• Title/Summary/Keyword: yellowish brown

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Two New Euryspongian Sponges (Dictyoceratida: Dysideidae) from Korea

  • Lee, Kyung-Jin;Sim, Chung-Ja
    • Animal Systematics, Evolution and Diversity
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    • v.23 no.1
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    • pp.35-38
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    • 2007
  • Two new sponges, Euryspongia coreana n, sp, and E. regularis n, sp., collected from Hataedo, Ulleungdo and Chujado, Korea by SCUBA diving during the period from 2001 to 2005. Euryspongia coreana n. sp, is very close to E. lactea Row, 1911 and E. arenaria Bergquist, 1961 in skeletal structure, but primary and secondary fibres of the new species are thicker than those of E. lactea, E. arenaria is cored with mostly spicule fragments but E. coreana n. sp. is cored with mainly sand. E. regularis n. sp. is readily distinguished from other eurypsongian sponges. by its thickly encrusting growth form, yellowish ivory colour, and thickness of fibres. The bright yellow color and regular ladder-like skeletal structure are major features distinguishing this E. regularis n. sp. from other euryspongian sponges. Most species are brown, violet, red or orange in color except for E. lactea (milky white), E. arenaria (biscuit) and E. coreana n. sp. (yellowish ivory). Other euryspongian sponges have regularly or irregularly well developed secondary fibres, but E. regularis n. sp. has simple and regular secondary fibres.

Growth and Tield Performance of Selected Forage Crops Cultivated on Imperfectly Drained Paddy Field under Subsurface Drainage by PVC Pipes (배수 약간 불량지 논에서 PVC 파이프 암거배수에 의한 사료작물 재배)

  • 김정갑;박근제;김건엽;한민수
    • Journal of The Korean Society of Grassland and Forage Science
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    • v.16 no.3
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    • pp.219-224
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    • 1996
  • Silage comkv, suwwn 19). sorghum $\times$ sudangrass(p. 988) and winter ryeNaton) were cultivated on imperfectly drained paddy field under two different draining methods, subsurface darinage by PVC pipes and open ditsched surface drainage. The crops were harvested at the stage of hard dough for corn and soft dough for wrghum and rye. The soil physical properties. soil colors. soil structure and soil wetness were improved in the subsurface drainage. Gravitational water table occured depth in 110 cm(dry season)~75cm(rain season). In soil profile description, yellowish brown with yellowish red mottles and well developed granular structure were found in the surface A horizon. The portion of solid phase in subsoils(B horizon) was reduced from 48.6%(undrained) to 43.7 %. A blocky structure with dark gray to gray were described in the open ditsched surface drainage. Severe wet depression of the crops was observed due to it's higher moisture contents, where the gravitational water occured depth in 25~37cm during the rainy season. The chemical properties of paddy soils were less affected by drainage methods. The concentration of available phosphate. organic matter and exchangeable K, Ca and Mg were decreased in the subsurface drained soils. The annual dry matter yields of com-rye cropping were 17.8 ton in the undrained, 21.6 ton in the open ditsch drainage and 35.9 ton/ha in the subsurface drainage.

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Notes on the Endothia Canker of Carpinus laxiflora and its Pathogenic Fungus, Endothia fluens Schw Shear et Stevens (서-나무 위축병(萎縮病)과 그 병원균(病原菌))

  • Kim, Kichung
    • Journal of Korean Society of Forest Science
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    • v.6 no.1
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    • pp.6-10
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    • 1967
  • In the present paper author investigated the symptom, pathogenic fungus and pathogenicity of Endothia canker of Carpinus laxiflora in Korea, and made clear the indistinct discription on its pathogen in the past. 1. The pathogen is identified as Endothia fluens (Schw.) Shear et Stevens. The discription is recorded as follows: Stromata cortical, erumpent, spherical or conical, outer yellowish-brown and inner yellowish, 0.5 to 2.5 mm in diameter; perithecia irregularly embeded in the bottom of stroma, 7 to 23 in a stroma usually spherical to elliptical or irregular, 235 to $370{\mu}$ in diameter, with black slender necks; each neck open the papilliate ostiole to the surface, about 250 to $400{\mu}$ in length; asci clavate or fusoid, colorless, 31.16 to 42.64 by 6.54 to $8.20{\mu}$ in size, average 37.02 by $6.84{\mu}$, with 8 ascospores in double line; ascospores elliptical, ovate or cylindrical, with rounded ends, hyaline, 1-septate, not constrict at the septum, 6.51 to 9.30 by 3.16 to $3.72{\mu}$, average 7.61 by $3.44{\mu}$ in size; pycnidia formed abundantly in stroma. spherical at first but later irregular large cavity by fussing each other; pycnospores oblong or rod-shaped, hyaline, non-septate, 3.8 by $1.9{\mu}$ in size; spore-horn formed abundantly under moist condition. 2. The pathogen is wound parasite invading the hosts through the wound. But after the infection is established, expanding the disease lesion is swiftly vigorus.

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A Study on the Making Properties of Natural Pigments based on Substance Characteristics for Hwangto in Korea (국내 산출되는 황토의 특징에 따른 천연(제조)안료 특성연구)

  • Mun, Seong Woo;Kang, Yeong Seok;Park, Ju Hyun;Han, Min Su;Jeong, Hye Young
    • Journal of Conservation Science
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    • v.35 no.6
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    • pp.600-611
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    • 2019
  • Yellow to reddish brown soil is generally referred to as hwangto and is used in various industries in Korea. Despite the fact that it is used as an inorganic pigment in dancheong, limited studies have been conducted on the properties of pigments associated with soil and on the mineralogical characteristics of hwangto. This study examines how the pedological and mineralogical features of hwangto affect pigment properties. Results indicate that reddish and yellowish soils have differences in terms of soil texture, mineral composition, oil absorption and stability under light. Reddish soil is mostly found in clay regions, whereas Ulleungdo hwangto is found in loam regions. Yellowish soil is mostly present in the clay loam to loam zones. whereas Haenam hwangto exists in the sandy clay loam zone. As a result of a mineralogical analysis, reddish soil is classified into the feldspar group and clay soil. The major minerals in the yellowish soils are similar however these soils differ in terms of clay mineral compositions. results of the characteristics of pigments prepared by the traditional method revealed that the average particle size is in the range of 10-20 ㎛, reddish soil has an average of 20 ml/100 g higher oil absorption than yellowish soil. In addition, reddish soil is more susceptible to discoloration and deterioration under light than yellowish soil. This study confirms that the soil and mineral characteristics of hwangto affect the physical properties and stability of produced pigments. These result can be used as basic data in future studies natural inorganic pigments using hwangto.

A Study on Morphological and Pattern Analysis in 2 kinds of Paeoniae Radix (2종(種) 작약류(芍藥類)의 내외부형태(內外部形態)와 패턴분석 연구(硏究))

  • Song, Kyoung-Song;Choi, Go-Ya;Kim, Hong-Jun;Ju, Young-Sung
    • Korean Journal of Oriental Medicine
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    • v.11 no.2
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    • pp.141-154
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    • 2005
  • The following is a taxonomic list of the specific features of external and internal shape and pattern analysis of Paeonia lactiflora PALL. and P. obovata MAX as the standard of herbal medicine. 1. External shape of original plant P. lactiflora has lancelate and elliptical leaves with no hair on both sides. It bears a flower bud at the shoot apex or leaf axil. On the other hand, P. obovata has obovate leaves with hair on the back side. It has a single flower bud at the shoot apex. 2. Physical characteristics of herbal states P. lactiflora has a bright and smooth external surface whose color is light red brown, light gray on its section and it is not easy to cut. On the other hand, P. obovata has a coarse external surface whose color is dark brown, pinkish on its section and it is easy to cut. 3. Physical characteristics of herbal state in currents Paeonia Radix Alba is brown on the external surface, and whitish on its section. On the other hand, Paeonia Radix Rubra is dark brown on the external surface, and yellowish-white on its section. 4. Internal characteristics Internal shape is correspond to that of Paeonia Radix described in literatures. Only P. lactoflora has a concentrated vascular bundle toward centeral cylinder. On the other hand, P. obovata has a scattered vascular bundle at the cortex. 5. Physicochemical pattern by HPLC Both P. lactoflora and P. obovata showed the same pattern. Paeoniforin, a main component, appears upon 13.68 in retention time (Rt) in both. In addition, both contain a large amount of paeoniflorin. Such results will, in the future, be used as basic source for the additional research, such as biological reactions and genetic discrimination.

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Occurrence of Blossom Blight of Petunia Caused by Choanephora cucurbitarum in korea (Choanephora cucurbitarum에 의한 페튜니아 꽃썩음병)

  • 권진혁;강수웅;김정수;박창석
    • Research in Plant Disease
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    • v.7 no.2
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    • pp.112-115
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    • 2001
  • Blossom blight of petunia caused by Choanephora cucurbitarum was found in greenhouses around Jinju area, Gyeongnam province, Korea in April 2001. The disease started with water-soaked lesions on the flower which rapidly withered and was rotten. Calyces developed water-soaked, dark-green lesions, and then were rotten. Whitish mycelia and monosporous sporangiola were produced on the lesions. The fungus isolated from the lesions produced white to pale yellowish brown mycelia with scattered monosporous sporangiola on potato-dextrose agar (PDA) plates. Size of sporangium was 37.2~135.8 um. Monosporous sporangiola were elliptic, fusiform or ovoid, and brown in color and their size was 10.4~22.4$\times$7.4~12.9 um. Sporangiospores were elliptic, fusiform or ovoid in shape, dark brown or brown in color and were 13.7~23.5$\times$8.7~13.8 um in size, and had appendaged appressorium of 3 or more. Zygospores were black, and 40.8~61.5 um in size. The fungus grew on PDA at 15-4$0^{\circ}C$, and optimum temperature was 3$0^{\circ}C$. This is the first report on the blossom blight of petunia caused by C. cucurbitarum in Korea.

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Identification and Characterization of Eurotium rubrum Isolated from Mejuin Korea

  • Yun, Yeo-Hong;Hyun, Min-Woo;Suh, Dong-Yeon;Kim, Yong-Min;Kim, Seong-Hwan
    • Mycobiology
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    • v.37 no.4
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    • pp.251-257
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    • 2009
  • We isolated and identified a strain of Eurotium rubrum from Meju that has not been reported in Korea. This fungus is yellowish brown; reverse dark brown on CYA and PDA while yellow on 2% MEA at $25{^{\circ}C}$. Cleistothecia are first bright yellow and gradually turned brown. Mycerial growth on CYA attained a diameter of 30 mm at $20{^{\circ}C}$, 37 mm at $25{^{\circ}C}$ and 32 mm at $30{^{\circ}C}$ after 15 days. The isolate grew slower on 2% MEA ($<$ 20 mm 15 days at $25{^{\circ}C}$) compared to CYA and PDA ($<$ 40 mm 15 days at $25{^{\circ}C}$). Cleistothecia are superficial, yellow to light brown, globose to subglobose, 40~75 ${\mu}m$ in diameter. Asci are 8-spored and globose to subglobose 8~11 ${\mu}m$. Ascospores are disciform, 4.0~5.0 ${\mu}m$ in length and 4.2~4.5 ${\mu}m$ in width. Conidia are ovate or bacillar, finely roughened to densely spinulose, 4.6~6.0 ${\mu}m$ in length and 3.0~4.3 ${\mu}m$ in width. Compared to known Eurotium rubrum, the Korean isolate showed 99% sequence similarity in ITS rDNA (554 bp) and calmodulin (750 bp) gene and 100% in $\beta$-tubulin (1016 bp) gene. The E. rubrum isolate also had weak $\beta$-glucosidase and protease activities.

Characteristics of the Dalseong Acid Mine Drainage and the Role of Schwertmannite (달성폐광산 산성광산배수의 발달특징과 슈베르트마나이트의 역할)

  • Choo, Chang-Oh;Jeong, Gyo-Cheol;Lee, Jin-Kook
    • The Journal of Engineering Geology
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    • v.17 no.2 s.52
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    • pp.187-196
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    • 2007
  • The Dalseong acid mine drainage were studied focused on the characters of schwertmannite that controls geochemistry of the stream. Besides chemical analysis of stream water, particle size analysis, XRD SEM and TEM were performed on precipitates of streams and on wasted metalliferous ores. The AMD discharged from the abandoned mine reveals a decrease of pH and EC downward stream. Euhedral sulfur occurs as equigranular aggregates on the altered pyrite while fine acicula goethite coalesces to form cross, star, or starfish-like shapes. Water chemistry plotted on the Eh-pH diagram shows that schwertmannite and ferrihydrite are stable phases. Reddish brown precipitates consist of mostly schwertmannite with less goethite, whereas yellowish brown precipitates are composed of geothite with less schwertmannite. The particle size of precipitates ranges $d(0.1)\;0.861{\mu}m{\sim}3.769{\mu}m,\;d(0.5)\;3.984{\mu}m{\sim}15.255{\mu}m,\;and\;d(0.9)\;9.875{\mu}m{\sim}56.726{\mu}m$. Schwertmannite is characterized by equigranular spheric form. Pincushion or spicule with 100nm width and $200{\sim}300nm$length form on schwertmannite sphere with radial growth patterns. It is highly probable that reddish or yellowish brown precipitates formed in many AMDs may contain schwerhnannite. Because it can serve as sink for removing heavy elements by adsorption in AMD system, there is a need to correctly identify schwertmannite in precipitates and to characterize its phase stability.

A Study on Functionality of the Ulreungdo Seokganju as Korean Traditional Red Pigment (한국 전통 적색광물안료 울릉도석간주의 기능성 연구)

  • Do, Jin-Young;Kim, Soo-Jin;Lee, Sang-Jin;Ahn, Byung-Chan;Yun, Seong-Chul;Kim, Kwang-Jong
    • Journal of the Mineralogical Society of Korea
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    • v.22 no.2
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    • pp.153-162
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    • 2009
  • The main compositions of "Seokganju", a Korean traditional red mineral pigment, are iron oxides. To investigate its mineralogical and functional properties, we had got its ore from Juto cave in Ulreoung island, which was a famous field of it in Korean documents. The ore occurs as a paleosol between the olivine basalt and amphibole trachyte in discontinuously. It is reddish brown and yellowish brown and consists mainly of clay minerals with minor debris. Its reddish and yellowish brown color are due to the hematite and ferrihydrate, respectively. These iron oxides are precipitated as ferrihydrate from the ferrous water in the paleosol and partly changed to hematite. The color reproduced in timber by using seokganju pigment with traditional tools and methods is similar to that in heritage building. The moistureproofing and fire resistance of Ulreungdo seokganju is far better than that of artificial seokganju. Moreover, the combustion tests show that the artificial seokganju promote the ignition and combustion of the timber. Ulreungdo seokganju is regarded as a pigment with fungicidal efficacy because growth of two wood decay fungi (cov. and typ.) are inhibited in solid medium with it.

Petrological and Geological Safety Diagnosis of Multi-storied Stone Pagoda in the Daewonsa Temple, Sancheong, Korea (대원사 다층석탑의 지질학적 및 암석학적 안전진단)

  • 이찬희;서만철
    • Economic and Environmental Geology
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    • v.35 no.4
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    • pp.355-368
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    • 2002
  • The multi-storied Daewonsa stone pagoda (Treasure No. 1112) in the Sancheong, Korea was studied on the basis of deterioration and geological safety diagnosis. The stone pagoda is composed mainly of granitic gneiss, partly fine-grained granitic gneiss, leucocratic gneiss, biotite granite and ceramics. Each rock of the pagoda is highly exfoliated and fractured along the edges. Some fractures in the main body and roof stones are treated by cement mortar. This pagoda is strongly covered with yellowish to reddish brown tarnish due to the amorphous precipitates of iron hydroxides. Dark grey crust by manganese hydroxides occur Partly, and some Part coated with white grey gypsum and calcite aggregates from the reaction of cement mortar and rain. As the main body, roof and upper part of the pagoda, the rocks are developed into the radial and linear cracks. Surface of this pagoda shows partly yellowish brown, blue and green patchs because of contamination by algae, lichen, moss and bracken. Besides, wall-rocks of the Daewonsa temple and rock aggregates in the Daewonsa valley are changed reddish brown color with the same as those of the pagoda color. It suggests that the rocks around the Daewonsa temple are highly in iron and manganese concentrations compared with the normal granitic gneiss which color change is natural phenomena owing to the oxidation reaction by rain or surface water with rocks. Therefore, for the attenuation of secondary contamination, whitening and reddishness, the possible conservation treatments are needed. Consisting rocks of the pagoda would be epoxy to reinforce the fracture systems for the structural stability on the basements.