• Environmental Sciences Bulletin of The Korean Environmental Sciences Society
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• 제4권1호
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• pp.51-57
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• 2000

Changes in the proline accumulation of ten-day-old seedlings of Vigna angularis in response to NaCl treatment were monitored. The proline content increased gradually both with an increase in the exposure time to salt stress and in a concentration-dependent manner. The increased proline accumulation was stronger in the shoots than in the roots. The salt stress by itself resulted in a significant inhibition of the chlorophyll content. Pre-treatment with proline before salinization lasting 48 h did not significantly affect the endogenous proline level in the roots, in contrast, a considerable increase of proline was observed in the shoots. The application of exogenous proline to the seedlings increased the endogenous proline content and improved the root and shoot growth under saline conditions. Detached leaves also exhibited an increased proline level in response to the applied NaCl, however, at a lower magnitude than in the intact seedlings. The proline alleviated the inhibitory effect of the NaCl in a concentration-dependent manner, thereby suggesting that salinity is a strong inducer of proline accumulation. In addition, abscisic acid eliminated the inhibitory effect of the salt salinity, thereby indicating a protective role on salinity stress and a regulatory role in proline synthesis. Accordingly, it would appear that proline may be involved in salt tolerance.

• BMB Reports
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• 제46권9호
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• pp.439-447
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• 2013

Rice is a monocot gramineous crop, and one of the most important staple foods. Rice is considered a model species for most gramineous crops. Extensive research on rice has provided critical guidance for other crops, such as maize and wheat. In recent years, climate change and exacerbated soil degradation have resulted in a variety of abiotic stresses, such as greenhouse effects, lower temperatures, drought, floods, soil salinization and heavy metal pollution. As such, there is an extremely high demand for additional research, in order to address these negative factors. Studies have shown that the alternative splicing of many genes in rice is affected by stress conditions, suggesting that manipulation of the alternative splicing of specific genes may be an effective approach for rice to adapt to abiotic stress. With the advancement of microarrays, and more recently, next generation sequencing technology, several studies have shown that more than half of the genes in the rice genome undergo alternative splicing. This mini-review summarizes the latest progress in the research of splicing and alternative splicing in rice, compared to splicing in humans. Furthermore, we discuss how additional studies may change the landscape of investigation of rice functional genomics and genetically improved rice.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
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• pp.450-452
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• 2004

Using factor analysis and bivariate comparisons of major components in ground water, three geochemical processes were identified as controlling factors of ground water chemistry; 1) natural mineralization by water rock interactions, 2) effect of seawater which includes salinization by seawater near seashores and deposition of sea salt, and 3) nitrate contamination by N fertilization. Contribution of rainfall was also estimated from the measured composition of wet deposition. The geochemical processes were separated using total alkalinity as an indicator for natural mineralization, Cl for effect of seawater, and nitrate for N fertilization. Relatively high correlation of major components with nitrate suggests that nitrification of nitrogenous fertilizers significantly affects ground water chemistry. Total cations derived from nitrate sources have good linearity for nitrate in equivalent basis with a slope of 1.8, which is a mean of proton production coefficients in nitrification of two major compounds in nitrogenous fertilizers, ammonium and urea. Contribution of nitrate sources to base cations, Cl, and SO$_4$ in ground water was determined considering maximum contribution of natural mineralization to estimate a threshold of the effect of N fertilization for ground water chemistry, which shows W fertilization has a greatest effect than any other processes in ground water with nitrate concentration greater than 50 mg/L for Ca, Mg, Na and with concentration greater than 30 mg/L for Cl and SO$_4$.

• 농촌계획
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• 제8권1호
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• pp.41-59
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• 2002

The condition and management of land resources has become an increasing matter of concern in recent years, because of the pressure placed upon land for agricultural use by expanding populations and economic development. Pressures upon land quality can lead to various forms of land degradation, such as in soil erosion, soil fertility decline, adverse changes in water resources, salinization of irrigated areas, or decline in the biological condition of forests or rangelands. In 1992, World Bank estimates that the cost of degraded areas has been estimated as 10-50 times higher than that of measures to prevent degradation. Based upon a survey interviewed with people living in rural areas, the present study argue that it is important to establish policies for preventing changes in agricultural land use, to provide early warning of adverse trends and identification of problem areas. The present study also stresses that stewardship of agricultural land resources plays a leading role in achieving sustainable rural development not to mention agricultural and forestry production.

• 한국암석학회:학술대회논문집
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• 한국암석학회.한국광물학회 2000년도 공동학술발표회 논문집
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• pp.3-11
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• 2000

The earth environment consists of four spheres : geosphere, hydrosphere, atmosphere and biosphere. The geosphere consists mostly of minerals. It, however, contains some water and air in its shallow depth. Although hydrosphere and atmosphere consist predominantly of water and air, respectively, both contain some minerals. The biosphere consisting of various organisms is present in the interfaces of geosphere, hydrosphere and atmosphere. The natural environment of the earth is continuously changing by the interaction of four spheres. It suggests that out relevant environmental problems can not be revolved without understanding the natural relationship of these four spheres. Minerals in our environment are very important because they are the main constituent materials of the earth and they control our environment. The roles of minerals in our environment have not been understood even in the scientific society. Thus their roles have been neglected. Review of studies on the environmental mineralogy so far made at our laboratory and others show that minerals control the environment in various ways. Minerals neutralize the acid water as well as acid rain. Minerals in soils and rocks are major neutralizer of the acid rain. Salinization of sea water is attributed to the ionic substitution between minerals and sea water. Some minerals control the humidity of the air. Corals, the products of biomineralization, are the main carbon controller of the air. Minerals also adsorb heavy metals, organic pollutants and radioactive nuclides. Such remarkable functions for controlling the environment come from the mineral-water reaction and biomineralization. All these phenomena are subjects of the environmental mineralogy, a new field of earth science.

• 한국토양비료학회지
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• 제45권6호
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• pp.1065-1072
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• 2012

Crop productivity decreases globally as a result of salinization. However, salinity impact on greenhouse-grown crops is much higher than on field-grown crops due to the overall concentrations of nutrients in greenhouse soils. Therefore, this study was performed to determine the short-term changes in growth, photosynthesis, and metabolites of tomato plants grown in greenhouse under heavily input of fertilizers evaluated by microbial activity and chemical properties of soils. The soils (< 3, 3.01~6, 6.01~10 and > 10.01 dS $m^{-1}$) from farmer's greenhouse fields having different fertilization practices were used. Results showed that the salt-accumulated soil affected adversely the growth of tomato plants. Tomato plants were seldom to complete their growth against > 10.0 dS $m^{-1}$ level of EC. The assimilation rate of $CO_2$ from the upper fully expanded leaves of tomato plants is reduced under increasing soil EC levels at 14 days, however; it was the highest in moderate or high EC-subjected (3.0 ~ 10.0 dS $m^{-1}$) at 28 days. In our experiment, soluble sugars and starch were sensitive markers for salt stress and thus might assume the status of crops against various salt conditions. Taken together, tomato plants found to have tolerance against moderate soil EC stress. Various EC levels (< 3.0 ~ 10.0 dS $m^{-1}$) led to a slight decrease in organic matter (OM) contents in soils at 28 days. Salinity stress led to higher microbial activity in soils, followed by a decomposition of OM in soils as indicated by the changes in soil chemical properties.

• 한국작물학회:학술대회논문집
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• 한국작물학회 2017년도 9th Asian Crop Science Association conference
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• pp.188-188
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• 2017

Rice (Oryza sativa L.) is one of the major crops that is seriously impacted by global soil salinization. Rice is among those crops where most of the high-yielding cultivars are highly sensitive to salinity. The key to a plant survival under NaCl salt stress is by maintaining a high $K^+/Na^+$ ratio in its cells. Selection for salinity tolerance genotypes of rice based on phenotypic performance alone is less reliable and will delay in progress in breeding. Recent advent of molecular markers, microsatellites or simple sequence repeats (SSRs) were used to find out salt tolerant rice genotypes. In the current experiment phenotyping and genotyping studies were correlated to differentiate different rice accessions for salinity tolerance. Eight rice accessions along with check plant Dongjin were screened by physiological studies using Yoshida solution with 50mM NaCl stress condition. The physiology studies identified four tolerant and four susceptible accessions based on their potassium concentration, sodium concentration, $K^+/Na^+$ ratio and biomass. 17 SSR markers were used to evaluate these rice accessions for salt tolerance out of which five molecular markers were able to discriminate tolerant accessions from the susceptible accessions. Banding pattern of the accessions was scored comparing to the banding pattern of Dongjin. The study identifies accessions based on their association of $K^+/Na^+$ ratio with molecular markers which is very reliable. These markers identified can play a significant role in screening large set of rice accessions for salt tolerance; these markers can be utilized to improve salt tolerance of commercial rice varieties with marker-assisted selection (MAS) approach.

• Asian Journal of Atmospheric Environment
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• 제9권2호
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• pp.173-186
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• 2015

In Bangladesh, increases in the tropospheric ozone ($O_3$) concentration and in soil salinization may lead to crop damage. To clarify the effects of $O_3$ and/or soil salinity on Bangladeshi wheat cultivars, BAW1059 (salt-tolerant) and Shatabdi (salt-sensitive) were exposed to 70-day treatments with $O_3$ (charcoal-filtered air (CF), $1.0{\times}O_3$, and $1.5{\times}O_3$) and different levels of soil salinity (0, 4, and $8dS\;m^{-1}$). In both cultivars, the whole-plant dry mass and grain yield were significantly reduced by exposure to $O_3$. Increased soil salinity caused significant reductions in whole-plant growth and yield in Shatabdi, but the reductions were negligible in BAW1059. No significant interactions between $O_3$ and salinity were detected for growth, yield, and leaf gas exchange parameters in both cultivars. We concluded that the effects of $O_3$ are not ameliorated by soil salinity in two Bangladeshi wheat cultivars, regardless of their salinity tolerance.

• 환경영향평가
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• 제25권1호
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• pp.41-50
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• 2016

우리나라는 약 30년 간 환경영향평가가 시행되고 있으며 이 기간 동안 환경영향평가의 대상 사업 및 평가 항목 등에 대한 다양한 개정이 수행되었다. 하지만 현행 환경영향평가법 상의 토양 관련 평가 항목은 토양 환경의 일부분에 국한하여 고려되고 있다. 본 연구는 국내 환경영향평가 지침을 분석하여 토양 관련 평가 항목을 분석하였으며 해외의 환경영향평가제도 내 토양 관련 평가항목을 분석하였다. 이를 통해 국내 환경영향평가 제도에서 토양 환경 평가의 문제점과 시사점을 도출하였다. 우리나라의 경우 환경영향평가 제도 내의 수질, 토양, 지형 지질, 수리 수문 평가 항목에서 토양과 관련된 인자를 분석하고 있다. 그 대상은 토양 오염도, 비옥토, 우수유출량, 비점오염원 등 주로 오염과 관련한 인자이다. 하지만 해외의 경우 토양 압밀, 토양 밀폐, 토양 염류화 등 토양의 기능 및 질과 연관된 항목을 분석 중에 있다. 우리나라 국토의 지속가능한 개발을 위하여 해외의 경우와 마찬가지로 토양 관련 평가 인자를 개정할 필요가 있다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2019년도 학술발표회
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• pp.223-223
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• 2019

기후 변화에 따른 해수면 상승은 해안 지하수의 해수침투를 야기해 해안 지하수의 염도를 증가시킨다. 또한 해수면 상승은 토양 염류화를 심화시켜 농작물에 피해가 발생하며, 지하수위를 증가시켜 불포화대의 토양두께가 감소한다. 이처럼 지하수 해수침투가 발생하는 포화대와 토양 염류화가 발생하는 불포화대는 서로 연관되어 있지만, 대부분 포화대와 불포화대 연구는 별도로 진행되어왔다. 본 연구에서는 해안 간척지의 해수면 상승에 따른 포화대의 해수침투 및 불포화대의 토양염류화 영향을 연계하여 모의하였다. 포화대 모의는 미국지질조사국(United States Geological Survey, USGS)에서 개발한 3차원 이송확산 모델인 SUTRA, 불포화대 모의는 미국환경청(United States Environmental Protection Agency, USEPA)에서 개발한 1차원 이송확산모델인 VADOFT를 사용하였다. 해수면 상승 시나리오는 IPCC에서 공표한 바와 같이 RCP 4.5와 RCP 8.5 시나리오를 사용하였고, 미래 2100년까지 자료를 사용하였다. 해수면 상승 시나리오에 따라 해수침투 및 토양염류화 면적 그리고 지하수위 및 불포화대 토양두께를 정량적으로 산정하였다. 한반도 91개 간척지에 대해서 모의를 수행하였고, 과거 대비 미래 후반기 RCP 4.5 시나리오에서는 지하수 해수침투 면적이 $82.19km^2$, RCP 8.5 시나리오에서는 $83.71km^2$ 증가하는 것으로 나타났다. 또한 토양 염류화 면적은 과거 대비 미래 후반기 RCP 4.5 시나리오에서는 $22.25km^2$, RCP 8.5 시나리오에서는 $24.86km^2$ 증가하는 것으로 나타났다. 담수호 또는 저수지가 있는 대상 지역에서는 해안선으로부터 거리 및 관리 수위가 해수 침투를 야기시키는 중요한 요인으로 나타났으며, 해수침투 저감을 위해서는 해안선 인근 저수지 수위의 적절한 유지관리가 필요할 것으로 판단된다. 본 연구에서는 해수면상승에 따른 해안선의 위치변화와, 기존 관정에서의 양수량, 강수량 변화를 고려하는 것에 한계가 있기 때문에, 향후 위의 세 가지 사항을 복합적으로 고려한 추가 연구가 필요하다고 사료된다.