• Geomechanics and Engineering
• /
• 제22권2호
• /
• pp.173-185
• /
• 2020

Calcareous soil is originated from marine biogenic sediments and weathering of carbonate rocks. The formation history for calcareous sediment includes complex physical, biological and chemical processes. It is preferably selected as the major fill materials for hydraulic reclamation and artificial island construction. Calcareous sands possess inter pores and complex shape are liable to be damaged at normal working stress level due to its fragile nature. Thus, the engineering properties of calcareous soil are greatly affected by its high compressibility and crushability. A series of triaxial shear tests were performed on calcareous sands derived from South China Sea under different test conditions. The effects of confining pressure, particle size, grading, compactness, drainage condition, and water content on the total amount of particle breakage for calcareous soil were symmetrically investigated. The test results showed that the crushing extent of calcareous sand with full gradation was smaller than that a single particle group under the same test condition. Large grains are cushioned by surrounding small particles and such micro-structure reduces the probability of breakage for well-graded sands. The increasing tendency of particle crushing for calcareous sand with a rise in confining pressure and compactness is confirmed. It is also evident that a rise in water content enhances the amount of particle breakage for calcareous sand. However, varying tendency of particle breakage with grain size is still controversial and requires further examination.

• 한국토양비료학회지
• /
• 제49권6호
• /
• pp.789-794
• /
• 2016

Continuous excessive application of phosphorus (P) fertilizer and manure in plastic film house soils can lead to an accumulation of P in soils. The understanding of P sorption by soils is important for fertilizer management. In this study, 9 samples were collected for acidic and calcareous soils as non-cultivated soil and plastic film house soils as cultivated soil Phosphorus sorption data of acidic soils fit the Langmuir equations, Freundlich equations in calcareous and plastic film house soils. In calcareous and plastic film house soils, the slope of isotherm adsorption changed abruptly, which could be caused P precipitation with $CaCO_3$. The calculated Langmuir adsorption maximum ($S_{max}$) varied from 217 to 1,250, 139 to 1,429, and $714mg\;kg^{-1}$ for acidic soils, calcareous soils, and plastic film house soils with low available phosphate concentration, respectively. From this result, maximum P adsorption by the Langmuir equation could be regarded as threshold of P concentration to induce the phosphate precipitation in soil. Phosphate-sorption values estimated from one-point isotherm for acidic and calcareous soils as non-cultivated soils were comparable with the $S_{max}$ values calculated from the Langmuir isotherm.

• 한국환경농학회지
• /
• 제20권5호
• /
• pp.352-357
• /
• 2001

Cadmium (Cd) has been identified as a potential contaminant in agricultural and environmental soils. Ionic condition in the soils is an important factor to influence Cd availability. In this study, the effect of sulfate or nitrate application on Cd sorption in acidic and calcareous soils was investigated. The Cd, sulfate $(SO_4)$, and nitrate $(NO_3)$ sources were solutions of $CdCl_2$, $K_2SO_4$, and $KNO_3$, respectively. The soil-solution system pH was affected by the application of sulfate or nitrate in both acidic and calcareous soil system, but there was not clear pH difference between pre- and simultaneous applications of sulfate or nitrate (PAS/PAN or SAS/SAN). Solution ionic strength (I) values were similar between the acid and calcareous soil systems after applying the Cd even though it was significantly different in the untreated control soils. However after applying the sulfate or nitrate, the I values increased and were always higher with SAS/SAN treatments. Solution Cd concentration also increased with the application of sulfate or nitrate. However, the Cd concentration in soil solution controlled by Cd sorption in the systems was different between PAS/PAN and SAS/SAN treatments only in the calcareous soil system, but not in the acidic soil system. The difference in Cd concentration between SAS/SAN and PAS/PAN in the calcareous systems may be caused by system pH, ionic strength, complexation, and predominately, competition of the $Cd^{2-}$ with the index $K^+$ ion. Potassium ion-Cd competition in the acidic soil system may be minimized because of the abundance of hydrogen ions.

• 한국토양비료학회지
• /
• 제29권2호
• /
• pp.173-180
• /
• 1996

난용성(難溶性) 인산염(燐酸鹽) 가용화능(可溶化能)이 있는 Pseudomonas putida 와 Aspergillus niger 를 공시(供試) 균주(菌株)로 하여 산성(酸性) 토양(土壤)인 적황색토(赤黃色土)와 알칼리성(性) 토양(土壤)인 석회질토(石灰質土)에 피망을 재배하며, 선발(選拔)된 난용성(難溶性) 인산염(燐酸鹽) 가용화균(可溶化菌)의 접종효과를 조사(調査)하였다. 재배(栽培) 후(後) 토양(土壤) 유효인산(有效燐酸) 함량(含量)은 적황색(赤黃色) 토양의 무접종(無接種)에 비해 무비구(無肥區) 및 시비구(施肥區)에서는 Aspergillus niger, 볏짚구(區)에서는 Pseudomonas putida 와 Aspergillus niger 접종시(接種時) 유의(有意)하게 높았으나, 석회질토양에서는 뚜렷한 경향을 보이지 않았다. 피망의 인산(燐酸) 흡수량(吸收量)은 알칼리성(性)칸 토양(土壤)인 석회질토양(石灰質土壤)의 Pseudomonas putida 및 Aspergillus niger 접종시(接種時) 볏짚시용구를 제외한 무비구(無肥區) 및 시비구(施肥區)에서 증가(增加)하였다. Cellulase 활성(活性)은 접종에 의한 처리간 뚜렷한 차이는 없었으나 적황색(赤黃色) 토양(土壤)의 볏짚 시용구에서 가장 높았다. Phosphatase 활성은 적황색(赤黃色) 토양(土壤)에서는 Aspergillus niger 가 접종(接種)된 모든 처리에서 증가(增加)하였으며, 그 중 시비구(施肥區)와 볏짚 시비구(施肥區)에서는 유의성(有意性)이 있었고, 석회질토양(石灰質土壤)에서는 인산염(燐酸鹽) 가용화균(可溶化菌)이 접종된 모든 처리에서 증가하였으며, 특히 시비구(施肥區)에서는 Aspergillus niger, 볏짚구(區)에서는 Pseudomonas putida 접종시(接種時) 유의성(有意性)있게 증가(增加)하였다.

• 한국농업기계학회:학술대회논문집
• /
• 한국농업기계학회 2000년도 THE THIRD INTERNATIONAL CONFERENCE ON AGRICULTURAL MACHINERY ENGINEERING. V.II
• /
• pp.236-245
• /
• 2000

The feasibility of precision farming for small sized fields was studied by determining fertilizing amount of nitrogenous and calcareous to a cite specific region. A detailed soil survey at three experimental fields of 672㎡, 300㎡ and 140㎡ revealed a considerable spatial variation of the pH and organic matter(OM) levels. Soil organic matter was measured using Walkley-Black method and soil pH was measured with a pH sensor. Soil sample was obtained by Grid Node Sampling Method. The soil sampling depth was 10 - 20 cm from the soil surface. To display soil nutrient variation, a soil map was made using Geographic Information System (GIS) software. In soil mapping, soil data between nodes was interpolated using Inverse Distance Weighting (IDW) method. The variation was about 1 - 1.8 in pH value and 1.4 -7 % in OM content. Fertilizing Amount of nitrogenous and calcareous was determined by the fertilizing equation which was proposed by National Institute of Agricultural Science and Technology.(NIAST). The variation of fertilizing amount was about 3 - 11 kg/10a in nitrogenous and 70 - 140 kg/10a in calcareous. The results showed a feasibility of precision fertilizing for small size fields.

• Journal of Biosystems Engineering
• /
• 제25권3호
• /
• pp.241-250
• /
• 2000

The feasibility of precision fertilizing for small size fields was studied by determining fertilizing amount of nitrogenous and calcareous to a cite specific region. A detailed soil survey at three experimental fields of $672m^2$, $300m^2$ and $140m^2$ revealed a considerable spatial variation of the pH and organic matter(OM) levels. Soil organic matter was measured using Walkley-Black method and soil pH was measured with a pH sensor. Soil sample was obtained by Grid Node Sampling Method. The soil sampling depth was 10∼20 cm from the soil surface. To display soil nutrient variation, a soil map was made using Geographic Information System (GIS) software. In soil mapping, soil data between nodes was interpolated using Inverse Distance Weighting (IDW) method. The variation was about 1∼1.8 in pH value and 1.4∼7% in OM content. Fertilizing Amount of nitrogenous and calcareous was determined by th fertilizing equation which was proposed by National Institute of Agricultural Science and Technology(NIAST). The variation of fertilizing amount was about 3∼11 kg/10a in nitrogenous and 70∼140 kg/10a in calcareous. The results showed a feasibility of precision fertilizing for small size fields.

• 한국토양비료학회지
• /
• 제39권6호
• /
• pp.396-402
• /
• 2006

토양 유기탄소는 토양의 질 및 토양 비옥도의 평가 또는 시비량의 결정 등에 주요한 요인으로 고려되어 왔으며 온실가스의 방출 및 지구 온난화에 영향을 주고 있다. 따라서 토양 유기탄소의 적절한 관리는 토양의 질을 향상시키는 것뿐만 아니라 온실가스원을 관리하는 차원에서 중요성이 더욱 강조되고 있다. 이 연구의 목적은 압력센서를 이용한 무기탄소 측정 장치를 이용하여 토양중 무기탄소량을 측정하고 건식연소법과 습식연소법을 이용하여 석회암에서 유래된 토양의 유기탄소을 분석 비교 하고자 하였다. 건식연소법으로 측정된 총탄소의 값에서 무기탄소 측정장치를 통해 얻어진 무기탄소값을 뺀 값을 유기탄소량으로 계산하였다. 탄산석회 ($CaCO_3$)를 이용한 무기탄소 표준시료의 양과 개발된 무기탄소 측정장치 출력 값 간에 매우 유의한 직선의 관계가 얻어졌다. 충청북도 및 강원도 일대 석회암 지역에서 채취한 토양시료를 이용하여 건식연소법과 무기탄소 분석 장치를 이용하여 탄소함량을 분석한 결과 총 탄소 중량대비 약 22-28%의 무기탄소가 관측되었다. 습식연소법과 건식연소법으로 측정한 토양의 유기탄소간에 유의한 상관관계를 나타냈다. 결론적으로 개발된 토양무기탄소 분석장치는 토양 중 무기탄소의 간편한 측정을 통하여 석회암등에서 유래된 토양의 유기탄소를 효과적으로 분석하는데 기여할 수 있다.

• 한국환경농학회지
• /
• 제25권3호
• /
• pp.236-246
• /
• 2006

In this study, we give insight into questionable results that can be encountered in the conventional sequential extraction of heavy metals (Cd, Cu, and Zn) from soils. Objectives of this study were to determine the extraction variability of exchangeable (EXC)-metals as using six different EXC-extractants commonly accepted, and to investigate selectivity problems with carbonates bound (CAB)-metal fraction, a buffered acetate (1.0 M NaOAc; pH 5.0) extractable-metal fraction, leading to erratic results in especially non-calcareous soils. The contents of EXC-metals were markedly varied with the different extractability of various EXC-metal extractants used. The contents of EXC-Cd fraction were ranged from 2.0 to 74.3% of total Cd content in all of the metal spiked soils studied. The contents of EXC-Zn fraction extracted with the different EXC-extractants were varied with soil types, which were from 0.4 to 3.9% of total Zn in the calcareous soils, from 7.6 to 17.9% in the acidic soil, and from 13.6 to 56.8% in the peat soil. However, the contents of EXC-Cu fraction were relatively similar among the applications of different EXC-meal extractants, 0.2 to 2.1 % of total Cu, in all soils tested. Also, these varied amounts of EXC-metal fractions, especially Cd and Zn, seriously impacted the contents of subsequent metal fractions in the procedure. Furthermore, the CAB-Cd, -Cu, and -Zn fractions extracted by the buffered acetate solution were in critical problem. That is, the buffered acetate solution dissolved not only CAB-metals but also metals that bound or occupied to subsequent fractions, especially OXD-metal fraction, in both calcareous and non-calcareous soils. The erratic results of CAB-fraction also seriously impacted the amounts of subsequent metal fractions. Therefore, the conventional sequential extraction should be reconsidered theoretically and experimentally to quantify the target metal fractions or might be progressively discarded.

• Journal of Applied Biological Chemistry
• /
• 제42권3호
• /
• pp.134-139
• /
• 1999

The distributions of Cd, Cu, and Zn concentration in soil treated with one (1988) or two (1988 and 1993) applications of sewage sludge at rates of 0, 25, 50, and $100Mg\;ha^{-1}$ (dry weight basis) were determined to assess the accumulation and mobility of the heavy metals. The heavy metals accumulated almost entirely in 0 to 15 cm soil depths. Small amounts of the metals moved out of the tillage zone (0-15 cm depth) into the subsoil, but even at the high rate of sewage sludge, little movement of heavy metals occurred below 100 cm depth. The water-extractable Cd, Cu, and Zn concentrations were very low regardless of the rate of sewage sludge application. Availability of metals as determined by DTPA extraction showed the percentage of DTPA-extractable/total concentration increased with sewage sludge application. In the 0-15 cm depth of sewage sludge treated soil, the percentage of DTPA-extractable/total concentration was higher than 46% for Cd, but the value was less than 27% and 17% for Cu and Zn, respectively. The Cd, Cu, and Zn added to this calcareous clay soil by sewage sludge application were not very mobile, and the amount of plant available form was very small.

• 한국지반공학회:학술대회논문집
• /
• 한국지반공학회 2010년도 추계 학술발표회
• /
• pp.241-252
• /
• 2010

This study investigates the application of dilatometer test for evaluating the deformation characteristics of granular soil. $K_D$ is the most sensitive to the stress history among CPT and DMT measurements, and $E_D$ and $q_c$ are observed to be similarly affected by the stress history. The coefficient of at-rest earth pressure($K_0$) is an indirect measure evaluating the stress history of granular soil. A relation using only DMT indices provides appropriate prediction of $K_0$ values. Although penetration of dilatometer inevitably induces the failure of cementation bonds, $E_D$ reflects the deformation characteristics of undamaged cementation relatively well. Therefore, a slightly better prediction of M value for cemented sand is achieved by using $E_D$ rather than $q_c$. Because of the weaker particle strength of calcareous sand compared than quartz sand, the majority of sand particles adjacent to dilatometer probe will be crushed during penetration. The particle crushing will induce the less contraction of the dilatometer membrane during penetration, consequently, the smaller $K_D$ and $E_D$ of calcareous sand.