with soils originated from granite and basalt rocks. The granite origin soils with different amounts of available phosphorus have no effect of phosphate application on rice yield, while the basalt origin soil has the big effect. 2. Almost same pattern of change in pH and concentrations of phosphorus and cations in the soil solutions during the submerging period was. shown. Almost no difference in the values was recognized between NPK and NK treatments of the granite origin soils, but the difference of the basalt origin soil was recognized. 3. it was estimated from solubility diagram that phosphorus concentration in the soil solutions was governed by phosphate applied and variscite in the soils for the early stage of submerging period, and then it became to be governed by vivianite in the soils.

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