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光波長이 오이(Cucumis sativus L.) 플러그苗의 生長에 미치는 影響
용영록,전지영,황세진,김일섭,정천순 강릉대학교 동해안지역연구소 2000 東海岸硏究 Vol.11 No.1
This research was carried to find out the optimum artificial light condition for plug seedling production of high quality cucumber through investigating growth response of the seedling by both light wave length and treatment period. The treatment with blue and red fluorescent lamp increased the fresh weight involving hypocotyl and root and controlled the elongation of hypocotyl, compared with other treatments. The 30-day-old seedling treatment with blue and red light for 12 hours showed that vegetative growth including root, stem and leaves was better than that of seedling treated with other lamps. Seedling under blue and red light for 12 hours grew 60.0mm and 0.55g in length and weight of hypocotyl. respectively, Hypocotyl length and weight were 44.9mm and 0.62g when seedling was grown under above light condition for 6 hours. Total chlorophyll contents of hypocotyl were highest in the light mixing treatment, and this accelerated greening. Morphological characteristics by investigating cross and longitudinal section of 30-day-old cucumber seedling treated with the mixing fluorescent lamps indicated that epidrmis tissues were usually single layer and thicker, resulting in small, compact and non-intercellular spaces of cells. On the other hand, epidermis tissues of the control composed of large, longer and round cells and cortex tissues showed large intercellular spaces between cells. Longitudinal section of photo-treated hypocotyl showed that there were more shorter cells and non-intercellular spaces of cells than untreated tissues. As a result, blue and red light mixing treatment controled the cell elongation of seedling hypocotyl, resulting in shortening hypocotyl of cucumber seedling.
Kim, Rog-Young,Yang, Jae E. 한국토양비료학회 2014 한국토양비료학회지 Vol.47 No.1
Agricultural soils surrounding mine areas in South Korea are often contaminated with multiple metals such as Cd, Pb and Zn. It poses potential risks to plants, soil organisms, groundwater, and eventually human health. The aim of this study was to examine the changes in phytoavailability of Cd, Cu, Pb and Zn after application with calcined eggshell (CES; 0, 1, 3, and 5% W/W) in an agricultural soil contaminated by mine tailings. The contents of Cd, Cu, Pb and Zn in soils were 8.79, 65.4, 1602, and $692mgkg^{-1}$ (aqua regia dissolution), respectively. The experiments were conducted with lettuce (Lactuca sativa L. var. longifolia) grown under greenhouse conditions during a 30-d period. $NH_4NO_3$ solution was used to examine the mobile fraction of these metals in soil. The application of CES dramatically increased soil pH and inorganic carbon content in soil due to CaO and $CaCO_3$ of CES. The increased soil pH decreased the mobile fraction of Cd, Pb, Zn: from 3.49 to < $0.01mgkg^{-1}$ for Cd, from 79.4 to $1.75mgkg^{-1}$ for Pb, and from 29.6 to $1.13mgkg^{-1}$ for Zn with increasing treatment of CES from 0 to 5%. In contrast, the mobile fraction of Cu was increased from 0.05 to $3.08mgkg^{-1}$, probably due to the formation of soluble $CuCO_3{^0}$ and Cu-organic complex. This changes in the mobile fraction resulted in a diminished uptake of Cd, Pb and Zn by lettuce and an increased uptake of Cu: from 4.19 to < $0.001mgkg^{-1}$ dry weight (DW) for Cd, from 0.78 to < $0.001mgkg^{-1}$ DW for Pb, and from 133 to $50.0mgkg^{-1}$ DW for Zn and conversely, from 3.79 up to $8.21kg^{-1}$ DW for Cu. The increased contents of Cu in lettuce shoots did not exceed the toxic level of $>25mgkg^{-1}$ DW. The mobile contents of these metals in soils showed a strong relationship with their contents in plant roots and shoots. These results showed that CES effectively reduced the phytoavailability of Cd, Pb, and Zn to lettuce but elevated that of Cu in consequence of the changed binding forms of Cd, Cu, Pb, and Zn in soils. Based on these conclusions, CES can be used as an effective immobilization agent for Cd, Pb and Zn in contaminated soils. However, the CES should be applied in restricted doses due to too high increased pH in soils.
Feasibility Study of Different Biochars as Adsorbent for Cadmium and Lead
Kim, In Ja,Kim, Rog-Young,Kim, Ji In,Kim, Hyoung Seop,Noh, Hoe-Jung,Kim, Tae Seung,Yoon, Jeong-Ki,Park, Gyoung-Hun,Ok, Yong Sik,Jung, Hyun-Sung 한국토양비료학회 2015 한국토양비료학회지 Vol.48 No.5
The objective of this study was to evaluate the effectiveness of different biochars on the removal of heavy metals from aqueous media. The experiment was carried out in aqueous solutions containing $200mg\;CdL^{-1}$ or $200mg\;PbL^{-1}$ using two different biochars derived from soybean stover and orange peel (20 mg Cd or $Pbg^{-1}$ biochar). After shaking for 24 hours, biochars were filtered out, and Cd and Pb in the filtrate were analyzed by flame atomic absorption spectrophotometer (FAAS). In order to provide information regarding metal binding strength on biochars, sequential extraction was performed by modified SM&T (formerly BCR). The results showed that 70~100% of initially added Cd and Pb was adsorbed on biochars and removed from aqueous solution. The removal rate of Pb (95%, 100%) was higher than that of Cd (70%, 91%). In the case of Cd, orange peel derived biochar (91%) showed higher adsorption rate than soybean stover derived biochar (70%). Cd was adsorbed on the biochar mainly in exchangeable and carbonates fraction (1st phase). In contrast, Pb was adsorbed on it mainly in the form of Fe-Mn oxides and residual fraction (2nd and 4th phase). The existence of Cd and Pb as a form of surface-precipitated complex was also observed on the surfaces of biochars detected by field emission scanning electron microscope (FESEM) and energy dispersive X-ray spectrometer (EDAX).
A Brief Review of Soil Systematics in Germany
Rog-Young Kim(김록영),Jwa-Kyung Sung(성좌경),Seok-Cheol Kim(김석철),Byoung-Choon Jang(장병춘),Yeon-Kyu Sonn(손연규) 한국토양비료학회 2010 한국토양비료학회지 Vol.43 No.1
각 나라마다 토양이 생성되는 환경이 다르고, 토양분류가 활용되는 목적이 다르기 때문에 세계적으로 다양한 토양분류체계가 발전되어 왔다. 1998년부터 국제적으로 통용되기 시작한 WRB 분류체계와 미국의 분류체계인 Soil Taxonomy는 그동안 국내에 잘 알려져 왔지만, 위의 두 체계와 분류기준을 달리하는 독일 분류체계인 Soil Systematics는 아직 잘 알려져 있지 않다. 본 논문에서 독일 분류체계의 구성과 분류기준을 소개하고자 한다. German Systematics는 6 단계 구조로 이루어져 있고, 상부에서 하위 순서로, soil divisions, soil classes, soil types, soil subtypes, soil varieties, soil subvarieties로 세분화된다. 독일 토양은 먼저 토양수분상태에 따라 4개의 soil divisions 중 하나로 분류되며, 이들은 육지토양, 반육지토양, 반습지/습지토양, 토탄토양이다. 육지토양은 다시 토양발달상태, 층위분화에 따라 13개의 soil classes로 분류되며, 예로 토양발달이 미약한 O/C-토양, 토양발달이 많이 진전되고 Ae-층을 갖는 Podsole (WRB 명명법: Podzols; U.S. Taxonomy: Spodosols)를 들 수 있다. 반육지토양은 지하수토양, 담수토양, 해수토양, 해변토양의 4개의 soil classes로, 반습지/습지토양은 반습지토양, 습지토양의 2개의 soil classes로, 토탄토양도 자연적, 인위적 토탄토양의 2개의 soil classes로 세분화된다. Soil classes는 U.S. Taxonomy의 orders와 비교될 수 있다. 육지토양의 soil classes는 다시 29개의 soil types로, 토양발달이 미약한 토양은 모재에 따라, 토양발달이 진전된 토양은 토양생성과정에 따라 분류된다. 반육지토양의 soil classes는 토양발달 정도에 따라 17개의 soil types로, 반습지/습지토양의 soil classes는 유기물함량에 따라 5개의 soil types로, 토탄토는 생성과정에 따라 5개의 soil types로 세분화된다. Soil types은 독일 토양조사의 기본 단위이며, U.S. Taxonomy의 great groups과 비교될 수 있다. 토양단면의 미세한 형태학적 차이를 고려하여 다시 약 220개의 soil subtypes, 수천 개의 soil varieties과 soil subvarieties로 세분화될 수 있다. Due to diverse soil-forming environments and different purposes of the soil classification, numerous soil classification systems have been developed worldwide. The World Reference Base for Soil Resources (WRB) and the Soil Taxonomy of the United States are well-known in Korea. However, the German Soil Systematics based on somewhat different principles from the two former systems is little-known. The objective of this paper is therefore to give a short overview of the principles of the German Soil Systematics. The German Soil Systematics consists of a six-level hierarchical structure which comprises soil divisions, soil classes, soil types, soil subtypes, soil varieties, and soil subvarieties. Soils in Germany are firstly classified into one of four soil divisions according to the soil moist regime: terrestrial soils, semi-terrestrial soils, semi-subhydric/subhydric soils, and peats. Terrestrial soils are subdivided into 13 soil classes based on the stage of soil formation and the horizon differentiation. Semi-terrestrial soils are differentiated into four classes regarding the source of soil moist: groundwater, freshwater, saltwater, and seaside. Semi-subhydric/subhydric soils are subdivided into two classes: semi-subhydric and subhydric soils. Peats are classified into two classes of natural and anthropogenic origins. Classes can be compared to orders of the U.S. Taxonomy. Classes are subdivided into 29 soil types with regard to soil forming-processes for terrestrial soils, into 17 types with regard to the soil formation for semi-terrestrial soils, into five types with regard to the content of organic matter for semi-subhydric/subhydric soils, and also into five types with regard to peat-forming processes for peats. The soil mapping units in Germany are types, which can be additionally subdivided into ca. 220 subtypes, several thousands of varieties and subvarieties using detailed nuances of morphologic features of soil profile. Soil types can be compared to great groups of the U.S. Taxonomy.