• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
• /
• 1998.11a
• /
• pp.64-68
• /
• 1998

본 연구는 오염토양/지하수의 정화를 위하여 사용되는 계면활성제 교정기술의 보다 현실적인 평가를 위하여 토양에 흡착된 계면활성제에 대한 소수성 유기오염물인 Naphthalene과 Phenanthrene의 흡수현상에 대한 연구결과를 나타내었다. 음이온 계면활성제인 Sodium Dodecyl Sulfate (SDS)와 중성 계면활성제인 Tween 80의 흡착곡선은 소수성 꼬리 (hydrophobic tails)간의 상호작용에 의하여 S-형 모양을 보이며 이들 흡착된 계면활성제는 Micelle로 존재하는 계면활성제에 비하여 유기오염물에 대한 보다 강한 흡수능력을 나타내었다. 결과에 나타난 흡수능력의 차이는 계면활성제가 흡착되어있거나 Micelle상태로 존재할 경우 다른 구조를 형성하기 때문이라 사료된다. 흡수된 계면활성제와 Micelle의 상호경쟁에 의하여 유기오염물의 부동성(immobility)을 나타내는 분배계수(distribution coefficient)는 계면활성제의 농도에 반비례하였다. 결론적으로 토양/지하수의 오염물 정화를 위하여 계면활성제 교정기술의 적용 시 고정상 (solid phase)에 있는 흡착 계면활성제에 의한 유기오염물의 지체현상 (retardation)을 고려하여야 한다.

• Korean Journal of Soil Science and Fertilizer
• /
• v.29 no.3
• /
• pp.218-225
• /
• 1996

Using water vapor adsorption data foe some typical Korean soils. we calculated the adsorption energy distribution functions and average adsorption energies for these soils using theory of adsorption on hetergeneous surfaces. As a local adsorption models the BET and a new Aranovich equations were applied. The distribution functions were broad, indicating rather high energetic inhomogeneity of the surface.

• Korean Journal of Environmental Agriculture
• /
• v.11 no.2
• /
• pp.101-108
• /
• 1992

In order to illustrate adsorption phenomena of herbicides(alachlor and paraquat) on soils, absorption equation of herbicides and the relationships between soil properties and adsorption constants were investigated with 22 soils. The results were as follows : 1. The shaking time for approaching equillibrium reaction of herbicides(alachlor and paraquat) with woils were about 30 minutes for paraquat and 4 hours for alachlor, respectively. 2. The distribution coefficients of alachlor were inbetween 0.81-33.83 in 5 ppm and 0.09-15.52 in 50 ppm, respectively. 3. The adsorption of alachlor was positively correlated with organic matter and paraquat was with clay content of soils. 4. Both paraquat and alachlor were highly adsorbed in Chunpo series soil containing low contents of organic matter and clay on account of different mechanism from other soils, 5. Freundlich's adsorption constant(K) was greater than distribution coefficient(Kd), and the differences between K and Kd's were to be increased with increasing equillibrium concentrations.

• Korean Journal of Soil Science and Fertilizer
• /
• v.24 no.2
• /
• pp.124-129
• /
• 1991

A mass balance method which measures directly both the sorbed pesticide and equilibrium solution concentration was compared with the batch method in a hypothetical experiment to determine the precision of sorption measurement. The mass balance method was shown to improve precision of sorption measurement. The two methods were also tested experimentally on the Wahiawa soil, 0-20, 40-60 and 100-120 cm, and Salinas soil, 0-15 and 115-130 cm. The mass balance method greatly improved precision of sorption measurement on the deep Wahiawa subsoil having the lowest sorption. The coefficient of variation (CV) for $K_d$ measurement was 20.3% for the batch method and 8.4% for the mass balance method. For other soil samples tested, precision of the batch method was relatively high but was still improved by the mass balance method.

• Proceedings of the Korean Society of Soil and Groundwater Environment Conference
• /
• 2001.09a
• /
• pp.244-248
• /
• 2001

사질 토양에서의 유기물 함량이 벤젠의 흡착과 생분해에 미치는 영향을 분석하기 위하여 다양한 분말 활성탄(PAC)함량 조건에서 비평형 배치 실험을 실시하였다. 비평형 배치실험에서 벤젠의 흡착과 생분해를 비교하기 위하여 BTEX 화합물에 대한 분해능이 우수한 Pseudomonas aeruginosam의 유무에 따른 두 가지의 실험 조건을 설정하였다. 실험 결과 반응 시간 1일까지 빠른 흡착양상을 보였으며, 2일부터 20일 까지는 매우 느린 흡착 양상을 보였다. 활성탄의 함량이 증가할수록 벤젠의 흡착은 증가하는 것으로 나타났으며, Pseudomonas aeruginosa가 첨가된 실험에서는 PAC 함량이 증가할수록 흡착은 증가하였으 나 bioavailability factor (B$_{f}$ ) 값이 감소하였다. 이는 bioavailability가 흡착에 의해 제한됨을 지시한다.

• Journal of Soil and Groundwater Environment
• /
• v.13 no.1
• /
• pp.52-59
• /
• 2008

Adsorption is a major process causing the accumulation of arsenic onto soil. Therefore, further understanding of the adsorption/desorption characteristics of arsenic species on soil is essential for predicting their fate and preparing appropriate remediation strategy to remove arsenic from soil. In this study, the column adsorption/desorption experiment has been performed with As(III) and As(V) on soil. Experiment with As(III) was conducted under reducing condition, whereas that with As(V) was under oxidizing condition. Most of As(III) was remained on the oxidation state during the experiment. The results showed that the adsorption/desorption rate of As(III) was higher than that of As(V). Adsorption and desorption of arsenic species were not completely reversible in the column experiment. It was also found that As(V) in the column experiment was adsorbed more rapidly on soil than in the batch experiment.

• The Korean Journal of Pesticide Science
• /
• v.2 no.1
• /
• pp.70-78
• /
• 1998

This study was conducted to investigate the adsorption-desorption characteristics of herbicide paraquat on clay minerals, humic materials, and soils under the laboratory conditions. Adsorption time of paraquat on clay minerals was faster than organic materials and soils. Adsorption amount on montmorillonite, 2:1 expanding-lattice clay mineral, was largest among the adsorbents tested. The adsorption capacity of paraquat was approximately 21 % of cation exchange capacity in soils, 45.1 % in kaolinite, and 80.6% in montmorillonite. Humic materials, humic acid and fulvic acid isolated from soil II, adsorbed larger amount of paraquat than kaolinite and soils. Distribution of tightly bound type of paraquat was larger in clay mineral and soils but loosely bound type was larger in humic acid and fulvic acid. In oxidized soil, the adsorption amount of paraquat was decreased to 85.1-95.5% of original soils. Distribution of unbound and loosely bound type of paraquat was decreased in oxidized soil but tightly bound type was increased. The competition cations decreased paraquat adsorption on humic materials and soils but not affected on montmorillonite. No difference was observed as the kinds of cations. In cation-saturated adsorbents, the adsorption amount was decreased largely in humic materials and soils but decreased a little in montmorillonite. The tightly bound type of paraquat in all adsorbents was not desorbed by pH variation, sonication, and cation application but loosely bound type was desorbed. However, the desorption amount was different as a kinds of adsorbents and desorption methods.

• Korean Journal of Soil Science and Fertilizer
• /
• v.38 no.5
• /
• pp.238-246
• /
• 2005

We conducted this investigation to observe competitive adsorption phenomena among the heavy metals onto the available sorption sites of soil particle surfaces in sandy clay loam and clay soil collected from Nonsan city, Chungnam and Yoosung, Daejeon in Korea, respectively. Polluted and contaminated soils can often contain more than one heavy metal species, resulting in competition for available sorption sites among heavy metals in soils due to complex competitive ion exchange and specific sorption mechanism. And the adsorption characteristics of the heavy metals were reported that the selectivity for the sorption sites was closely related with electropotential and electro negativity carried by the heavy metals. The heavy metals were treated as single, binary and ternary systems as bulk solution phase. Adsorption in multi-element system was different from single-element system as Cr, Pb and Cd. The adsorption isotherms showed the adsorption was increased with increasing equilibrium concentrations. For binary and ternary systems, the amount of adsorption at the same equilibrium concentration was influenced by the concentration of individual ionic species and valence carried by the respective heavy metal. Also we found that the adsorption isotherms of Cd and Pb selected in this experiment were closely related with electronegativity and ionic potential regardless number of heavy metals in solution, while the adsorption of Cr carried higher valance and lower electro negativity than Cd and Pb was higher than those of Cd and Pb, indicating that adsorption of Cr was influenced by ionic potential than by electronegativity. Therefore adsorption in multi-element system could be influenced by electronegativity and ionic potential and valance for the same valance metals and different valance, respectively. But it still needs further investigation with respect to ionic strength and activity in multi-element system to verify sorption characteristics and reaction processes of Cr, especially for ternary system in soils.

• Korean Journal of Soil Science and Fertilizer
• /
• v.7 no.4
• /
• pp.197-200
• /
• 1974

PCP adsorption experiment was carried out with six soils various in clay mineral and organic matter content and soil pH. The results were as follows; 1. The major factor governing the PCP adsorption is pH 2. The adsorption was increased with organic matter content at a certain pH 3. The adsorption was less related to crystalline clay mineral species.

• Korean Journal of Soil Science and Fertilizer
• /
• v.24 no.2
• /
• pp.116-123
• /
• 1991

Two solution to soil ratios, 2 : 1 and 5 : 1 were tested to determine the appropriate ratio in the sorption measurement off. sulfoxide for Wahiawa soil samples, 0-20 cm, 40-60 cm and 100-120 cm. and Salinas soil samples, 0-15cm and 115-130cm. One ${\mu}$ mol/L f.sulfoxide was used as an initial equilibration concentration. Sorption of f.sulfoxide at 5 : 1 ratio showed appropriate mixing, while sorption at 2 : 1 ratio indicated insufficient mixing during the various batch equilibration times (4, 12, 24 and 48 hours). For most samples the degree of sorption was about 20-50%, which falls in the desired range (20-80%) at the 5 : 1 ratio. An exception was with the low-sorptive Wahiawa subsoil in which the ranges were below 20%. Thus the 5 : 1 ratio can be used for f.sulfoxide sorption measurement. Four equilibration times (4, 12, 24 and 48 hours) and four concentrations(0.1, 1.0, 5.0 and $10{\mu}mol/L$) were used to determine the appropriate equilibration time for Wahiawa and Salinas soils. Sorption increased over all equilibration times, indicating no complete equilibrium within 48 hours. Apparent equilibrium was reached in 4 hours, and sorption increased slowly until 24 hours and faster thereafter, except for the Wahiawa soil, 100-120 cm. The recommended equilibration time is 24 hours, since it may eliminate the insufficient sorption and yet avoid undesirable transformation.