• 미생물학회지
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• 제26권2호
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• pp.122-128
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• 1988

The enzymatic properties of soil cellobiohydrolase were examined and compared with those of cellobiohydrolase-active extracts from soil in the forms of enzyme-humic complex and humicfree enzyme, and cellobiohydrolase partially pruified from Aspergillus niger. The pH optima of soil cellobiohydrolase and cellobiohydrolase-humic complex were greater by 1.5-3.0 pH units than those of cellobiohydrolase in humic-free extract and from A. niger. Soil cellobiohydrolase and cellobiohydrolase-humic complex were remarkably resistant to thermal denaturation and proteolysis. These results confirm that cellobiohydrolase in soil is atable in conditions which rapidly inactivate microbial cellobiohydrolase and that its stability is due to the immobilization of this enzyme by association with humic substances. The Michaelis-Menten constants (Km) for soil, cellobiohydrolase-humic complex, humic free extract and cellobiohydrolase from A. niger were 22.1mg/ml, 11.3mg/ml, 10.6mg/ml and 4.5 mg/ml of Avicel, respectively.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2002년도 추계학술발표회
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• pp.191-194
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• 2002

Humic acid, fulvic acid and humin present in volcanic ash soil were isolated by IHSS standard procedure and their characteristics were analyzed as a basic study to evaluate the effect of humic substances on the behaviour of pollutants in contaminated surface soil. The volcanic ash soil contained 42.1 % of total organic matter based on the oven-dried soil, and humin, humic and fulvic acids corresponded to 67.5 %, 15.2 %, 7.6 % of TOM respectively. Structural informations of the humic fractions were obtained from their elemental analysis and IR, CPMAS C-13 NMR spectral analysis and the differences among them are discussed with their C/H, O/C ratios and distributions of carbon types in the molecules.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1998년도 공동 심포지엄 및 추계학술발표회
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• pp.236-239
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• 1998

This research was performed to check the transport characteristics of heavy metals in contaminated soil, that is, the influence of humic acid and phosphate on transport characteristics of heavy metals was studied. From the results of column mode experiments about heavy metal behavior, the order time to reach breakthrough and equilibrium was soil ＋ humic acid( 20g ) > soil ＋ humic acid ( 5 g ) > soil without Humic acid addition > soil+humic acid( 50g ). It is because the dissolved organic carbon content increased as the soil organic matter content increased. As the phosphate increased, so did the time to reach breakthrough and equilibrium. The order of time was soil + phosphate( 50 mg ) > soil + phosphate( 20 mg ) > soil . phosphate( 10 mg ) > soil without phosphate addition. It is because the phosphate ion worked as alkalinity donor and the calcium ion co-injected worked as the accelerator of coprecipitation of heavy metals.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 총회 및 춘계학술발표회
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• pp.397-400
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• 2003

In this study, humic and fulvic acids in soils at the vicinity of domestic atomic power plants(NPPs), located in Yungkwang(YK), Uljin(UJ), Kori(KR), Koseong(KS), Wolseong(WS) area, and in volcanic ash soils of the Cheju island(Mt. Hanla(HL), Manjanggul(MJ)) were isolated, and characterized using chemical(elemental analysis, proton exchange capacity, molecular size distribution) and spectroscopic(UV/Vis., IR, FL, $^{13}$ C NMR spectra) methods. The results were compared with one another and compiled for their DB establishments. The humic substances distribution (humic acid, fulvic acid, Humin) in the soils were also determined by IHSS standard method. Main purpose of this study was to provide a basic data needed to evaluate the effect of humic substances on the migrational behaviour of radioactive elements in contaminated surface soil.

• Applied Biological Chemistry
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• 제9권
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• pp.153-159
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• 1968

강원도(江原道) 춘성군(春城郡) 동산면(東山面) 원창이리(元倉二里) 면내리(面內里)의 화전토양수점(火田土壤數點)을 공시(供試)하여 토양(土壤)의 일반적(一般的) 성질(性質)과 홍법(弘法), 대우(大羽)에 의한 Simon의 수정법(修正法)으로 부식(腐植)의 형태(形態)를 분석검토(分析檢討)하였든바 그 결과(結果)를 요약(要約)하면 다음과 같다. 1) 본화전토양(本火田土壤)은 일반화학성분(一般化學成分)이 보통(普通) 토양(土壤)과 근사(近似)하나 C.E.C.는 크며 유기물(有機物)이 특(特)히 많이 함유(含有)되어 있다. 2) 추출제(抽出劑)에 따른 추출부식(抽出腐植)은 NaOH의 Na-pyrophosphate, NaF.의 순(順)이며 토층(土層)에 따른 추출량(抽出量)은 상층(上層)일수록 많으며 PQ% 역시(亦是) 상층(上層)일수록 크다. 3) 부식화도(腐植化度)는 NaOH. Na-pyrophosphate 추출부식(抽出腐植)은 근사(近似)하나 NaF 추출부식(抽出腐植)은 낮다. 층위별(層位別)로 보면 하층(下層)일수록 높으며 토양(土壤)의 부식화도(腐植化度)의 순위(順位)는 약간 B 토양(土壤)이 높은것 같다. 4) $Mg^{++}$에 의하여 부식산(腐植酸)을 ${\alpha}$ 형(形), ${\beta}$ 형(形)으로 분할(分割)하였으며 NaOH 추출부식산(抽出腐植酸)의 ${\alpha}$ 형(形), ${\beta}$ 형(形) 부식산(腐植酸)이 부식화도(腐植化度)가 높으며 Na-pyrophosphate 추출부식산(抽出腐植酸)의 부식화도(腐植化度)는 낮다. 경작기간(耕作期間)에 따른 부식화도(腐植化度)의 변화(變化)는 별(別)로 찾아 볼 수 없다. 5) ${\alpha}$, ${\beta}$ 형(形) 부식산(腐植酸)의 흡광곡선(吸光曲線)을 보면 추출제(抽出劑)에 따른 변화(變化)는 없고 동일(同一)한 곡선(曲線)이 나타났다.

• 한국토양비료학회지
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• 제6권1호
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• pp.67-73
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• 1973

Soil humic substances are defined as a humified part of the soil organic matters and regarded to play beneficial roles for colloid chemical properties and the fertility of the soils. This paper is referred to review the present trend of the studies on the forming processes of humic substances and on the effect on plant metabolism by some organic compounds that are directly absorbed by plants. It is generally considered that the humic substances are formed organic matters in soil or plant materials through numerous organic or biochemical processes. However, the nature of the constituting "core" and of attachment of carbohydrate, nitrogen containing compounds like protein, phenolic compounds and metals to the core are unclear though various models are suggested. It is reviewed that some organic compounds, phenclic acids, derived from humic substances are effective on plant metablism in many cases, although the mechanisms are remained to be clarified.

• Near Infrared Analysis
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• 제1권1호
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• pp.31-35
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• 2000

Near-infrared reflectance spectroscopy(NIRS) was used to determine the humic acids in soil samples from the fields of different crops and land-use over Youngnam and Honam regions in Korea. An InfraAlyzer 500 scanning spectrophotometer was obtained near infrared relectance spectra of soil at 2-nm intervals from 1100 to 2500nm. Multiple linear regression(MLR) or partial least square regression (PLSR) was used to evaluate a NIRS method for the rapid and nondestructive determination of humic acid, fulvic acid and its total contents in soils. The raw spectral data(log 1/R) can be used for estimating humic acid, fulvic acid and its total contents in soil by MLR procedure between the content of a given constituent and the spectral response of several bands. In which the predicted results for fulvic acid is the best in the constituents. The new spectral data are converted from the raw spectra by PLSR method such as the first derivative of each spectrum can also be used to predict humic acid and fulvic acid of the soil samples. A low SEC, SEP and a high coefficient of correlation in the calibration and validation stages enable selection of the best manipulation. But a simple calibration and prediction method for determining humic acid and fulvic acid should be selected under similar accuracy and precision of prediction. NIRS technique may be an effective method for rapid and nondestructive determination for humic acid, fulvic acid and its total contents in soils.

• 한국환경농학회지
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• 제12권1호
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• pp.35-40
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• 1993

담수토양중 diazinon의 거동에 미치는 토양유기물의 영향을 알아보기 위하여 담수토양에 토양유기물분획인 humin, humic acid, fulvic acid 와 diazinon을 처리하여 각 부식물질의 농도별 (0.1%, 0.5% 1.0%) diazinon 1.8ppm과 5.0ppm의 흡착률을 조사한 주요결과는 다음과 같다. 1. 1.8ppm diazinon의 흡착률은 humin > FA > HA의 순으로 많았고, 최대흡착률은 1.0% humin 첨가구에서 12.4%, 1.0% HA 첨가구에서 10.44%, 1.0% FA 첨가구에서 11.86% 이었다. 2. 5ppm diazinon의 흡착률은 1.0% humin 첨가구에서 10.21%, 1.0% HA 첨가구에서 10.4%, 1.0% FA 첨가구에서 10.64%를 보였다. 즉, diazinon의 첨가량 증가는 흡착률에 영향을 미치지 못하였다. 3. 부식물질별 diazinon의 흡착경향은 humic acid와 fulvic acid에서는 4시간 이내에 최대흡착률을 보였으나, humin에서는 4시간 이후에도 계속 흡착이 이루어 졌다. 4. 부식물질의 농도가 증가함에 따라 diazinon의 흡착률도 증가하였으며, humin 처리구에서 그 경향이 가장 뚜렷하였다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제16권1호
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• pp.51-61
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• 2011

Germination tests were conducted to determine the practical concentration levels at which plants can reproduce naturally during the phytoremediation of soils contaminated with a high concentration of petroleum hydrocarbons and heavy metals. The effects of humic acids on plant growth and soil physicochemical properties were also investigated. The results show that phytoremediation can be applied in soils contaminated by multiple contaminants at the former soil contamination potential level of Korean soil quality standards considering successful natural reproduction. It was observed that germination rates of Helianthus annuus and Festuca arundinacea were high after all treatments, and transplantation was more appropriate for Phragmites communis in phytoremediation. Humic acids had a positive effect on the growth of both aboveground and belowground biomass of herbaceous plants. Growth inhibition by multiple contaminants is more severe in the case of aboveground biomass. Germination and growth tests suggest that Helianthus annuus is a suitable phytoremediation plant for soils contaminated with a high concentration of petroleum hydrocarbons and heavy metals. The addition of humic acids also caused changes in the physicochemical properties of contaminated soils. An increase in the carbon and nitrogen content due to the addition of humic acids and a correlation between cation exchange capacity(CEC) and the organic matter content were observed.

• 분석과학
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• 제15권4호
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• pp.373-380
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• 2002

본 연구는 토양에 침적된 방사능 물질의 거동에 부식산이 미치는 영향을 평가하기 위한 기초연구로서 깊이별 토양에 존재하는 휴믹산과 풀빅산을 추출하여 그 특성을 분석하였다. 휴믹산과 풀빅산의 분자량 분포는 한외여과법을 이용하여 조사하였으며, 분광학적 특성으로는 자외선-가시광선, 적외선 및 형광분광 분석을 실시하였다. 휴믹산의 주요 분자량 분포 영역은 30~100 kDa (46~56%)이었으며, 풀빅산은 10~30 kDa (33~43%) 이었다. 토양 깊이가 증가할수록 휴믹산과 풀빅산 분자의 분자량은 전체적으로 감소하는 경향을 보였다. 자외선-가시광선 분석 결과, 휴믹산이 풀빅산에 비하여 전체적으로 1.4~1.5배 더 높은 흡광계수 (280 nm)를 나타내었고, 휴믹산의 경우 토양 깊이가 증가할수록 흡광계수가 증가하였다. Synchronous 형광 분석 결과, 휴믹산과 풀빅산의 방향족 고리화합물은 428 nm 영역 (type 1)과 498 nm 영역 (type II)에서의 형광피크에 해당하는 두 가지 특성 구조를 가짐을 알 수 있었다. 휴믹산 분자는 대부분 장파장 영역 (type II)에서의 방향족 고리구조 특성을 보였으며, 휴믹산과 풀빅산 모두 토양층의 깊이가 증가할수록 장파장 영역의 방향족 고리 특성이 증가하는 경향을 보였다. 적외선 분석 결과, 풀빅산이 휴믹산에 비해 카르복실기 (${\sim}1720cm^{-1}$)의 피크세기가 높았으며, 토양 깊이가 증가할수록 휴믹산과 풀빅산분자의 카르복실기의 피크세기가 증가하는 특성을 보였다.