• 한국축산식품학회지
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• 제38권2호
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• pp.273-281
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• 2018

Preheating conditions (low-, medium-, and high heat-) did not significantly affect the buffering capacity (BC) of skim milk powder (SMP), whereas the level of demineralization significantly affected the BC of whey powders (WP). Heat treatment ($85^{\circ}C$ for 30 min) of both SMP and WP (90% demineralized) mixtures (88:12, 76:24, 64:36 and 52:48; SMP:WP) resulted in a reduced BC, and the extent of this reduction increased with the proportion of WP increased in the samples. High-buffering milk prepared by the addition of phosphate salts (40 mM $NaH_2PO_4$ and 60 mM $Na_2HPO_4$) delayed the rate of pH decline during yoghurt fermentation. The high-buffering yoghurt showed a significantly higher water holding capacity (WHC) than that of control yoghurt (p<0.05), as well as a more uniform and interconnected microstructure with small pore sizes than those of control yoghurt. No significant differences were found between high-buffering and control yoghurt regarding the viable bacterial counts of starter. The manipulation BC can potentially improve the quality characteristics of yoghurts, such as WHC and texture.

• Journal of the Korean Wood Science and Technology
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• 제35권5호
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• pp.38-45
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• 2007

Flakeboards made from ring- and drum-cut flakes of Douglas-fir, hemlock, red lauan and kapur using two kinds of resin levels were evaluated for the selected properties according to flake thickness. The pH and buffering capacity of four species were determined. Those of kapur were extremely different from the other three species. These pH and buffering capacity values result in the poor internal bond strength of kapur flakeboard. The internal bond strength was affected significantly by flake thickness, resin content and species. MOR and MOE in bending strength were maximized at medium drum-cut flake thickness. Screw holding strength was not consistent for flake thickness, but it was influenced by species. Thickness swelling and water absorption of Douglas-fir and hemlock flakeboard were minimized at medium drum-cut flake thickness.

• 대한화학회지
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• 제43권2호
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• pp.172-181
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• 1999

수용성 규산나트륨 빌더를 개발하기 위하여 물유리와 수산화나륨을 적정비율로 혼합한 후 메탄올에 분산시켜 $SiO_2/Na_2O$의 몰 비율이 2.4∼2.8인 무정형 규산나트륨 고체분말을 제조하였다. 이때 규산나트륨의 $SiO_2/Na_2O$의 몰비, 용해도, thermogram, SEM, BET 등을 통하여 그 물리적 특성을 조사하였으며 빌더로서의 기본적인 특성을 규명하기 위해 $SiO_2/Na_2O$의 몰비가 1.0, 2.4, 2.8인 규산나트륨 빌더와 제올라이트를 사용하여 pH 유지능력, 온도에 따른 칼슘이온 결합능, 계면활성제 흡착능 등을 조사하였다. 그 결과 수용성 규산나트륨 화합물이 세제용빌더로서 가져야할 특성인 pH 유지능력 및 용해도에 있어서 제올라이트 보다 우수한 성능을 나타냈으나 칼슘이온 결합능 및 계면활성제 흡착능은 낮게 나타났으며, 규산나트륨의 $SiO_2/Na_2O$의 비율이 증가할수록 pH 유지능력과 이온교환능력은 감소하지만 계면활성제 흡착능력은 다소 증가함을 알 수 있었다.

• 한국토양환경학회지
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• 제2권1호
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• pp.35-44
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• 1997

토양층과 모암층에서의 산성우에 대한 중화능력을 평가하기 위하여 인공강우를 이용한 컬럼실험을 실시하였으며 토양을 이루고 있는 모암 특성의 차이에 의한 산성강하물의 완충효과를 비교하기 위하여 연구지역내의 모암의 조성광물에 차이가 있는 두 개의 골짜기를 선정하고 골짜기에 흐르는 지표수의 pH를 1996년 5월부터 1996년 10월까지 측정하였다. 컬럼실험에서 사용한 인공강우는 증류수에 황산과 질산을 적절히 첨가하여 pH를 각각 3, 4, 및 5로 조절하였으며 컬럼유출수의 주요 양이온과 음이온을 측정하였다. A층위와 B층위의 양이온 교환용량(CEC)은 각각 9.68 meq/100g과 6.16 meq/100g 이었으며 인공강우의 살포시 컬럼유출수의 pH는 중간층토양에서보다 양이온 교환용량이 큰 표층토양에서 더 크게 나타났다. 컬럼유출수에서의 $Ca^{2+}$, $Mg^{2+}$, $Na^{+}$의 합이 점차로 감소하여 지속적인 산성우는 토양의 양이온 교환용량을 감소시키는 것으로 나타났다. 현장조사결과에 따르면 골짜기의 하류로 내려옴에 따라 지표수의 pH는 계속 증가하여 하류로 흐르는 과정에서의 완충효과를 나타내었다. 이러한 완충효과는 모암의 조성광물중 kaolinite와 illite 이외에도 smectite를 함유하고 있는 골짜기에서 더 크게 나타나는 것이 특징적이었다. 이 결과는 토양충 뿐만 아니라 모암이 산성우의 완충용량을 가지고 있음을 나타내었다.

• 한국환경농학회지
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• 제25권2호
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• pp.157-163
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• 2006

Investigation of Cd and Zn availability in four different soils as affected by the interactions of these two heavy metals was conducted using the metal desorption quantity-intensity (Q/I) isotherms. The soils were artificially contaminated with proper concentrations of Cd and Zn as $CdSO_4\;and\;ZnSO_4$ solutions. DTPA (diethylene triamine pentaacetic acid) - extractable and water-extiactable Cd or Zn from the soils were used as $Q_{Cd}\;or\;Q_{Zn}\;and\;I_{Cd}\;or\;I_{Zn}$ factors, respectively. The coefficient of determination for Cd and Zn desorption Q/I linear regression in the soils ranged from 0.947 to 0.999, which indicated that Q and I factors were closely correlated. The buffering capacity of Cd, $BC_{Cd}$, in the soils decreased with increasing Zn treatments, and the $BC_{Cd}$ values were ranged between 205.8 and 2255.6. The decreases of $BC_{Cd}$ values were mainly dependent upon the increases of $I_{Cd}$ factors. However, Zn buffering capacity. $BC_{Zn}$ decreased with increasing Cd treatments in acidic soils, and increased in neutral and calcareous alkaline soils. The $BC_{Cd}$ values were ranged from 143.2 to 6158.0. The values of $BC_{Zn}$ as influenced by the treatments of Cd were also controlled by the solubility of water-extractable Zn, $I_{Zn}$ factor. The solubility of water-extractable Cd and Zn was significantly dependent upon the changes of soil pH that were impacted by the treatment of Zn and Cd, respectively. Also, the availability of Cd was higher than Zn availability in the acidic and neutral soils, but Zn was higher than Cd in the calcareous alkaline soil.

• 한국의류학회지
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• 제20권1호
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• pp.228-238
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• 1996

The purpose of this study was to evaluate the effect of chacteristics of knit fabrics on the microclimate of the skin simulating system. To determine the effect of characteristics of knit fabrics, vapor state of sweat pulse was simulated in the closed system. Different contents of fibers such as cotton, wool and polyester with different yarn size and knit types were chosen for specimens. The changes of humidity and temperature of air layer in the simulated systems were measured. Buffering indices, $K_d$ and $\beta_r$, were determined by considering $\alpha_p, \DeltaP_{max}, t_{max}, and tan\beta$. Physical properties of knit fabrics such as thickness, porosity, air resistance and moisture vapor transport were measured. Results showed that vapor pressure of wool was lower than cotton or polyester This was attributed to the hydrophilicity of wool which absorbed moisture rather quickly and retained in the knit fabric. The time to decrease vapor pressure was faster for polyester than cotton or wool. As a result, $K_d$ was in the order of wool> polye, item> cotton. $\beta_r$ of wool was rower than cotton or polyester due to its lowers porosity and slower desorption rate. For the yarn size, $K_d$ was in the order of 80's> 60's> 30's; thinner and lighter yarn showed better water vapor transport property. For knit type, buffering capacity of single jersey was better than interlock knit fabric. Statistical analysis showed that the air permeability was the most influential factor far the water vapor transport properties.

• 대한토목학회논문집
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• 제29권1A호
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• pp.75-84
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• 2009

본 연구에서는 혼합 콘크리트의 염소이온 고정화 능력, 수화물의 부식 억제 능력(Buffering capacity) 및 모르타르 내 철근 부식 측정을 통하여 콘크리트 내 철근 부식의 임계 염소이온 농도를 도출하였다. 실험 시 결합재로서 보통 포틀랜드 시멘트(OPC), 30% 플라이애시(PFA), 60% 고로슬래그 미분말(GGBS), 10% 실리카퓸(SF)를 치환한 혼합 시멘트를 사용하였다. 염소이온 고정화는 수분추출방법을 이용하여 측정하였으며, 시멘트의 부식 억제 능력은 결합재에 따른 산에 대한 저항성 측정을 통해 평가하였다. 염소이온이 함유된 모르타르 내 철근 부식은 재령 28일에 선형 분극 방법을 이용하여 측정하였다. 실험 결과, 염소이온 고정화 능력은 결합재 내의 $C_{3}A$ 함유량과 물리적 흡착에 의해 크게 영향을 받음을 알 수 있었다. 염소이온 고정화 정도는60% GGBS > 30% PFA > OPC > 10% SF 의 순으로 나타났다. pH 감소에 따른 시멘트의 부식 억제 능력은 같은 pH 값에서 결합재의 종류에 따라 다양하게 나타났다. 부식전류가 $0.1-0.2{\mu}A/cm^{2}$에 이를 때 부식이 발생한다는 가정하에, 부식에 대한 임계 염소이온 농도에 대하여 OPC는 1.03, 30% PFA는 0.65, 60% GGBS는 0.45, 10% SF는 0.98%로 각각 계산되었다. 그에 비해 임계 염소이온 농도의 새로운 표현방법으로 제시한 [$Cl^{-}$]:[$H^{+}$] 몰 농도비의 단위로 계산하였을 때, 임계 염소이온 농도는 결합재에 관계없이 0.008-0.009로 도출되었다.

• The Korean Journal of Ecology
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• 제16권2호
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• pp.169-180
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• 1993

Soils of four combinations, sand with high content of organic matter(SL), sand with low content of OM(SS), siltyl loam with high content of OM(LL) and silty loam with low content OM (LS), were filled on column and then percolated with simulated sulfuric acid rain with pH 5.6, 4.0, 3.5, 3.0 and 2.5. From soil leachates, pH and concentrations of basic cations and Al were determined. Cation concentrations in the leachates increased as pH of the rain decreased. The orders of buffering capacity of soil, leachability of cation from soil, leaching sensitivity of ion andbase saturation sensitivity of soil to acidity of the rain water were SS$\leq$K <$\leq$LL

• 한국환경과학회지
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• 제7권2호
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• pp.149-156
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• 1998

Enoronmental problems caused by certain geologic conditions Include pollution of soil by heavy metal, acidization of souls , acid mine drainage, Pound-water pollution, and natural radioactivity, as well as zoo-logical hazards such as landslide and subsidence. The acrid mine drainage contains large amount of heavy metals nO, therefore. cause serious pollution onto the nearby drainage systems and soils. In spite of this prospective environmental danger, few studies have been done on the acid mine drainage derived from non-metallic ore deposits such as pyrophyllitefNapseok) deposits. The sudo-bearing pyrophyllite ores, alteration zones, and mine talllngs of pyrophylllte deposits produce acrid mine drainage by the okidation of weathering. Compared to the fresh host rocks, the ores and altered rocks of pyrophyllite deposits produce acidic solution which contain higher amount of heavy metals because of OeP lower buffering capacity to acrid solution. The pus of urine water and nearby stream water of pyrophyllite deposits are 2.1~3.7, which are strong- ly acidic and much lower than that (6.2~7.2) of upstream water and than that (6.8~7.6) of the stream water derived from the non-mineralized area. This study reveals that this acrid mine drainage can affect the downstream area which is 8km far from the pyrophyllite deposits, even though the drain Is diluted with abundant non-contaminated river water This suggmists that not only acid mine drainage but also the sulfide-bearing sediments originated from the pyrophyllite deposits move downstream and form acidic water through continuous oxidation reaction. The heavy metals such as Pb, Zn, Cu, Cd, Nl, Mn and Fe are enriched In the mine water of low pH, and their contents decrease as the pH of mine water Increases because of the Influx of fresh stream wainer. SoUs of the Pyrophyulte deposits are characterized by high contents of heavy metals. The stream sediments containing the yellowish brown precipitates formed by neutralization of acid mine drainage occur in all parts of the stream derived from the pyrophyllite deposits, and the sediments also contain high amounts of heavy metals. In summary, the acid mine drainage of the pyrophyllite deposits is located in the upstream part of Hoidong water reservoir in Pusan contains large amounts of heavy metals and flows into the Holdong water reservoir without any purification process. To protect the water of Holdong reservoir, the acid mine drainage should be treated with a proper purification process.

• 한국토양비료학회지
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• 제30권1호
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• pp.56-61
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• 1997

원예작물(園藝作物) 영농방식(營農方式)이 노지(露地)에서 시설재배(施說栽培)로, 직파(直播)에서 대규모 육묘재배(育苗栽培)로 전환됨에 따라 상토수요(床土需要)는 계속 증가되고 있으나, 이에 대한 적정 물리성(物理性) 기준 설정이 미흡하여 새로운 상토재료(床土材料)의 선발(選拔)과 적정상토(適正床土)의 제조(製造)에 필요한 기초 자료를 얻고자 시판(市販)되고 있는 주요 상토재료(床土材料)인 광물질(鑛物質) vermiculite 와 perlite, 유기재료(有機材料)인 peatmoss, osmunda 와 bark을 가지고 주요 물리성(物理性)인 입경(粒徑), 보수력(保水力)과 삼상(三相) 등을 조사(調査) 분석(分析)하였다. Peatmoss는 직경이 0.25mm 에서 16mm 까지의 입자들이 고르게 분포되어 있으나, bark는 5.7mm 이상의 입자가, osmunda는 2.0mm 이상, vermiculite는 1.0~3.4mm, Perlite 는 0.5~2.0mm 크기의 입자가 대부분이었다. 광질(鑛質)인 vermiculite와 perlite는 pH가 7.0 이상으로 높으나, 유기질(有機質)인 peatmoss는 pH 3.8 내외로 아주 낮고, bark와 osmunda는 pH 5.5 내외이었다. 수분장력 1kPa에서 5kPa 사이인 역용수분함량(易用水分含量)은 peatmoss가 39.2%, perlite 34.0%, vermiculite 16.9% 의 순이었으며, osmunda와 bark 는 4.8% 이하 이었으며 5kPa에서 10kPa 사이인 완형수분량(緩衡水分量) (Water buffering capacity)은 peatmoss와 vermiculite 가 각각 6.1% 와 2.3% 이었고, 나머지는 1% 미만으로 매우 낮았다. Osmunda와 bark는 수분의 감소곡선(減小曲線)과 공기의 증가곡선(增加曲線)이 만나는 최적수분장력이 0.64kPa, 0.73kPa로 쉽게 물이 빠지는 경향(傾向)이므로 적정치 2.5kPa에 접근시키려면 세립질(細粒質) 물질의 첨가가 필요하고, peatmoss, perlite, vermiculite는 이 값이 4kPa 부근이므로 더욱 조립질(粗粒質)의 재료(材料)를 혼합이 필요한 것으로 판단된다. Pot 상태에서 상토재료별로 물을 충분히 간직하고 있는 상태에서의 수분장력은 peatmoss가 2.2kPa에 해당하였으며, 대체로 1kPa~4.3kPa 범위에 있었다.