• 대한예방의학회:학술대회논문집
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• 1998.10b
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• pp.127-128
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• 1998

• The Journal of Engineering Geology
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• v.19 no.2
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• pp.165-175
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• 2009

This study is concerned with creep characteristics of red shale in the Haman Formation by the single stage and multi stage loading tests. Creep constants in the Griggs's experiential equation, ${\epsilon}_t$= a+$b{\cdot}log$ t + $c{\cdot}t$, are determined by regression analysis on the total data obtained. The transition time between the primary and second creep means the time when the differential value of $b{\cdot}log$ t is equal to the differential value of $c{\cdot}t$. The correlation equation between loads (${\sigma}$%) and creep constants is deduced from the three times multi stage loading tests. Also a failure time under each loads is anticipated from creep constants and maximum strain at the failure.

• The Korean Journal of Quaternary Research
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• v.25 no.2
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• pp.39-48
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• 2011

Phytolith analysis of sediments at the river mouth of valley bottom plains in Myosa-ri, Haman is performed. By the phytolith results, Phragmites and Oryza sativa are dominated in the lower horizon. An abundance of Paniceae and Andropogoneae indicates the active agricultural activities under wet conditions. Moreover, the results of archeological studies suggest the paddy fields in the Three States Age. The phytolith assemblages are dominated in the middle horizon and they gradually increase in the upper horizon. The rice cultivation layer is not proportional to total phytolith yield due to the dominance of Oryza sativa in the lower horizon. However, because the Oryza sativa are continuously observed over the entire sediments, it is suggested that there had been the agricultural activities for the entire periods.

• Economic and Environmental Geology
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• v.30 no.4
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• pp.327-340
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• 1997

Geochemical characteristics of groundwater, based on chemical analyses of 54 water samples, differ among main rocks of Haman formation, Panyawoel formation, andesite and granite in Daegu area in relation to mineralogical and chemical compositions of the rocks. Concentrations of most solutes are higher in groundwaters of Haman and Panyawoel formations than in those of andesite and granite. High concentrations of $Ca^{2+}$ and $Mg^{2+}$ in groundwaters of the sedimentary rocks result mainly from reaction of $CO_2$-charged water with calcite and weathered feldspars. Average groundwaters in the sedimentary rocks are oversaturated with respect to calcite. Major types of groundwaters are hard $Ca(HCO_3)_2$ and $CaSO_2-CaCl_2$ with hardness of 442 mg/l for Haman formation and 275 mg/l for Panyawoel formation whereas they are soft $Ca(HCO_3)_2$ with hardness 35 mg/I for andesite and 39 mg/I for granite. $Ca(HCO_3)_2$ type results mainly from calcite-dissolution and $CaSO_4-CaCl_2$ from pyrite and partly from domestic pollutants. $CaSO_4-CaCl_2$ type may indicate that groundwaters in the sedimentary rocks are more evolved geochemically than those in the igneous rocks, but it is not obvious because the type might be affected by pyrie dissolution and domestic pollutions. Acid rain is buffered by active calcite in the sedimentary rocks. In the igneous rocks acid rain might react with gibbsite and other forms of $Al(OH)_3$ that might have accumulated as weathering products of primary silicates, and is buffered.

• Journal of People, Plants, and Environment
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• v.23 no.1
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• pp.35-46
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• 2020

The purpose of this study was to investigate the effects of the horticultural therapy program on patients with mild cognitive impairment and mild dementia depending on the frequency and duration of the interventions. We developed the same 15-session program to improve cognitive functions and life satisfaction and alleviate depression of the elderly women with mild cognitive impairment or mild dementia. Subjects in Longer Treatment group participated in the program once a week for 15 weeks and subjects in Shorter Tratmet group participated twice a week for 7½ weeks. This study conducted pretest-posttest verification of both groups using quasi-experimental design involving 21 subjects. Elderly life satisfaction, Geriatric Depression Scale (short form), and the Korean Version of Consortium to Establish a Registry of Alzheimer's Disease (CERAD-K) were used in the evaluation. As a result, both groups showed an increase in life satisfaction, and a decrease in depression. However, there was a significant difference in the changes of the CERAD-K scores between the two groups (p < .05). In Longer Treatment group, life satisfaction increased significantly (p < .001), and depression decreased at a marginally significant level (p = .068), but no statistically significant change was observed in neurocognitive function. In Shorter Treatment group, life satisfaction increased at a marginally significant level (p = .059), and depression and CERAD-K scores decreased significantly (p < .05). However, in the case of Mini-Mental State Examination (MMSE-K), there was no significant change in both groups. According to these results, when planning a horticultural therapy program for persons with mild cognitive impairment or mild dementia, it is effective to organize and execute the program by determining the duration of intervention as 3 to 4 months or longer, even if this reduces the number of interventions per week.

• Korean Journal of Environmental Agriculture
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• v.16 no.4
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• pp.356-364
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• 1997

To investigate the water quality status of agricultural water source for greenhouse area in Gyeongnam, the surface water quality was examined six times from October in 1995 to March in 1996 at five areas in Gyeongnam. The pH values of surface water were in the range of 6.6${\sim}$9.1 pH in Kimhae and Changnyong areas were out of range in 6.0${\sim}$8.5 which was water quality standard for agriculture. The DO values of surface water were relatively high with average 10.0mg/l in Kimhae, Changnyong, Sacheon and Chinju areas except for Haman area. The BOD values of surface water exceeded water quality standard for agriculture(8.0mg/l) in three sites and one site in Haman and Sacheon, respectively. The COD values of surface water exceeded water quality standard for agriculture(8.0mg/l) in Kimhae, Changnyong and Haman. The ${NH_4}^+-N$ values in surface water of Changnyong and Haman areas were 1.21mg/l and 2.75mg/l, respectively. The average values of $NO_3\;^--N$ in surface water was appropriate for agriculture. The values of $K^+,\;Na^+,\;Mg^{2+},\;Ca^{2+},\;{PO_4}^{3-}$ and $SO_4^{2-}$ in Haman were the highest of those of the others. And Pb was below 0.1mg/l which was water quality standard for agriculture. The average values of Cu, Cd and Zn were below water quality standard for agriculture. Between COD and SS in surface water was positively correlated with r$=0.799^{{\ast}{\ast}}$. BOD in surface water was positively correlated with $NH_4\;^+-N,\;PO_4\;^{3-},\;SS,\;K^+,\;Na^+$ and $Cl^-$. Surface water pollution status of agricultural water source of greenhouse areas in Gyeongnam was in order of Chinju< Sacheon< Kimhae< Changnyong< Haman area.

• Proceedings of the KSEG Conference
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• 2003.04a
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• pp.159-163
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• 2003

• 한국문화재보존과학회:학술대회논문집
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• 2005.03a
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• pp.114-130
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• 2005

• 한국지구과학회:학술대회논문집
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• 2004.02a
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• pp.59-59
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• 2004

• Journal of Ocean Engineering and Technology
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• v.32 no.5
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• pp.361-366
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• 2018

The present study analyzed the variation factors in inducing a salinity change using the existing observation network in the section between the Nakdong River Estuary Barrage and Changnyeong-Haman Weir, and also examined the seasonal changes in precipitation, salinity, and discharge. Furthermore, this study analyzed the causes of a salinity increase by collecting observational data during a period when abnormal salinity occurred, and further investigated the salinity transfer time in a section of approximately 5.3 km from the Nakdong River Estuary Barrage to Nakdong River Bridge to understand the behavioral characteristics of the salinity moving upstream. The study results would make it possible to control the increase in salinity and block salt water from moving upstream by understanding the salinity variation characteristics according to the discharge amount. This will provide stability in collecting water from various residential, agricultural, and industrial sources through water intake facilities scattered near the Nakdong River Estuary Barrage.