• 한국토양비료학회지
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• 제43권5호
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• pp.637-643
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• 2010

석회고토 및 패화석비료를 대체할 수 있는 토양개량제로 활용가치가 높은 굴껍질을 사과 '감홍' 재배 과수원에 시용하여 고두병 발생에 미치는 효과를 검토하였다. 석회고토와 굴껍질을 처리한구는 무처리구에 비해 표토와 심토의 토양 pH와 치환성 칼슘 함량이 증가된 반면, 치환성 나트륨 함량은 차이가 없었다. 사과의 고두병 발생비율은 무처리구가 10.4%로 가장 높았고 굴껍질 4 Mg$ha^{-1}$ 이상 처리할 경우 3.7% 이하로 유의적인 감소를 보였으며 석회고토 처리구는 8.9%로 무처리구와 비슷한 수준이었다. 굴껍질 시용량과 수확기 표토 및 심토의 pH와 치환성 칼슘 함량은 고두병 발병비율과 고도로 유의적인 부의상관을 보였다. 고두병 발병비율을 경감시킬 수 있는 굴껍질 시용량은 4 Mg $ha^{-1}$ 이지만 시험 후 토양의 치환성 칼슘 함량, pH 및 과실중량, 수량 등을 감안할 때 최적의 굴껍질 시용량은 2 Mg $ha^{-1}$로서 석회소요량과 같았다.

• 한국토양비료학회지
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• 제9권2호
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• pp.65-70
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• 1976

세가지 종합액비(綜合液肥)(Compresal 1호(號) 및 2호(號)와 3p)를 농가수도(農家水稻)(미네히까리) 포장(圃場)에서 출수(出穗) 10일전(日前)과 10일후(日後) 및 20일후(日後) 3회(回)에 걸쳐 살포(撒布)(1,000배액(倍液) $80{\ell}$/10a)하여 다음과 같은 결과를 얻었다. 1. 모든 액비(液肥)에서 등숙율(登熟率)이 높았으며(10% 수준(水準)에서 유의(有意)) 수확지수(收穫指數)도 높아(5%수준(水準)) 균일포장(均一圃場)에서는 수량(收量)에도 유의성(有意性)있는 효과(効果)가 기대되었다. 2. 수확기(收穫期)에 있는 지엽분석결과(止葉分析結果)로 고찰(考察)한 바로는 철과다(鐵過多), 인산결핍지(燐酸缺乏地)로 액비(液肥)의 시용(施用)은 인산(燐酸)을 보충(補充)하고 철(鐵)의 이동(移動)을 막은것으로 보였다. 지엽중(止葉中)의 Mn농도(濃度)는 처리(處理)를 하므로써 증가(增加)되였으며(5% 수준(水準) 유의성(有意性)) 액비중(液肥中) Mn은 인산(燐酸)에 의(依)하여 상위부(上位部) 이동(移動)이 촉진(促進)되어 Fe/Mn 균형유지(均衡維持)에 기여한 것 같다. 4. 지엽중(止葉中)의 질소(窒素)는 불충분(不充分)하였으나 액비(液肥)의 효과(効果)가 등숙율(登熟率)에 관여된 것으로 보였다. 5. Ca농도(濃度)는 처리지엽(處理止葉)에서 증가(增加)하였으나 Mg B. Zn은 감소(減少)하였다.

• Asian-Australasian Journal of Animal Sciences
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• 제15권3호
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• pp.357-365
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• 2002

A survey was under taken of six district of Northern India viz. Bareilly, Pilibhit, Udham Singh Nagar, Nainital, Almora and Rampur. The age, breed, sex and physiological status recorded. A total number of 854 cattle examined out of which lactating (274 cases), non lactating (302 cases) heifers (128 cases), calves (82 cases) and adult male (68 cases) were examined. An incidence of 4.92 percent (42) of microfilarisis was recorded. The highest prevalence was observed in Rudrapur District of Udham Singh Nagar (33.33%, 4/12), followed by Lalkaun in Nanital District (21.74%, 10/46), Rampur (12.50%, 2/16), Bareilly (8.16%, 8/98) and Pilibhit (1.22%, 1/82). No infection was observed in Almora region. Amongst 854 cattle of different group incidence was highest in adult male (12.20%, 10/82), followed by non lactating (3.82%, 12/314) and lactating (2.70%, 2/74), (7.64%, 12/157) was found in Heifers. For haemeto-biochemical, serum minerals estimations and therapeutic study 32 animals suffering from filariasis and 18 healthy animals were taken. 16 animals were treated with ivermectin $@200{\mu}g/kg $ body weight. Effect of this disease on production has also been estimated for which body weight and milk production was observed. The main clinical manifestations observed were anaemia, loss of appetite, debility, oedematous swelling especially in the abdominal region, increased heart rate, and respiration rate. Haematological changes indicated decrease in hemoglobin, total erythrocyte count, packed cell volume, erthrocyte fragility and neutrophil, whereas there was significant increase in erythrocytes sedimentation rate (ESR), total leukocyte count (TLC), lymphocyte and eosinophils. Biochemical changes showed significant reduction in the values of serum albumin, A : G ratio, where as there was significant increase in blood glucose, blood urea nitrogen (BUN), globulin, total lipid, total cholesterol, phospholipids, serum bilirubin. Serum mineral profile also altered markedly, which indicate a significant decrease in Ca, Cu, Fe, Zn, and Mn with increase value of Na and Cl. There was no significant change in P and K values. Enzyme pattern in micro filaria infected animal indicated increased level of AST, ALT, alkaline phosphatase, ornithine carbamyl transferase, sorbitol dehydrogenase, glutamate dehydrogenase, isocitric dehydrogenase and lactate dehydrogenase. In blood gas values and acid/base balance, there was an increase in $PVCo_2$ and $PVo_2$. It has been observed that microfilaria infected cattle showed decrease in body weight and milk production. Animal treated with ivermectin showed the return of these above values toward normalcy.

• 한국대기환경학회지
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• 제27권5호
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• pp.603-613
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• 2011

The collection of $PM_{10}$ and $PM_{2.5}$ samples was made at Gosan site of Jeju Island. Their ionic compositions of both inorganic and organic phases were then analyzed to examine their acidification and neutralization characteristics in atmospheric aerosols. The mass concentrations of $PM_{10}$ and $PM_{2.5}$ at Gosan site were $37.6{\pm}20.1$ and $22.9{\pm}14.3{\mu}g/m^3$, respectively, showing the content ratio of $PM_{2.5}$ to $PM_{10}$ as 61.0%. In the evaluation of ionic balance, the correlation coefficients (r) between the sums of cationic and anionic equivalent concentrations were excellent with 0.982 ($PM_{10}$) and 0.991 ($PM_{2.5}$). The concentration ratios of $PM_{2.5}/PM_{10}$ derived for nss-$SO_4^{2-}$, $NO_3^-$, and $NH_4^+$ were 0.94, 0.56, and 1.02, respectively, indicating the relative dominance of fine fractions. The acidifying capacity of inorganic anions ($SO_4^{2-}$ and $NO_3^-$) in $PM_{10}$ and $PM_{2.5}$ were 96.5% and 97.3%, while those of organic anions ($HCOO^-$ and $CH_3COO^-$) in each fraction were 2.9% and 2.0%, respectively. On the other hand, the neutralizing capacity of $PM_{10}$ and $PM_{2.5}$ by $NH_3$ were 72.8% and 82.3%, while their $CaCO_3$ counter parts were 22.5% and 13.3%, respectively.

• 한국환경농학회지
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• 제28권1호
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• pp.32-37
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• 2009

본 연구는 산촌형 조건불리 지역의 농업 소수계에서 영농활동이 주변 수질환경에 미치는 영향을 평가하고자 하였다. 고성천 유역에서 토지이용형태별 토양의 화학적 특성을 비교한 결과, 논토양과 밭토양의 pH와 유기물의 함량은 비슷하였으나, 밭토양은 논토양에 비해 유효인산과 치환성 칼리와 칼슘의 함량이 월등히 높았다. 또한, 고성천의 수질 모니터링 결과, 하부로 내려갈수록 영양물질의 농도는 높았으며, 특히 전 조사지점에서 평상시에 비해 강우시에 $COD_{Mn}$과 T-P의 농도가 높았다. 유역내 논과 밭이 혼재되어 있는 지류에서 토지이용형태별 SS 및 T-N과 T-P의 농도 부하 특성을 평가한 결과, 논은 다른 토지이용형태에 비해 영양물질을 흡수하는 특성을 가지고 있어 영양물질의 지표배출 감소 효과 및 유입된 영양물질의 저류 능력을 지니고 있어 수질정화 효과가 있었다. 산촌형 조건불리 지역인 고성천 유역에서 영농기간 동안 질소와 인의 유입량-유출량은 -98.9와 -29.7 kg $ha^{-1}$로 유출되는 양이 많았는데, 이는 고성천 유역이 전형적인 농업지역으로 영농활동으로 인한 투입량이 적은 반면에 수확물로의 배출량이 많았기 때문으로 생각된다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.121-121
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• 2004

The groundwater in the Pocheon area occurs from both a fractured bedrock aquifer in igneous and metamorphic rocks and an alluvial aquifer with a thickness of <50 m, and forms a major source of domestic and agricultural water supply. In this study, we performed a hydrogeochemical study in order to identify the control of geochemical processes on groundwater quality. For this study, groundwater level and physicochemical parameters (EC, Eh, pH, alkalinity) were monitored once a month from a total of 150 groundwater wells between June 2003 to August 2004. A total of 153 water samples (13 surface water, 66 alluvial groundwater, 74 bedrock groundwater) were also collected and analyzed in February 2004. Groundwater chemistry in the study area is very complex, depending on a number of major factors such as geology, degree of chemical weathering, and quality of recharge water. Hydrochemical reactions such as the leaching of surficial and near-solace soil salts, dissolution of calcite, cation exchange, and weathering of silicate minerals are proposed to explain the chemistry of natural groundwater. Alluvial groundwaters locally have very high TDS concentrations, which are characterized by their chloride(nitrate)-sulfate-bicabonate facies and low Na/Cl ratio. Their grondwater levels are highly fluctuated according to rainfall event. We suggest that high nitrate content and salinity in such alluvial groundwaters originates from the local recharge of sewage effluents and/or fertilizers. Likewise, high concentrations of nitrate were also locally observed in some bedrock groundwaters, suggesting their effect of anthropogenic contamination. This is possibly due to the bypass flow taking place through macropores. Tile degree of the weathering of silicate minerals seems to be a major control of the distribution of major cations (sodium, calcium, magnesium, potassium) in bedrock groundwaters, which show a general increase with increasing depth of wells. Thermodynamic interpretation of groundwater chemistry shows that the groundwater in the study area is in chemical equilibrium with kaolinite and Na-montmorillonite, which indicates that weathering of plagioclase to those minerals is a major control of hydrochemistry of bedrock groundwater. The interpretation of the molar ratios among major ions, as well as the mass balance calculation, also indicates the role of both dissolution/precipitation of calcite and Ca-Na cationic exchange as bedrock groundwaters evolves progressively.

• Asian-Australasian Journal of Animal Sciences
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• 제17권5호
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• pp.621-628
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• 2004

Twenty male buffalo calves of 6-9 months of age (average body weight, 97 kg) were randomly allocated into two main groups of four (control) and sixteen (supplemented) calves. The supplemented group was further divided in to four equal sub-groups, with the two groups supplemented with a liquid preparation of urea-molasses, UML1, containing fish meal and UML2, containing formaldehyde treated deoiled mustard cake (FDMC) and the other two, with a semi-solid preparation, UMC1 with FDMC and deoiled rice bran (DORB) contributing similar level of CP as in UML2 and UMC2 with double the level of FDMC to that in UMC1. The control group was fed with DORB along with ad libitum wheat straw at 40:60 ratios. The rest of the groups were fed on the above diet supplemented with 500 g (as fed basis) of urea-molasses preparations. The experimental feeding was carried out for 24 weeks including a metabolism trial towards the end of experimental feeding. Daily feed intake and fortnightly change in live weight were also recorded during the study. Catalytic supplementation of 500 g urea-molasses induced 8-25% higher voluntary feed intake of wheat straw, resulting in 15-25% higher DM and OM intake. The digestibility of DM, OM, total carbohydrate, NDF, ADF, hemicellulose and cellulose in all the dietary groups were comparable. The CP digestibility of calves in supplemented groups were higher (p<0.05) than the control group. The balance of nutrients, viz. N, Ca and P, was also higher in the supplemented groups. Significantly higher intake of digestible CP coupled with other digestible nutrients attributed to higher TDN (1.67-1.78 vs. 1.37 kg) and ME (5.94-6.31 vs. 4.87 Mcal) intake in urea-molasses supplemented groups which resulted in higher live weight gain compared to that in control group (p<0.01). Between the supplements, UML2 and UMC2 faired non-significantly, indicating formalin treated mustard cake as a suitable replacement to fishmeal in the supplement. The overall ranking based on intake and digestibility of nutrients, live weight gain, economic evaluation and input-output relationship revealed that the rations with UML2 and UMC1 to be of greater value compared to other types. From the study it can be concluded that young ruminants can be reared successfully on a basal diet of deoiled rice bran and wheat straw supplemented with cheaper urea-molasses-mineral mix.

• 한국대기환경학회지
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• 제17권6호
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• pp.475-485
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• 2001

The presence of airborne particles in the earth atmosphere expert important controls on the global climate because of their effects on the radiative balance. However, there are major uncertainties associated with the direct and indirect radiative effects of aerosols. In addition, their physicochemical properties cannot only the decline of air quality but also damage human health. Airborne particles were collected by two different commercial air samples, high volume sampler(for TSP) and low volume sampler(for P $M_{10}$ ) at the campus of Kunsan National University during February to September, 2000. In most cases, TSP and P $M_{10}$ were sampled once a week for the duration of 24 hours from 9:00 a.m. In addition samples were collected more intenisve, when the yellow dust was expected. Each sample was analyzed for pH and major ions concentration (C $l^{[-10]}$ , S $O_4$$^{2-}$, N $O_3$$^{[-10]}$ , N $a^{+}$, N $H_4$$^{+}$, $K^{+}$, $Mg^{2+}$, $Ca^{2+}$) by ion chromatography and atomic absorption spectrophotometry. Acidity (pH) of TSP and P $M_{10}$ ranged from 5.09 to 8.51 and from 6.22 to 7.54, respectively. The concentrations of airborne particles were found to satisfy both the short and long-term air quality standards during the sampling period. If the ratio of ionic concentrations originating from None sea salt(Nss) to sea salt(ss) in aerosol samples was concerned, it was found that the ionic concentrations from marine environment contributed dominantly in total mass concentration in the airborne particles. When seasonal trends were examined, the TSP concentrations in spring were higher than those of other seasons. It may result form frequent occurrences of yellow dust and during the spring season. The concentration ratio of P $M_{10}$ to TSP ranged from 0.78 to 1 during the sampling period. pH in the airborne particle was highest during spring, but the other seasons maintained almost same level. These results suggest that alkaline species in yellow dust can directly neutralize aerosol acidity. During spring season, yellow dust could be a positive factor that can defer the acidification of surface soil and water by neutralizing acidic aerosols in the atmosphere.osphere.

• 한국습지학회지
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• 제17권4호
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• pp.325-331
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• 2015

불투수면의 증가와 도시화 현상은 지하수량의 감소, 지표수의 고갈, 홍수의 증가 등과 같은 자연적인 물순환 시스템에 변화를 가져왔다. 또한, 인간이 사용할 수 있는 수량의 감소 또한 초래하게 되었다. 이에 빗물의 적절한 처리와 재활용은 최근 발생되는 수문학적 문제의 해결에 도움이 될 수 있을 것으로 예상되어왔다. 따라서 본 연구는 지붕빗물유출수를 침투 및 저류 기작으로 처리하여 자연적인 물순환의 회복을 이루고자 침투화분 기술을 개발하였다. 연구결과, 침투화분 기술은 평균 79% 정도의 강우유출유량 저감효과가 있는 것으로 분석되었다. 또한 유출유량 지연효과 및 첨두유량 지연효과도 발생하였는데, 약 3시간의 유출지연효과와 38%의 유량 저감효과가 발생하는 것으로 나타났다. 한편, 침투화분의 오염물질 처리효율은 TSS 97%, BOD 및 CODcr 94%, TN 86%, TP 96%, Total Cu, Total Zn, Total Pb의 중금속은 약 93% 처리되었으며, 처리수의 오염물질 농도는 TSS 13.3mg/L, BOD 3.6mg/L, TN 4.7mg/L 및 TP 0.1mg/L로 분석되어 도시재이용수, 조경용수, 공업용수로서 사용이 가능할 것으로 분석되었다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제28권1호
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• pp.1-14
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• 2023

In this study, column tests using relatively uniform Jumunjin sand media were conducted to evaluate the feasibility of calcium polysulfide (CaS_x, CPS) in removing high concentration of Zn²⁺ in groundwater. The injected CPS solution reacted rapidly with Zn²⁺ in artificial groundwater and effectively reduced Zn²⁺ by more than 99% through metal sulfide precipitation. Since the density (d = 1.27 g/cm³ ) of CPS solution was greater than that of water, CPS solution settled down rapidly while capturing Zn²⁺ and formed stable CPS layer similar to dense nonaqueous phase liquid. Mass balance analysis on Zn²⁺ in CPS solution suggested that CPS solution effectively reacted with Zn²⁺ to form metal sulfide precipitates except for high groundwater seepage velocity of 400 cm/d. With greater groundwater seepage velocity, injected CPS did not completely dissolve at the CPS-water interface, but a partially-misible CPS layer continuously moved and reacted with Zn²⁺+ in the direction of groundwater flow. Since hydraulic conductivity (K_h) decreased slightly due to the generated metal precipitates in the inter-pores of media, injection of CPS solution should be optimized to prevent clogging. As evidenced by both XRF and SEM/EDS results, ZnS precipitates were clearly observed through the reaction between the CPS solution and Zn²⁺. Further study is warranted to evaluate the feasibility of CPS to remove high-concentration heavy metalcontaminated groundwater in complex and heterogeneous media.