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(10R)-3c-Acetoxy-10r.13c-dimethyl-17c-((1R:4R)-1.4.5-trimethyl-hexen-(2t)-yl)-(9cH.14tH)-Δ5.7-dodecahydro-1H-cyclopenta[a]phenanthren | 2874-25-1

中文名称
——
中文别名
——
英文名称
(10R)-3c-Acetoxy-10r.13c-dimethyl-17c-((1R:4R)-1.4.5-trimethyl-hexen-(2t)-yl)-(9cH.14tH)-Δ5.7-dodecahydro-1H-cyclopenta[a]phenanthren
英文别名
3β-Acetoxy-24βF-methyl-9β-cholestatrien-(5.7.22t);O-Acetyl-isopyrocalciferol;9β-Ergostatrien-(5.7.22t)-yl-(3β)-acetat;Essigsaeure-(9β-ergostatrien-(5.7.22t)-yl-(3β)-ester);3β-Acetoxy-9β-ergostatrien-(5.7.22t);Isopyrocalciferol acetate;[(3S,9R,10R,13R,14R,17R)-17-[(E,2R,5R)-5,6-dimethylhept-3-en-2-yl]-10,13-dimethyl-2,3,4,9,11,12,14,15,16,17-decahydro-1H-cyclopenta[a]phenanthren-3-yl] acetate
(10<i>R</i>)-3<i>c</i>-Acetoxy-10<i>r</i>.13<i>c</i>-dimethyl-17<i>c</i>-((1<i>R</i>:4<i>R</i>)-1.4.5-trimethyl-hexen-(2<i>t</i>)-yl)-(9<i>cH</i>.14<i>tH</i>)-Δ<sup>5.7</sup>-dodecahydro-1<i>H</i>-cyclopenta[<i>a</i>]phenanthren化学式
CAS
2874-25-1
化学式
C30H46O2
mdl
——
分子量
438.694
InChiKey
NGEVNHYPVVOXPB-ZLQSPFBJSA-N
BEILSTEIN
——
EINECS
——
  • 物化性质
  • 计算性质
  • ADMET
  • 安全信息
  • SDS
  • 制备方法与用途
  • 上下游信息
  • 反应信息
  • 文献信息
  • 表征谱图
  • 同类化合物
  • 相关功能分类
  • 相关结构分类

计算性质

  • 辛醇/水分配系数(LogP):
    8
  • 重原子数:
    32
  • 可旋转键数:
    6
  • 环数:
    4.0
  • sp3杂化的碳原子比例:
    0.77
  • 拓扑面积:
    26.3
  • 氢给体数:
    0
  • 氢受体数:
    2

SDS

SDS:a1b99ddbf9fd1d9544f103df611bbe3c
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上下游信息

  • 上游原料
    中文名称 英文名称 CAS号 化学式 分子量
  • 下游产品
    中文名称 英文名称 CAS号 化学式 分子量

反应信息

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文献信息

  • Mueller, Hoppe-Seyler's Zeitschrift fur Physiologische Chemie, 1935, vol. 233, p. 223,231
    作者:Mueller
    DOI:——
    日期:——
  • The Impact of Municipal Solid Waste Management on Greenhouse Gas Emissions in the United States
    作者:Keith A. Weitz、Susan A. Thorneloe、Subba R. Nishtala、Sherry Yarkosky、Maria Zannes
    DOI:10.1080/10473289.2002.10470843
    日期:2002.9
    Technological advancements, environmental regulations, and emphasis on resource conservation and recovery have greatly reduced the environmental impacts of municipal solid waste (MSW) management, including emissions of greenhouse gases (GHGs). This study was conducted using a life-cycle methodology to track changes in GHG emissions during the past 25 years from the management of MSW in the United States. For the baseline year of 1974, MSW management consisted of limited recycling, combustion without energy recovery, and landfilling without gas collection or control. This was compared with data for 1980, 1990, and 1997, accounting for changes in MSW quantity, composition, management practices, and technology. Over time, the United States has moved toward increased recycling, composting, combustion (with energy recovery) and landfilling with gas recovery, control, and utilization. These changes were accounted for with historical data on MSW composition, quantities, management practices, and technological changes. Included in the analysis were the benefits of materials recycling and energy recovery to the extent that these displace virgin raw materials and fossil fuel electricity production, respectively. Carbon sinks associated with MSW management also were addressed. The results indicate. that the MSW management actions taken by U.S. communities have significantly reduced potential GHG emission's despite an almost 2-fold increase in waste generation. GHG emissions from MSW management were estimated to be 36 million metric tons carbon equivalents (MMTCE) in 1974 and 8 MMTCE in 1997. If MSW were being managed today as it was in 1974, GHG emissions would be similar to60 MMTCE.
  • Dimroth, Chemische Berichte, 1937, vol. 70, p. 1631,1635
    作者:Dimroth
    DOI:——
    日期:——
  • Effect of burning on soil organic matter content and N mineralization under shifting cultivation system of Karen people in Northern Thailand
    作者:Sota Tanaka、Tomonori Ando、Shinya Funakawa、Chainarong Sukhrun、Thammanoon Kaewkhongkha、Katsutoshi Sakurai
    DOI:10.1080/00380768.2001.10408418
    日期:2001.9
    In the traditional shifting cultivation system practiced by the Karen people in northern Thailand, the effects of burning on the content of extractable organic matter, microbial biomass, and N mineralization process of the soils were studied. Five plots (5 x 5 m(2) quadrat) with 0, 10, 20, 50, and 100 Mg ha(-1) of slashed materials were arranged and burned. Ten to 20 Mg ha(-1) of slashed biomass corresponded to the amount commonly burned by the Karen people. During the burning process, the soil temperature at the depth of 2.5 cm in the 100 Mg ha(-1) plot almost evenly increased to 300 degreesC while the temperature in the 10 to 50 Mg ha(-1) plots increased with large variations from 50 to 300 degreesC. Burning caused a conspicuous increase in the contents of organic C and (organic+ mineral)-N extracted at room temperature and a simultaneous decrease in the contents of microbial biomass C and N, especially in the soil of the 100 Mg ha(-1) plot. In the rainy season, the values of the changes induced by burning reverted to the values recorded before burning, except for the microbial biomass in the 100 Mg ha(-1) plot, which still remained lower. Based on an incubation experiment, N mineralization rate was higher in the soils taken just after burning, especially in the 100 Mg ha(-1) plot, than in the soils taken during the rainy season. However, the soil in the 100 Mg ha(-1) plot was considered to have the lowest ability to supply mineral N among the soils in the rainy season. Burning of 10 to 20 Mg ha(-1) biomass corresponding to the values recorded in Karen peoples' shifting cultivation system was more compatible with soil ecology in terms of N supply at the initial stage of crop growth and of microbial biomass recovery during the rainy season, compared to the burning of 100 Mg ha(-1) biomass corresponding to the value recorded in a natural forest. Thus, the shifting cultivation system implemented by the Karen people can be considered to be a well-balanced agricultural system.
  • AGARWAL, VINITA;HUSAIN, SHAKIR;GUPTA, K. C., ACTA CHIM. HUNG., 127,(1990) N, C. 77-81
    作者:AGARWAL, VINITA、HUSAIN, SHAKIR、GUPTA, K. C.
    DOI:——
    日期:——
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同类化合物

(5β)-17,20:20,21-双[亚甲基双(氧基)]孕烷-3-酮 (5α)-2′H-雄甾-2-烯并[3,2-c]吡唑-17-酮 (3β,20S)-4,4,20-三甲基-21-[[[三(异丙基)甲硅烷基]氧基]-孕烷-5-烯-3-醇-d6 (25S)-δ7-大发酸 (20R)-孕烯-4-烯-3,17,20-三醇 (11β,17β)-11-[4-({5-[(4,4,5,5,5-五氟戊基)磺酰基]戊基}氧基)苯基]雌二醇-1,3,5(10)-三烯-3,17-二醇 齐墩果酸衍生物1 黄麻属甙 黄芪皂苷III 黄芪皂苷 II 黄芪甲苷 IV 黄芪甲苷 黄肉楠碱 黄果茄甾醇 黄杨醇碱E 黄姜A 黄夹苷B 黄夹苷 黄夹次甙乙 黄夹次甙乙 黄夹次甙丙 黄体酮环20-(乙烯缩醛) 黄体酮杂质EPL 黄体酮杂质1 黄体酮杂质 黄体酮杂质 黄体酮EP杂质M 黄体酮EP杂质G(RRT≈2.53) 黄体酮EP杂质F 黄体酮6-半琥珀酸酯 黄体酮 17alpha-氢过氧化物 黄体酮 11-半琥珀酸酯 黄体酮 麦角甾醇葡萄糖苷 麦角甾醇氢琥珀酸盐 麦角甾烷-6-酮,2,3-环氧-22,23-二羟基-,(2b,3b,5a,22R,23R,24S)-(9CI) 麦角甾烷-3,6,8,15,16-五唑,28-[[2-O-(2,4-二-O-甲基-b-D-吡喃木糖基)-a-L-呋喃阿拉伯糖基]氧代]-,(3b,5a,6a,15b,16b,24x)-(9CI) 麦角甾烷-26-酸,5,6:24,25-二环氧-14,17,22-三羟基-1-羰基-,d-内酯,(5b,6b,14b,17a,22R,24S,25S)-(9CI) 麦角甾-8-烯-3-醇 麦角甾-8,24(28)-二烯-26-酸,7-羟基-4-甲基-3,11-二羰基-,(4a,5a,7b,25S)- 麦角甾-7,22-二烯-3-酮 麦角甾-7,22-二烯-17-醇-3-酮 麦角甾-5,24-二烯-26-酸,3-(b-D-吡喃葡萄糖氧基)-1,22,27-三羟基-,d-内酯,(1a,3b,22R)- 麦角甾-5,22,25-三烯-3-醇 麦角甾-4,6,8(14),22-四烯-3-酮 麦角甾-1,4-二烯-3-酮,7,24-二(乙酰氧基)-17,22-环氧-16,25-二羟基-,(7a,16b,22R)-(9CI) 麦角固醇 麦冬皂苷D 麦冬皂苷D 麦冬皂苷 B