• Title/Summary/Keyword: liming

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Testicular Characteristics and the Block to Spermatogenesis in Mature Hinny

  • Han, Hongmei;Wang, Aihong;Liu, Liming;Zhao, Gaoping;Su, Jie;Wang, Biao;Li, Yunxia;Zhang, Jindun;Wu, Baojiang;Sun, Wei;Hu, Shuxiang;Li, Shuyu;Zhao, Lixia;Li, Xihe
    • Asian-Australasian Journal of Animal Sciences
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    • v.29 no.6
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    • pp.793-800
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    • 2016
  • Most hinnies (female donkey${\times}$male horse) and mules (female horse${\times}$male donkey) are sterile with few reports of equine fertile hybrids. The main cause of this sterility is thought to be a meiotic block to spermatogenesis and oogenesis. This study compared the developmental features of the testes and a histological analyses of spermatogenesis in a male hinny with those of a normal, fertile stallion and Jack donkey. Hinny testes showed a thicker tunica albuginea, fewer blood vessels and more connective tissue in the testis parenchyma than those of the stallion and Jack donkey. Although the mean number of seminiferous tubules was significantly higher in stallion and hinny than Jack donkey (p<0.01), the mean proportion of seminiferous tubules was lower in the hinny (p<0.01) which resulted in a smaller diameter of seminiferous tubules. The mean number of spermatogonia and spermatocytes per unit area were significantly lower in hinny testis (p<0.01) and no spermatids or mature spermatozoa cells were found during immunofluorescent analyses. These results indicated that defects in seminiferous tubule development and structure occur in the testis of hinnies. Furthermore, most spermatogonia and spermatocytes cease development in synapsis during mid-meiosis of spermatocytes, which results in a block to spermatogenesis that prevents the formation of spermatids and matured spermatozoa during meiosis in male hinnies.

Greenhouse Gas Inventory in Land-Use Change and Forestry in Korea (임업 및 토지이용부문의 온실가스 흡수 및 배출 현황)

  • 이경학;손영모;김영수
    • Journal of Korea Foresty Energy
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    • v.20 no.1
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    • pp.53-61
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    • 2001
  • An approach method for the greenhouse gas inventory in land-use change and forestry in Korea based on the 1996 revised IPCC(Intergovernmental Panel on Climate Change) guideline was developed and carbon budget of the year 1998 in this sector was estimated using the developed method as follow. For the category of changes in forests and other woody biomass stocks, carbon removal from the atmosphere by growth was 11,911 thousands TC(tons of carbon), carbon emissions to the atmosphere by harvests was 824 thousands TC, and net carbon removals was, therefore, 11,087 thousands TC, Emissions from decay of biomass remained after conversion of forest land to other land uses was estimated to 82 thousands TC For the category of land-use change and management, carbon emissions in mineral soils from land-use change was 1,025 thousands TC, that from liming of agricultural soils was 32 thousands TC, and total emissions was, therefore, 1,057 thousands TC. In summary, the carbon budget of land-use change and forestry of the year 1988 was as follows; the removal of 11,911 thousands TC, the emissions of 1,963 thousands TC, and the net removal of 9,948 thousands TC which was 9.6% of the emissions of 103,601 thousands TC from energy sector of the same year.

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Dynamics of Heavy Metals in Soil Amended with Oyster Shell Meal (굴 패화석시용에 따른 토양 내 중금속 동태 변화)

  • Lee, Ju-Young;Hong, Chang-Oh;Lee, Chang-Hoon;Lee, Do-Kyoung;Kim, Pil-Joo
    • Korean Journal of Environmental Agriculture
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    • v.24 no.4
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    • pp.358-363
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    • 2005
  • A large amount of oyster-shell waste has been illegally disposed at oyster farm sites along the southern coast of Korea, which already created serious environmental problems. Therefore, the study was undertaken to increase the consumption of oyster shell meal as a soil amendment. The effects of oyster shell meal on dynamics of heavy metals and uptake of heavy metals by spring Chinese cabbage were evaluated in silt loam soil (in Gyeongsang National University, Jinju, Gyeongnam-do, Korea), where 0, 4, 8, 12 and 16 Mg $ha^{-1}$ oyster-shell meal fertilizer were added. Lime treatment (2 Mg $ha^{-1}$) was selected as a control. In the results of this study, cabbage yields were increased by increasing levels of oyster-shell meal fertilizer. With increasing levels of oyster-shell meal fertilizer, total heavy metals concentrations were not significant among treatments. However, 0.1N HCl extractable heavy metals concentration was significantly reduced due to increasing of soil pH. A lot of portion (ca. $80{\sim}90%$) heavy metals fraction of all fractions was residual phase in soil after harvesting. The contents of Cu, Mo, Zn in cabbage were slightly increased by increasing levels of oyster shell meal fertilizer. However, there were no toxic symptoms of heavy metals during cultivation. Conclusively, it was estimated that oyster shell fertilizer could be a good amendment to increase productivity of crop and reduce uptake of heavy metals by crop and mobility of heavy metals in soil.

Soil problems for developing grass land in Jeju (제주도(濟州道) 초지개발(草地開發)에 있어서 토양학적(土壤學的) 문제점(問題點))

  • Lee, Chong Ki;Lee, Keun Sang
    • Korean Journal of Soil Science and Fertilizer
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    • v.8 no.3
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    • pp.153-160
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    • 1975
  • Jeju island has high potential productivity of livestock in terms of climate, geography, and economic prospect. Grass-land is now widespread and increasing rapidly year after year. However, the productivity of grass land is very low compared with that of main land. It is supposed that the low productivity is due to improper chemical properties of volcanic ash soil which is mostly distributed in the island. Volcanic ash soil, which have high alumina ratio, is characterized by the lack of bases and avilable phosphorous while its phosphorous fixation capacity is very high. In addition to poor chemical properties, low level of fertilization technique appears to be another limitation to grass production. Farmers have not given care to improve their soil to be suitable for grass cultivation. In order to increase the productivity of grassland in Jeju, the proper amounts of N, P, and K fertilizer should be applied following the improvements of poor chemical properties such as liming and a great deal of phosphorous increment, using mainly fused phosphate, based upon the balance of bases, and the application of organic matter and micro-elements which can be easily deficient in soil.

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Survey on Packaging Waste Occurrence and Recycling for Each Packaging Material in Europe (유럽의 포장 폐기물 발생 및 포장 재료별 재활용에 관한 고찰)

  • Kim, Doyeon;Ko, Euisuk;Lee, Hakrae;Shim, Woncheol;Yang, Liming;Kim, Jaineung
    • KOREAN JOURNAL OF PACKAGING SCIENCE & TECHNOLOGY
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    • v.23 no.1
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    • pp.17-26
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    • 2017
  • In order to confirm European packaging waste statistics, this study was investigated annual variability of packaging waste generated, target of recovery and recycling rate for packaging waste and recycling rate of European countries based on Eurostat database. Eurostat is regional society statistics organization designated by European community to distribute development, production and European statistics. From 2005 to 2013, paper and paperboard packaging were generated the largest amount among the total amount of packaging waste generated during the period and the share of main packaging materials were generally constant among the packaging materials. In addition, European Union member countries have established target for the recycling rate and recycling rate for packaging waste which has been well maintained by most EU countries since the 2008 directive was enacted. The recycling rate for whole packaging waste such as glass, paper and paperboard, metal, plastic, wood continues to increase in Europe. In this study, Europe packaging waste statistics were organized and analyzed as yearly transformation of Europe packaging waste occurrence and disposal, recycling rate and recovery rate target value of Europe countries and recycling rate of each country in Europe base on centralized Eurostat database. Moreover GDP reduction were also confirmed due to trend changes and indirect impacts such as economic slump by packaging waste and recycling.

Effect of Lime Application on Growth and Yield of Peanut at Newly Reclaimed Upland Soil (야산(野山) 개간지(開墾地) 토양(土壤)에서 땅콩의 생육(生育) 및 수량(收量)에 미치는 석회시용효과(石灰施用效果))

  • Kim, Heek-Kweon;Jeon, Jang-Hyeob;Kim, Dea-Hyang;Jeong, Ji-Ho;Park, Keon-Ho
    • Korean Journal of Soil Science and Fertilizer
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    • v.23 no.3
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    • pp.180-187
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    • 1990
  • This experiment was conducted to find a methode reducing peant empty pods when it was cultivated on a newly reclaimed upland soil in Kimjae, Jeonbuk, Korea. Liming materials, slaked lime and dolomite were applied to the soil at two levels : lime requirement amount neutralizing the soil and one of 1.5 times. The results are summarized as the followings. 1. There was a yield increase of 27% from the field applied 1.5 times amount of dolomite Compared to that of slaked lime. The number of empty pods per plant was at the lowest level with the treatment of higher amount of dolomite. 2. At the maturing stage of the plant there was a positive significant correlation observed between the content of MgO and other parameters such as no, of branchs per plant dry weight per plant, no, of pods per plant and 100 seed-weight. But the correlation between MgO content and the no of empty pods was negatively significant at 5% level. 3. The content of CaO and MgO was significantly correlated to hull and pod volumes, pod surface area, hull thickness and hull weight. 4. Correlation coefficients between yield and the contents of Ca and Mg in soil at mauring stage were $0.572^{**}$ and $0.556^{**}$ respectively.

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Soil Characteristics and Improvement of Reclaimable Hillside Land (산지토양(山地土壤)의 특성(特性)과 개량(改良))

  • Ryu, In-Soo
    • Korean Journal of Soil Science and Fertilizer
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    • v.11 no.4
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    • pp.247-262
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    • 1979
  • Majority of reclaimable soils in hillside lands in Korea are red yellow soils, with exception in Jeju island, where most of reclaimable hillside lands are composed of volcanic ash soils. Songjeong, Yesan and Samgag series are the major soil series of red yellow soils which are available for the reclamation. When observed in the fields, they are distinguished as reddish brown clay loam, red yellow sand loam and yellowish brown sand loam. They have moderately good physical properties but their chemical properties are generally poor for crop cultivations. The chemical properties of red yellow soils, as compared to long time cultivated (matured) soils, are characterized by very low pH, high in exchangeable Al content and phosphorus fixation capacity. Also extraodinary low available phosphorus and organic matter contents are generally observed. On the other, the chemical properties of volcanic ash soils are characterized by high armophous Fe and Al hydroxides and organic matter contents, which are the causative factors for the extremely high phosphorus fixation capacity of the soils. The phosphorus fixation capacity of volcanic acid soils are as high as 5-10 times of that of red yellow soils. Poor growth of crops on newly reclaimed red yellow soils are mainly caused by very low available P and pH and high exchangeable Al. Relatively high P fixation capacity renders the failure of effective use of applied P when the amount of application is not sufficient. Applications of lime to remove the exchangeable Al and relatively large quantity of P to lower the P fixation capacity and to increase the available P are the major recommendations for the increased crop production on red yellow hillside soils. Generally recommendable amounts of lime and P to meet the aforementioned requirements, are 200-250kg/10a of lime and $30-35kg\;P_2O_5/10a$. Over doses of lime. frequently induces the K, B, arid Zn deficiencies and lowers the uptake of P. In volcanic ash soils, it is difficult to alter the exchangeable Al and the P fixation capacity by liming and P application. This may be due to the peculiarity of volcanic ash soil in chemical properties. Because of this feature, the amelioration of volcanic ash soils is not as easy as in the case of red yellow soils. Application of P as high as $100kg\;P_2O_5/10a$ is needed to bring forth the significant yield response in barley. Combined applications of appropriate levels of P, lime, and organic matter, accompanied by deep plowing, results in around doubling of the yields of various crops on newly reclaimed red yellow soils.

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Study on the Oxidation Process of Potential Acid Sulfate Soil (잠재 산성황산염토양의 산화과정에 대한 연구)

  • Han, Kang-Wan;Chun, Jae-Chul;Cho, Jae-Young;Kim, Geum-Hee;Ann, Yeoul
    • Korean Journal of Soil Science and Fertilizer
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    • v.29 no.3
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    • pp.243-248
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    • 1996
  • To find out the oxidation process of potential acid sulfate soil(PASS) along with time. the PASS were treated with lime and ammonia water to adjust soil pH in laboratory column condition. pH range of PASS showed 6.5 to 7.5. however, complete oxidized PASS by $H_2O_2$ showed 2.1 to 2.5. After pilling the PASS under the natural condition. oxidation occured slowly from surface of the pilled soil. The oxidation of PASS proceeded slowly when the soil was in submerged condition. but quickly in dried condition. The content of sulfide-sulfur in PASS sharply decreased after exposing to the air and the decreasing rate was greater in dried than in submerged condition. The content of sulfate-sulfur continuously decreased in submerged condition. but increased in dried condition. Contents of $Fe^{+{+}}$ and $Al^{+{+}}$ in PASS were generally increased with time and the increasing rate was greater in submerged than in dried condition. Liming to PASS was slowly acting to pH change and ammonia water caused fast pH change within a short period of time. The contents of sulfate-sulfur and exchangeable aluminum in drainage water decreased with time and the contents of sulfide-sulfur and ferrous iron were increased.

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Studies on Degradation of Butachlor and Nitrofen in Different Soil Conditions (토양중(土壤中) Butachlor 와 Nitrofen의 분해(分解)에 관(關)한 연구(硏究))

  • Oh, Byung-Youl;Jeong, Young-Ho;Lee, Byung-Moo
    • Applied Biological Chemistry
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    • v.24 no.2
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    • pp.112-119
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    • 1981
  • The persistence of preemergence herbicides, butachlor [2-chloro-2,6-diethyl-N(butoxymethyl) acetanilide] and nitrofen(2,4-dichlorophenyl-4-nitrophenyl ether), at 10 ppm level in different soil conditions amended with organic matter and lime was studied under flooded and field moisture capacity. The microbial breakdown played a major role in the dissipation of the herbicides in soil. Nitrofen degradation in flooded soil was greatly accelerated, while it was slowed down in field moisture capacity as compared with butachlor. Increased amendment of rice straw to the soil shortened the half-life of butachlor under flooded condition, however it prolonged that of butachlor when the amendment was exceeded over 1% on dry weight basis. Liming the soil stimulated decomposition of the herbicides in the soil systems, which ap pears to be pH independent.

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Characteristics and Improvement of Potential Acid Sulfate Soil Derived from Continental Materials on Alluvial Fan (선상지(扇床地) 육성(陸成) 잠재특이산성토(潛在特異酸性土)의 특성과 개량)

  • Jung, Yeun-Tae;Yun, Eul-Soo;Son, Il-Soo
    • Korean Journal of Soil Science and Fertilizer
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    • v.25 no.3
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    • pp.195-201
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    • 1992
  • A Potential acid sulfate soil derived from continental Holocene deposits on the fan-base was found and it was characterized with improvement practices. Artesian wells were scattered in the area, and the imperfectly drained soils were featured by having fine loamy with 7~30% of gravels. The potential acid sulfate soil layers were typified by having darkness in color with around 3.3~3.8% of O.M. and 0.34~0.41% of total sulfur. Soil pH ranged from 3.4 to 3.8 but it was decreased to 1.9~2.5 after oxidation with $H_2O_2$. Ground water sprang out from an artesian well contained a high amount of minerals such as Na, Ca, Mg, K, etc. and about 80ppm of sulfate which seemed to be responsible for pyrite formation. The soil was classified to member of "Fine loamy, mixed, acid, mesic, sulfic Haplaquepts" in taxonomically, and "weak potential acid sulfate soils" in interpretatively. The installation of tile drains with adding fine earth and liming were effective. However, the pH goes down to 4.8 again after 3 years of improvement practices.

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