• 한국토양비료학회지
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• 제30권4호
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• pp.351-356
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• 1997

시설(施設) 참외는 이른 봄부터 가을까지 계속(繼續) 재배(栽培)하여 높은 소득(所得)을 올릴 수 있으나 뿌리혹선충(線蟲) 발생등(發生等) 연작(連作) 장해(障害)로 인(因)하여 계속(繼續) 재배(栽培)가 불가능(不可能)하여 그 원인(原人)과 효과적(效果的)인 토양토양관리(土壤土壤管理) 방법(方法)을 연구(硏究) 조사(調査)하기 위(爲)하여 참외연작지(連作地)의 시비량조사(施肥量調査), 토양분석(土壤分析), 객토실시(客土實施) 효과(效果) 및 참외 수확(收穫) 후(後)의 토양관리(土壤管理) 방법(方法)에 따른 효과(效果)를 분석(分析)한 결과(結果)를 요약(要約)하면 다음과 같다. 참외 연작장해(連作障害)는 3, 4년(年) 이상(以上) 연작시(連作時) 심해지며 장해(障害) 요인(要因)으로 염농도(鹽濃度) (EC)는 2.50 dS/m 이상(以上)에서 연장 재배가 불가능하였으며 연작장해(連作障害) 대책(對策)으로 실시(實施)하는 객토(客土)는 10a당(堂) 500 M/T를 넣고 토양시비(土壤施肥) 관리(管理)는 볏짚은 30%, 3요소(尿素)는 10% 정도(程度) 더주었을때 효과적(效果的)이었으며 그때 상품과(商品果) 및 당도(糖度)는 적어도 2년(年) 동안 각각(各各) 10%, $2.6^{\circ}$(Brix)증가 하였다. 참외 수확후(收穫後) 토양관리(土壤管理)는 참외를 6월하순(月下旬)에 수확(收穫)한 후(後) 벼재배(栽培) 하는 것이 연작(連作) 장해(障害)를 막는 방법(方法)으로 가장 좋았다. 부득이한 경우(境遇) 참외를 7-8월에 수확(收穫)한 후(後) 고온기(高溫期)에 40일간(日間) 담수(湛水) 태양열(太陽熱) 처리(處理)하거나 참외를 9-10월에 수확(收穫)한 후(後) 포크레인으로 심토(心土) 50cm이상(以上)까지 반전(反轉)하면 효과(效果)가 있었다.

• 암석학회지
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• 제17권1호
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• pp.44-50
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• 2008

대전지역에 날아온 황사의 근원지를 규명하기 위해 희토류원소 지구화학적 연구방법을 적용하였다. 대전지역 황사의 채집은 2007년 3월 31일에서 4월 2일 그리고 5월 25일에서 5월 27일 사이와 같이 총 2회에 걸쳐 수집되었다. 그리고 비교를 위해 한국지질자원연구원 주변의 토양을 채취하였다. 연구결과, 대전 지역 황사먼지의 경희토류(La-Gd) 분포도는 편평한 양상을 갖고 있고 Gd을 기점으로 중희토류(Gd-Lu)는 결핍되어 있으며 Eu의 이상은 관찰되지 않는다. 토양시료의 경우 경희토류의 경우 약간 부화된 경향을 보여주고, 중희토류의 분포도가 현저하게 결핍되어 있으며, Eu의 약한 부(-)의 이상을 보여준다. 이와 같이 대전지역 토양시료와 다른 양상을 갖는 대전 지역 황사먼지의 희토류원소 분포도의 특성은 중국의 오도스 사막 남동부의 풍성퇴적물과 매우 유사하다. 초기연구결과를 토대로 볼 때, 대전지역 황사의 주 근원지는 중국의 오도스 사막 남동부일 가능성이 매우 높은 것으로 나타났다.

• 한국토양비료학회지
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• 제6권1호
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• pp.35-52
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• 1973

우리나라 전작물(田作物)의 저위생산성의 원인(原因)과 그 대책(對策)을 토양학적(土壤學的)인 면(面)에서 추궁(追窮)함에 있어 우선(于先) 현재경작(現在耕作)이 많이 되여 있고 또 앞으로 개발(開發)의 가능성(可能性)을 가진 저구릉(低丘陵), 산록(山麓) 및 대지(臺地)의 적황색토(赤黃色土)에 대(對)하여 현재(現在)까지 밝혀진 조사(調査) 결과(結果)를 종합(綜合)하였으며 그 결과(結果)를 요약(要約)하면 다음과 같다. 1. 적황색토(赤黃色土)는 우리나라 남부(南部)를 비롯하여 중부이북(中部以北)의 저구릉(低丘陵), 산록(山麓) 및 대지(臺地)에 분포(分布)하고 있으며 화강암(花崗岩), 화강편마암(花崗片麻岩)을 비롯한 석회암(石灰岩), 혈암(頁岩) 그리고 홍적층(洪積層) 등(等)을 모재(母材)로 하고 있다. 2. 적황색토(赤黃色土)는 A, Bt, C층(層)으로 되여 있다. A층(層)은 유기물(有機物)이 엷게 덮여서 암색(暗色)을 띄우는 양질(壤質), 식양질(埴壤質)이며 Bt층(層)은 진갈색(眞褐色), 적갈색(赤褐色), 황적색(黃赤色)의 식질(埴質) 혹은 식양질(埴壤質)로서 토괴표면(土塊表面)에 점토피막(粘土皮膜)이 형성(形成)되여 있다. C층(層)은 모재(母材)에 따라 다양다색(多樣多色)하며 Bt층(層)에 비(比)하여 토성(土性)이 거칠고 토양구조(土壤構造)의 발달(發達)이 없다. 토양(土壤)의 깊이는 지형(地形) 모재(母材)에 따라 다르나 대부분(大部分)이 100cm 이내(內外)이다. 3. 적황색토(赤黃色土)의 물리적성질(物理的性質)에 있어 점토함량(粘土含量)은 표토(表土)에서 18~35% 심토(心土)에서 30~90%로서 심토(心土)의 점토함량(粘土含量)은 표토(表土)에 비(比)하여 약(約) 2배(倍) 내외(內外)가 된다. 가비중(假比重)은 표토(表土)에서 1.2~1.3심토(心土)에서 1.3~1.5 그리고 삼상(三相)의 분포(分布)는 표토(表土)에서 고상(固相) 45~50 액상(液相) 30~45, 기상(氣相) 5~25, 심토(心土)에서 고상(固相) 50~60, 액상(液相) 35~45, 기상(氣相) 15미만(未滿)으로 대부분(大部分)이 치밀(緻密)하다, 유효수분범위(有効水分範圍)는 비교적(比較的) 좁아서 표토(表土)에서 10~23%, 심토(心土)에서 5~16% 범위(範圍)이다. 4. 적황색토(赤黃色土)의 화학적성질(化學的性質)에 있어 토양반응(土壤反應)은 모재(母材)에 따라 달라서 석회암(石灰岩) 및 구하해혼성퇴적(舊河海混成堆積)을 모재(母材)로한 토양(土壤)에서는 중성(中性) 급지(及至) 염기성(鹽基性) 그밖의 토양(土壤)에서는 산성(酸性) 급지(及至) 강산성(强酸性)을 띠운다. 표상(表上)의 유기물함량(有機物含量)은 식생(植生), 침식(侵蝕), 경종(耕種) 등(等)에 따라서 차(差)가 크며 1.0~5.0% 범위(範圍)에 있다. 염기치환용량(鹽基置換容量)은 5~40me/100gr이며 이는 유기물(有機物), 점토(粘土), 미사함량(微砂含量) 등(等)과 밀접(密接)한 관계(關係)를 가지고 있다. 치환침출염기(置換浸出鹽基)는 용탈(溶脫)되여서 염기포화도(鹽基飽和度)가 대체(大體)로 낮지만 석회암(石灰岩)에 기인(基因)된 토양(土壤)에서는 석회(石灰), 마구네슘함량(含量)이 높아서 염기포화도(鹽基飽和度)도 높다. 5. 적황색토(赤黃色土)의 점토광물(粘土鑛物)은 대부분(大部分)이 Kaolin 광물중(鑛物中)의 하나인 Halloysite와 운모(雲母)의 풍화생성물(風化生成物)인 Vermiculite, Illite를 주광물(主鑛物)로 하고 있으며 소량(少量)의 Chlorite, Gibbisite, Hematite 혼층광물(混層鑛物)과 1차(次) 광물(鑛物)인 석영(石英) 및 장석(長石)이 존재(存在)한다. 6. 적황색토(赤黃色土)는 미국(美國)의 Red-yellow podzolic Soils 및 Reddish Brown Lateritic Soils의 일부(一部) 그리고 일본(日本)의 적황색토(赤黃色土)와 유사(類似)한 특성(特性)을 가진다. 미(美)7차(次) 시안(試案)에 의(依)하면 적황색토(赤黃色土)는 Udults 및 Udalfs 그리고 FAO 분류안(分類案)에 의(依)하면 Acrisols, Luvisols 그리고 Nitosols로 분류(分類)할 수 있다.

• 한국대기환경학회지
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• 제1권1호
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• pp.71-82
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• 1985

The effect on the particulate matters in the atmosphere was investigated in Seoul area from March, 1984 to Aprill, 1985. Aerosols were collected by filters on nine stages Andrsen Air Sampler, and size distribution and total concentration of the aerosols, Fe and Pb were measured. In spring with Yellow Sand the concentration of particles in aerosols was 185.55$\mug/m^3$ and CP/TA was 65.9%. But in spring without Yellow Sand those of particles was 135.45$\mug/m^3$ and CP/TA was 58.6%. Accordingly the concentration of coarse particles with Yellow Sand was higher than without them in Spring. Above results indicate that in Seoul Area the main source of air pollution originated from natural burdens, especially from soil. The concentration of Pb was similarly valued through both seasons in Seoul area but fine particles valued above coarse particles. On the other hand, in urban area, the natural and anthropogenic sources have influenced on the concentration of Pb. With referred to particle size distribution for Fe, the concentration of coarse particles was 0.168$\etag/m^3$ (CP/TA: 74.3%) in Spring with Yellow Sand, 0.096$\mug/m^3$ (CP/TA: 71.6%) without Yellow Sand and 0.083$\mug/m^3$ (CP/TA: 67.4%) in winter, respectively. Compared with fine particles, all of them were higher. It indicated that the origin of coarse particles in urban air was not related to anthropogenic source. The concentration of Fe was influenced by Yellow Sand and contributed to air pollution.

• 한국환경과학회지
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• 제12권2호
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• pp.133-137
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• 2003

The Yellow River delta is an important region where coastal and newly formed wetlands distribute in north China. Based on satellite remote sensing images and GIS techniques, this paper tends to delineate the dynamic changes of newly formed wetland in the Yellow River mouth from 1986.5 to 1996.10. Our results show that the newly formed wetland increased by 24.9 $\textrm{km}^2$ per year. Before 1990. 1 and it decreased by 2.40 $\textrm{km}^2$ per year after that. The northern and southwestern parts of the Yellow River mouth are main positions of decrease and the southern and the estuary parts are main positions of increase. The advancing rate of river mouth extending into the Bo Sea is decreasing obviously. The reason for that is the decreasing of water and sediments in the Yellow River, which caused by the increasing use of water and soil conservation on upper reach.

• 한국자원식물학회:학술대회논문집
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• 한국자원식물학회 2002년도 제9차 국제심포지움 및 추계정기학술발표회
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• pp.70-70
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• 2002

Two new species of Amanita were collected in central areas of Korea from 1997 to 2000. They were identified, described and illustrated. One of them, Amanita longstipeta has turtle-shaped warts of crust and its base is longer under the soil than is above the soil. The other A. aureofarinosa is covered with golden yellow farina and annulus is absent. Both are solitary in soil with sand.

• 대한지리학회지
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• 제32권
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• pp.1-10
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• 1985

• 한국환경복원기술학회지
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• 제18권5호
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• pp.37-48
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• 2015

Soil nutrient management is important to maintain the constant productivity of seedling production in the nursery for successful forest restoration. This study investigated the effects of organic manure and chemical fertilizer application levels on the growth, soil properties, and nutrient concentrations of yellow poplar seedlings. One-year-old yellow poplar seedlings were treated with the combination of 3 level organic manures(0, 5 Mg/ha, 10 Mg/ha; mixture of poultry manure, cattle manure, swine manure, and sawdust) and 3 level nitrogen-phosphorus-potassium(NPK) chemical fertilizers(0, 1x(urea, $30g/m^2$; fused superphosphate, $70g/m^2$; potassium chloride, $15g/m^2$), 2x). Organic manure significantly increased the soil pH and the concentrations of nitrogen, available phosphorous, exchangeable potassium, calcium, and magnesium. In contrast, the NPK chemical fertilizer decreased the soil pH and exchangeable calcium concentration, did not affect the soil concentrations of nitrogen and magnesium, and increased the concentrations of available phosphorous and exchangeable potassium. Both organic manure and NPK chemical fertilizer treatments increased the seedling height, root collar diameter, and dry weight by 39% and 25%, respectively. The treatment with manure 5 Mg/ha and NPK 2x chemical fertilizer mostly increased seedling dry weight by 2.6 times more than that of the control. Compared to the effects of the fertilization treatments on the soil properties, the effects on nutrient concentrations in the leaves were relatively small. These findings indicate that organic manure that was derived from livestock byproducts and sawdust can be utilized with chemical fertilizer to improve seedling production as well as conserving soil quality.

• 한국작물학회지
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• 제53권4호
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• pp.427-433
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• 2008

Barley Yellow Mosaic Virus (BaYMV) caused significant reduction in barley yield and is difficult to control due to alive parasitic soil-borne fungus, Palmyra gamines that transmits the, virus. Previous studies have indicated that a virus-free soil could be infested by using virus-contaminated farming machineneries and implements. For the further confirmation of this finding, different proportions of BaYMV-infested soil were mixed into virus free soil. Three barley varieties (Hordum vulgarae, cv "Olbori", "Baegdong" and "Sacheon 6") were sown in pots treated with different rate of P. graminis-infested soil ranging from 0% to 100% in October 20, 2001. Results showed that BaYMV infection increased as the rate of infested soil increased. Initial symptoms were observed in a pots treated with 10% infested soil in all the 3 varieties of barley. "Olbori" had about 5% infection in 20% infested soil and about 10% infection in 40% or 50% infested soil and about 20% infection in 60% infested soil. In "Baegdong", the trend of BYMV occurrence was similar with "Olbori" but the time of severe infection was earlier than "Olbori". BaYMV infection in "Sacheon 6" was even earlier than "Baegdong" with much more severe symptoms than "Baegdong". The growth rate of barley was affected by about 19-22% when grown in 20% infested soil. As the rate of BaYMV infested soil increased the heading date was delayed but the maturing date was early in "Olbori" and "Sacheon 6". Also, reduction rate of culm length in 3 varieties increased with increase of infested soil content. However, "Olbori" showed the highest reduction. "Sacheon 6", have been characterized with long spike length, however was significantly reduced as the infested soil increased. On the other hand, spike length of "Olbori" was not significantly affected despite of increased of infested soil. The reduction rate of 1000 kernel weight was higher in large kernel size cultivar "Sacheon 6" and "Olbori" than small kernel size "Baegdong" as increase of BaYMV-infested soil content.

• Geomechanics and Engineering
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• 제32권6호
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• pp.601-613
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• 2023

Low liquid limit silt, widely distributed in the middle and down reaches of Yellow River, has the disadvantages of poor grading, less clay content and poor colloidal activity. It is very easy to cause vehicle jumping at the bridge-embankment transition section when the low liquid limit silt used as the backfill at the abutment back. In this paper, a series of laboratory tests were carried out to study the physical and mechanical properties of the low liquid limit silt used as back filling. Ground granulated blast furnace slag (GGBFS) was excited by active MgO and hydrated lime to solidify silt as abutment backfill. The optimum ratio of firming agent and the compaction and mechanical properties of reinforced soil were revealed through compaction test and unconfined compressive strength (UCS) test. Scanning electron microscope (SEM) test was used to study the pore characteristics and hydration products of reinforced soil. 6% hydrated lime and alkali activated slag were used to solidify silt and fill the model of subgrade respectively. The pavement settlement regulation and soil internal stress-strain regulation of subgrade with different materials under uniformly distributed load were studied by model experiment. The effect of alkali activated slag curing agent on curing silt was verified. The research results can provide technical support for highway construction in silt area of the Yellow River alluvial plain.