• 대한전기학회:학술대회논문집
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• 대한전기학회 2011년도 제42회 하계학술대회
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• pp.1320-1321
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• 2011

According to the advance that solar power plants go into the desert, power plants are getting greater capacity. The desert is unspoiled resources and it is well suited to build a solar power plant, because of abundant solar radiation and long sunshine duration. but existing PV modules have several weaknesses and don't generate lower the rated power, because it wasn't designed to produce in extreme environments like a desert climate. The one of the weaknesses of PV modules is that the characteristics of the temperature of the Encapsulants(EVA sheet) are not good in a desert climate, because the EVA sheet is melt at high temperature. In this study, a decrease phenomenon of the transmittance depending on the melting point of the Encapsulant(PV module using EVA sheet : $75^{\circ}C$ PV module using PVB film : $110^{\circ}C$) is suggested, it would be the one of the important factors to achieve rated output of the PV modules in high temperature climate regions.

• Journal of Ecology and Environment
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• 제47권4호
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• pp.177-186
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• 2023

Background: Inner Mongolia, desertification is happening due to climate change and land use alterations. In order to evaluate desert restoration effectiveness, this study compares number of species and species diversity in restored (with planted trees), unrestored area, and the reference ecosystem (Ref-E, typical steppe and woody steppe). Results: The Ref-E had the most plant species (64 taxa), while the unrestored area had the fewest (5 taxa). Among restored areas (restored in 2012, 2008, 2005), older restoration sites had more species (18-42). Similarly, species richness (3.93-0.41) and diversity (1.99-0.40) were highest in the Ref-E and lowest in unrestored areas, with older restored sites having higher values. Conclusions: More plant species and diversity in older restoration areas suggest progress toward ecosystem stabilization, approaching the Ref-E. Therefore, tree planting in Inner Mongolia's Hulunbuir semi-arid desert is a successful restoration effort.

• 한국제4기학회지
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• 제17권2호
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• pp.33-38
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• 2003

This study is conducted to examine the data of climate or environmental change in the northeastern Asia during the last glacial maximum. A remarkable feature of the 18,000 BP biome reconstructions for China is the mid-latitude extention of steppe and desert biomes to the modem eastern coast. Terrestrial deposits of glacial maximum age from the northern part of Yellow Sea suggest that this region of the continental shelf was occupied by desert and steppe vegetation. And the shift from temperate forest to steppe and desert implies conditions very much drier than present in eastern Asia. Dry conditions might be explained by a strong winter monsoon and/or a weak summer monsoon. A very strong depression of winter temperatures at LGM. has in the center of continent has influenced in northeast Asia similarly. The vegetation of Hokkaido at LGM was subarctic thin forest distributed on the northern area of middle Honshu and cool and temperate mixed forest at southern area of middle Honshu in Japan. The vegetation landscape of mountain- and East coast region of Korea was composed of herbaceous plants with sparse arctic or subarctic trees. The climate of yellow sea surface and west region of Korea was much drier and temperate steppe landscape was extended broadly. It is supposed that a temperate desert appeared on the west coast area of Pyeongan-Do and Cheolla-Do of Korea. The reconstruction of year-round conditions much colder than today right across China, Korea and Japan is consistent with biome reconstruction at the LGM.

• Proceedings of the National Institute of Ecology of the Republic of Korea
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• 제1권1호
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• pp.58-67
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• 2020

Terrestrial ecosystems influence climate change via their climate regulation function, which is manifested within the carbon, water, and energy circulation between the atmosphere and surface. However, it has been challenging to quantify the climate regulation of terrestrial ecosystems and identify its regional distribution, which provides useful information for establishing regional climate-mitigation plans as well as facilitates better understanding of the interactions between the climate and land processes. In this study, a land surface model (LSM) that represents the land-atmosphere interactions and plant phenological variations was introduced to assess the contributions of terrestrial ecosystems to atmospheric warming or cooling effects over East Asia over the last half century. Three main climate-regulating components were simulated: net radiation flux, carbon exchange, and moisture flux at the surface. Then, the contribution of each component to the atmospheric warming or cooling (negative or positive feedback to the atmosphere, respectively) was investigated. The results showed that the terrestrial ecosystem over the Siberian region has shown a relatively large increase in positive feedback due to the enhancement of biogeochemical processes, indicating an offset effect to delay global warming. Meanwhile, the Gobi Desert shows different regional variations: increase in positive feedback in its southern part but increase in negative one in its eastern part, which implies the eastward movements of desert areas. As such, even though the LSM has limitations, this model approach to quantify the climate regulation is useful to extract the relevant characteristics in its spatio-temporal variations.

• 한국대기환경학회지
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• 제29권1호
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• pp.64-73
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• 2013

Because some particulate matter emission sources may inherently produce soluble species, or some soluble species may be produced during atmospheric transport, it is important to understand the origin of a particles's solubility when water-soluble tracers are used in source apportionment studies. Laboratory experiments were performed on three types of soils (Mongolia grassland, Mongolia desert, and Korean rural soils), to study the impact of acidification by nitric acid vapor on the solubility of metals in the soils. To achieve this goal, concentrations of water-soluble metals (Na, Mg, Al, K, Ca, Mn, and Fe) in the soils measured before and after acidification. Contributions of concentrations of water-soluble metal species before and after acidification attack to their total concentrations varied little with soil type. Concentrations of water-soluble Mg, Al, K, Ca, Mn, and Fe from the soils after interaction with nitric acid vapor increased, with significant increases in soluble Ca and Mn for all soil types suggesting soil acidification enhances the amount of leachable metal species in soil dust. There was little increase in water-soluble Na and K after acidification for each soil type. This experiment demonstrates that quantities of water-soluble metal species in particulate matter are produced under high gaseous nitric acid conditions.

• Journal of Microbiology and Biotechnology
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• 제28권9호
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• pp.1517-1526
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• 2018

Investigating bacterial diversity and its metabolic capabilities is crucial for interpreting the ecological patterns in a desert environment and assessing the presence of exploitable microbial resources. In this study, we evaluated the spatial heterogeneity of physicochemical parameters, soil bacterial diversity and metabolic adaptation at meter scale. Soil samples were collected from two quadrats of a desert (Thar Desert, India) with a hot, arid climate, very little rainfall and extreme temperatures. Analysis of physico-chemical parameters and subsequent variance analysis (p-values < 0.05) revealed that sulfate, potassium and magnesium ions were the most variable between the quadrats. Microbial diversity of the two quadrats was studied using Illumina bar-coded sequencing by targeting V3-V4 regions of 16S rDNA. As for the results, 702504 high-quality sequence reads, assigned to 173 operational taxonomic units (OTUs) at species level, were examined. The most abundant phyla in both quadrats were Actinobacteria (38.72%), Proteobacteria (32.94%), and Acidobacteria (9.24%). At genus level, Gaiella represented highest prevalence, followed by Streptomyces, Solirubrobacter, Aciditerrimonas, Geminicoccus, Geodermatophilus, Microvirga, and Rubrobacter. Between the quadrats, significant difference (p-values < 0.05) was found in the abundance of Aciditerrimonas, Geodermatophilus, Geminicoccus, Ilumatobacter, Marmoricola, Nakamurella, and Solirubrobacter. Metabolic functional mapping revealed diverse biological activities, and was significantly correlated with physicochemical parameters. The results revealed spatial variation of ions, microbial abundance and functional attributes in the studied quadrats, and patchy nature in local scale. Interestingly, abundance of the biotechnologically important phylum Actinobacteria, with large proposition of unclassified species in the desert, suggested that this arid environment is a promising site for bioprospection.

• 한국지리정보학회지
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• 제11권4호
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• pp.94-100
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• 2008

기후 시스템에서 지구온난화는 세계적으로 매우 중요한 문제이고 이는 기후변화, 이상기온, 폭우, 가뭄 등의 문제를 초래한다. 특히 가뭄은 기후변화에 의해 여러 해 동안 진행되어온 사막화를 가속화시킨다. 본 연구의 목적은 중국과 몽골 사막주변의 식생수분상태를 탐지하는 것이다. 본 연구에서는 중국과 몽골 사막 주변의 식생수분지수를 산출하기 위해 1999년부터 2006년까지의 SPOT/VEGETATION 위성 이미지를 이용하여 정규수분지수(NDWI: Normalized Difference Water Index)를 산출하였다. 건조한 상태의 식생은 사막화되기 쉽기 때문에 식생 수분은 사막화의 중요한 지표이다. SPOT/VEGETATION 위성영상의 근적외밴드(NIR)와 단파적외밴드(SWIR)의 밴드간 연산을 통하여 NDWI를 구하여 식생의 수분입자를 측정하였다. 그 결과 1999년부터 2006년까지의 NDWI는 사막주변영역에서 감소하는 경향을 보였고, 그 영역은 몽골 고비사막 북동지역과 중국 타클라마칸 사막의 남동지역에 위치해 있었다.

• 한국작물학회지
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• 제67권3호
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• pp.147-154
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• 2022

본 연구는 사막기후에서 벼 재배시 관개방법 및 관개량에 따른 벼의 생육 및 수량 특성을 알아봄으로써 적정 관개량 선정 및 사막기후환경에서 벼 관개시설 재배에 대한 기초자료로 활용하고자 수행한 결과는 다음과 같다. 관개방법별 총 관개량에서는 스프링클러 > 지표점적 > 지중점적 순서로 관개량이 많았고, 지중점적 FC80% 처리구에서 627 ton/10a로 관개량이 가장 적었으며, 관개량이 가장 많았던 스프링클러 FC120% 처리구 1,584 ton/10a 대비 60.4% 더 적은 것으로 조사되었다. 관개방법에 따른 쌀 수량에서는 지중점적 > 지표점적 > 스프링클러 순이였으며, 그 중 지중점적 FC120% 처리구에서 665 kg/10a로 관행구 대비 88.1%로 관수방법에서 가장 높은 수량성을 보였다. 따라서, 사막기후환경에서 벼 재배시 지중점적관개로 FC120% 처리 할 경우 물의 이용효율을 높이면서, 작물 수량증대에 유리할 것으로 사료된다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2008년도 학술발표회 논문집
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• pp.1438-1441
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• 2008

Throughout the history, the people of Iran have battled the dryness by innovations to preserve every drop of water that lands from the rare clouds, or from a stream flowing out of distant springs. Water is precious and held with highest respect, whether stored for drinking at an Ab-Anbar, or for washing and farming at the Houz in the middle of their oasis homes and orchards, or sourced at a Qanat spring or Jooy under ground. How it is that drinking water as cold as a mountain fall is found in desert of Iran? Ab-Anbar is an ancient means of water preservation and cooling through anunderground building structure. These underground structures have been present in Khorasan and other desert provinces of Iran as public or private water storage facilities, widely used before the installation of public plumbing systems in the late 1950s. Although many of these structures are still functional, most have been protected by government for restoration or viewing by the public as historical heritage. Khorasan natural dry climate and the massive surrounding deserts have been a breeding ground for many designs of Ab-Anbars. Today the existing number of such facilities stands in the province of Khorasan. Usually these structures were built in populated areas, also there are some forms of such structures on old trade routes and roadways leading to and from populated towns. This paper considers the history of Ab-Anbars in Khorasan as well as other relevant aspects such as types, components, construction methods and materials, filling and withdrawal systems.

• 대한원격탐사학회지
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• 제34권6_1호
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• pp.869-877
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• 2018

사막면적은 매년 증가하는 추세이며, 이에 따라 막대한 사회적 피해 비용을 발생시키고 있다. 이러한 사막은 광범위하게 분포하고 사람의 접근이 어려워 인공위성을 이용한 모니터링이 많이 이루어지고 있지만 인공위성의 센서에 따라 산출되는 사막 면적 비교 연구는 미비한 편이다. 센서의 선택에 따라 산출되는 사막 면적은 상이할 수 있고 이에 따라 기후 예측이나 사막화 방지대책 등에 영향을 미칠 수 있어 센서별로 산출되는 사막면적 자료의 특성을 인지하는 것은 중요하다. 본 연구에서는 Moderate Resolution Imaging Spectroradiometer(MODIS)와 Vegetation을 이용해 2001-2013년 동북아시아 지역의 사막 면적을 산출하고 비교 분석하였다. 분석결과, MODIS에서 산출한 사막 면적은 비교적 과소 탐지하는 경향과 $20,911km^2/year$로 감소하는 추세를 보였고 Vegetation에서 산출한 사막 면적은 $3,020km^2/year$로 증가하는 추세를 보였다. 또한 실측자료 확보가 힘든 사막지역에서 인공위성을 이용해 산출된 사막 면적의 간접검증을 위해 사막 면적 변화에 영향을 받는 황사 발생빈도와 상관관계 분석을 실시하였다. 그 결과, MODIS는 R=0.2071로 비교적 낮은 상관관계가 나타났고 Vegetation은 R=0.4837로 비교적 높은 상관관계가 나타났다. 이는 Vegetation이 동북아시아 사막 영역에서 보다 정확한 사막 면적 산출을 수행한 것으로 사료된다.