• Korean Journal of Food Science and Technology
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• v.45 no.4
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• pp.473-477
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• 2013

The aim of this study was to identify the optimal ingredient-mixing ratio of Job's-tear and wheat flour subjected to extrusion. A modified distance-based mixture design analysis was chosen for the experimental design. The results showed that the bending failure force, the a-value, and the water absorbtion index (WAI) value had no correlation with the mixture ratio of Job's-tear and wheat flour. However, the diameter of the extrudates, the L- and b-values, and the water solubility index (WSI) value were all found to be correlated to the mixture ratio. While the first three values were determined using a linear model, the WSI value was determined using a quadratic model. The diameter and color had an inverse correlation to the mixture ratio: the higher the ratio of Job's-tear to wheat flour, the lower the diameter and darker the color. The L- and b-values were found to change in accordance with the mixture ratio of Job's-tear to wheat flour. The lowest WSI value was obtained at a 40:60 ratio of Job's-tear to wheat.

• Journal of Korea Water Resources Association
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• v.50 no.6
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• pp.429-440
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• 2017

A series of multispectral high-resolution Korean Multi-Purpose Satellite (KOMPSAT) images were analyzed to detect the geographical changes in four different tidal flats in the west coast of South Korea. The method of unsupervised classification was used to generate a series of land use/land cover (LULC) maps from the satellite images, which were used as the input of the temporal trajectory analysis to detect the temporal change of coastal wetlands and its association with natural and anthropogenic activities. The accurately classified LULC maps extracted from the KOMPSAT images indicate that these multispectral high-resolution satellite data is highly applicable to generate good quality thematic maps for extracting wetlands. The result of the trajectory analysis showed that, while the tidal flat area of Gyeonggi and Jeollabuk provinces was estimated to have changed due to tidal effects, the reductive trajectory of the wetland areas belonging to the Saemangeum province was caused by a high degree of human-induced activities including large reclamation and urbanization. The conservation of the Jeungdo Wetland Protected Area in Jeollanam province revealed that the social and environmental policies can effectively protect coastal wetlands from degradation. Therefore, monitoring for wetland change using high resolution KOMPSAT is expected to be useful to coastal environment management and policy making.

• The Korean Journal of Nuclear Medicine Technology
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• v.16 no.1
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• pp.96-101
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• 2012

Purpose: Glomerular filtration rate is an important index for assessment of renal function, early discovery of renal disease, and progress observation of chronic renal disease patients. In the present study, the objective is to conduct a comparative analysis of differences between Gates and Modified Gates method in dynamic renal scintigraphy based on MDRD (Modification of Diet Renal Disease) formula using blood collection. Materials and Methods: Renal scintigraphy was performed for 45 patients who visited our hospital between November 2010 and August 2011. For 20 patients of those tested, glomerular filtration rates from Gates method and MDRD formula using AGUS equipment, were compared. For the other 20 patients, glomerular filtration rates from Modified Gates method and MDRD formula using INFINIA equipment. Finally, Gates and Modified Gates method were compared for 5 patients who indicated no change in glomerular filtration rates from MDRD formula during progress observation. Results: Glomerular filtration rates from both Gates and Modified Gates method showed a high correlation with those from MDRD formula ($p$<0.01, r=0.903, r=0.867), with a paired difference mean for Gates method of $2.05{\pm}2.54mL/min/1.73m$, and that for Modified Gates method of $25.2{\pm}3.71mL/min/1.73m$. Finally, the values for Gates method and those for Modified Gates method showed a high correlation for the five patients ($p$<0.05, r=0.949), with a paired difference mean of $20.4{\pm}8.84mL/min/1.73m$. Conclusion: Glomerular filtration rates from Gates method, Modified Gates method and MDRD formula showed mutually high correlations. If the tests are performed with recognition for the correlations between Gates and Modified Gates method used in a dynamic renal scintigraphy, then an accurate assessment of renal function is considered possible with an improved diagnostic ability.

• Geophysics and Geophysical Exploration
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• v.10 no.4
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• pp.369-376
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• 2007

Electrical resistivity tomography was carried out at seawater intrusion monitoring wells located at watershed in coastal areas. It is difficult to identify the characteristics of resistivity near monitoring well in case of using high signalto-noise ratio array due to the high conductivity condition in coastal aquifer although electrical resistivity survey is well adopted to delineate hydrogeological characteristics with the distribution of electrical resistivity. To improve the quality of electrical resistivity survey for two sites with seawater intrusion monitoring wells, inversion with the results of holeto-surface electrical resistivity tomography using single well was executed. The results of inversion for aquifer near wells were verified with the results of drilling log with the informations of fracture, electrical conductivity logging and normal resistivity logging. The inversion for aquifer near one of two wells was also performed at low and high tide with the same electrodes, respectively. From the inversion result, it is possible to obtain the resistivity images with high resolution and to identify the characteristics of aquifer related to seawater intrusion with tidal fluctuation. From this study, it was demonstrated that the hole-to-surface electrical resistivity tomography method accompanied with drilling log, electrical conductivity logging and normal resistivity logging would be useful to delineate the hydrogeological structures near monitoring wells in coastal areas.

• The Korean Journal of Nuclear Medicine Technology
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• v.18 no.2
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• pp.48-56
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• 2014

Purpose $^{99m}Tc$-DTPA renal scintigraphy serves as a key indicator to measure a kidney donor's Glomerular Filtration Rate (GFR) and determine the possibility of kidney transplant. The Gates method utilized to measure GFR considers 3 variables of renal depth, injection dose, and net kidney counts. In this research, we seek to compare changes in kidney donors' GFR according to renal depth measurement methods of the 3 variables. Materials and Methods We investigated 32 kidney donors who had visited the hospital from October, 2013 to March, 2014 and received abdominal CT and $^{99m}Tc$-DTPA GFR examination. With the cross-section image of the CT and the lateral image from a gamma camera, we measured the renal depth and compared with renal depth calculation equations-Tonnesen, Taylor, and Itoh methods. Renal depth-specific GFR was calculated by using Xeleris Ver. 2.1220 of GE. Then the results were compared with MDRD (Modification of Diet Renal Disease) GFRs based on serum creatinine level. Results The renal depths measured based on the CT and gamma camera images showed high correlation. Tonessen equation gave the lowest GFR value while the value calculated by using the renal depth of CT image was the highest with a 16.62% gap. MDRD GFR showed no statistically significant difference among values calculated through Taylor, Itoh, CT and gamma camera renal depth application (P>0.05), but exhibited a statistically significant change in the value based on Tonnesen equation (P<0.05). Conclusion This research has found that, in GFR evaluation in kidney donors by utilizing $^{99m}Tc$-DTPA, Tonnesen equation-based Gates method underestimated the value than the MDRD GFR. Therefore, if a MDRD GFR value shows a huge difference from the actual examination value, using an image-based renal depth measurement, instead of Tonnesen equation applied to Gates method, is expected to give an accurate GFR value to kidney donors.

• Journal of Chest Surgery
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• v.38 no.12 s.257
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• pp.835-843
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• 2005

Background: Cancer of the esophagus is one of the most malignant tumors with poor prognosis. The p53 gene alteration, over expression of Cyclin D1, and Ki67 index were thought to be the prognostic factors. However, their clinical significances in esophageal squamous cell carcinoma are controversial and p53 accumulation may not correlate with genetic mutation. The current study investigates their prognostic significance in squamous cell carcinoma of the esophagus. Material and Method: The Subjects studied were 124 esophageal squamous cell carcinoma patients who underwent esophagectomy. The mutation of p53, over expression of Cyclin D1, Ki67 labelling index, mitotic index were examined by using an immunohistochemical staining. We compared the results and investigated the correlation with the mutation of p53, overexpression of Cyclin D1, Ki67 labelling index, mitotic index and tumor size, and duration of survival. Result: There was no correlation between the results in immunohistochemical staining according to age, sex, tumor size, Iymph node status, and clinical stage of the disease. Mutant p53 protein was found in 69 cases (55.6$\%$). Median survival time was 21 months in cases with negative for mutant p53 protein and 22 months in positive cases. There was no significant difference in survival (p=0.46). Median survival time was 22 months in cases with negative for Cyclin D1 and 16 months in positive cases (p=0.18). Median and mean survival time was 22 months and 36 months when Ki67 labeling index was 40 or less (102 cases). Median and mean survival was 16 months and 23 months, when Ki67 labeling index was more than 40 (22 cases). There was significant difference in survival rate (p=0.011). Conciusion: Positivity of p53 and cyclin D1 was not useful in predicting the prognosis in our study. There was no significant correlation among mutant p53 protein accumulation, Cyclin D1 over expression, and Ki67 labeling index. However, in several studies, PCR single strand conformational polymorphism analysis of p53 showed a correlation to the prognosis. We thought that there was a significant discordance between p53 gene mutation and mutant p53 protein accumulation. When Ki67 labeling index was more than 40, prognosis was poorer, Ki67 seems to be a prognostic factor in our study. Therefore, we confirmed the possibility of using molecular markers as prognostic factors.

• The Korean Journal of Petroleum Geology
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• v.14 no.1
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• pp.1-11
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• 2008

As conventional oil and gas reservoirs become depleted, interests for oil sands has rapidly increased in the last decade. Oil sands are mixture of bitumen, water, and host sediments of sand and clay. Most oil sand is unconsolidated sand that is held together by bitumen. Bitumen has hydrocarbon in situ viscosity of >10,000 centipoises (cP) at reservoir condition and has API gravity between $8-14^{\circ}$. The largest oil sand deposits are in Alberta and Saskatchewan, Canada. The reverves are approximated at 1.7 trillion barrels of initial oil-in-place and 173 billion barrels of remaining established reserves. Alberta has a number of oil sands deposits which are grouped into three oil sand development areas - the Athabasca, Cold Lake, and Peace River, with the largest current bitumen production from Athabasca. Principal oil sands deposits consist of the McMurray Fm and Wabiskaw Mbr in Athabasca area, the Gething and Bluesky formations in Peace River area, and relatively thin multi-reservoir deposits of McMurray, Clearwater, and Grand Rapid formations in Cold Lake area. The reservoir sediments were deposited in the foreland basin (Western Canada Sedimentary Basin) formed by collision between the Pacific and North America plates and the subsequent thrusting movements in the Mesozoic. The deposits are underlain by basement rocks of Paleozoic carbonates with highly variable topography. The oil sands deposits were formed during the Early Cretaceous transgression which occurred along the Cretaceous Interior Seaway in North America. The oil-sands-hosting McMurray and Wabiskaw deposits in the Athabasca area consist of the lower fluvial and the upper estuarine-offshore sediments, reflecting the broad and overall transgression. The deposits are characterized by facies heterogeneity of channelized reservoir sands and non-reservoir muds. Main reservoir bodies of the McMurray Formation are fluvial and estuarine channel-point bar complexes which are interbedded with fine-grained deposits formed in floodplain, tidal flat, and estuarine bay. The Wabiskaw deposits (basal member of the Clearwater Formation) commonly comprise sheet-shaped offshore muds and sands, but occasionally show deep-incision into the McMurray deposits, forming channelized reservoir sand bodies of oil sands. In Canada, bitumen of oil sands deposits is produced by surface mining or in-situ thermal recovery processes. Bitumen sands recovered by surface mining are changed into synthetic crude oil through extraction and upgrading processes. On the other hand, bitumen produced by in-situ thermal recovery is transported to refinery only through bitumen blending process. The in-situ thermal recovery technology is represented by Steam-Assisted Gravity Drainage and Cyclic Steam Stimulation. These technologies are based on steam injection into bitumen sand reservoirs for increase in reservoir in-situ temperature and in bitumen mobility. In oil sands reservoirs, efficiency for steam propagation is controlled mainly by reservoir geology. Accordingly, understanding of geological factors and characteristics of oil sands reservoir deposits is prerequisite for well-designed development planning and effective bitumen production. As significant geological factors and characteristics in oil sands reservoir deposits, this study suggests (1) pay of bitumen sands and connectivity, (2) bitumen content and saturation, (3) geologic structure, (4) distribution of mud baffles and plugs, (5) thickness and lateral continuity of mud interbeds, (6) distribution of water-saturated sands, (7) distribution of gas-saturated sands, (8) direction of lateral accretion of point bar, (9) distribution of diagenetic layers and nodules, and (10) texture and fabric change within reservoir sand body.