共查询到20条相似文献，搜索用时 125 毫秒
1.
目的：优化枸杞多糖(LBP)的精制工艺,为LBP的开发提供参考。方法：以多糖提取率为指标,采用正交试验考察提取次数、提取时间、料液比对多糖提取工艺的影响。在单因素试验的基础上,以糖损失率为指标,利用正交试验优化活性炭除色素工艺,以蛋白清除率和糖损失率的综合评分为指标,采用正交试验优化酶-sevag法脱蛋白工艺。结果：最佳提取工艺为提取次数2次、提取时间30 min、料液比1∶10。最佳除色素工艺为活性炭用量1.0%、温度100℃、时间20 min;糖损失率为28.6%。最佳除蛋白工艺为酶用量1.5%、温度50℃、时间60 min;蛋白质清除率为28.2%,糖损失率为10.9%。结论：优选的LBP精制工艺稳定可行,适用于LBP产品开发。 相似文献
2.
目的:正交试验优选猫爪草纳米乳喷雾剂的最佳提取工艺。方法:以总黄酮提取量和浸膏得率的综合评分为评价指标，在单因素试验基础上，采用L9(3）正交试验考察猫爪草醇提工艺的溶剂体积、乙醇浓度、提取时间及提取温度对提取工艺的影响。结果:最佳提取工艺为以75%乙醇为提取溶剂，提取温度60 ℃，第1 次8倍量1.5 h，第2 次7倍量1 h，共提取2 次。结论:在单因素试验基础上，通过正交试验优选的提取工艺经验证稳定、简便易行、预测性好，为猫爪草纳米乳喷雾剂的进一步研发奠定了基础。 相似文献
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目的：优选老鹳草中柯里拉京的提取工艺条件，并通过对 α-淀粉酶活力的抑制作用初步判断柯里拉京的降糖作用。方法：以柯里拉京提取率为指标，采用单因素考察提取方法、提取溶剂和提取次数对老鹳草柯里拉京提取率的影响；在单因素试验的基础上，采用正交设计法优化老鹳草水提取工艺条件。结果：老鹳草水提取的最佳工艺条件为加水回流提取2次，用量8，6倍，提取时间 1.5，1.5 h，在此条件下，老鹳草柯里拉京的提取率 1.2%，影响老鹳草柯里拉京提取率的因素从大到小依次为：加水倍数＞提取时间＞浸泡时间。结论：通过对α-淀粉酶活力的抑制作用测定，表明老鹳草中柯里拉京有较好的降糖作用。 相似文献
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目的：优选复方莪术散颗粒的最佳提取与颗粒制备工艺，为该复方的开发利用提供试验依据。方法：采用正交试验法对复方莪术散进行提取，以淫羊藿苷的含量和收率综合评价为指标，通过L9（34）正交试验设计对醇的用量、提取的时间和提取次数进行考察，优选复方莪术散的醇提取工艺，再以浸膏为原料，通过L9（34）正交试验设计考察稀释剂（可溶性淀粉）的比例及粘合剂（乙醇）的浓度和干燥温度，制备复方莪术散颗粒。结果：复方莪术散提取最佳工艺为A2B22C11D1，即处方药材加60%浓度的10倍剂量的乙醇，提取2次，每次1.5h为最优。最佳制备工艺为A3B2C2，即干浸膏∶淀粉的比例为1∶2.5，并以90%乙醇为湿润剂，采用湿法制粒的方法，干燥温度为60℃，所制得颗粒剂经检查符合相关要求。结论：本试验所得复方莪术散颗粒剂的提取与制备工艺合理、可行，为该复方的开发利用提供了试验依据。 相似文献
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目的：优选大黄总蒽醌的提取工艺。方法：以大黄游离总蒽醌为主要指标，考察闪式法、超声法与回流法3种不同提取方法对其含量的影响，并采用正交实验法优化闪式提取法的工艺。结果：闪式法与回流法对大黄游离总蒽醌的提取率分别为87.1%、87.0%，均高于超声提取法的84.3%；闪式法每次提取时间为3min，较回流法与超声法更为迅速高效。闪式提取法优选的工艺条件为：料液比（g/mL）1∶9，提取时间80s，转速4000r/min。结论：闪式提取法能避免大黄蒽醌苷受热水解，提取时间短、效率高、经济节能，具有工业化生产应用的前景。 相似文献
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目的：优选前列舒康片的提取工艺。方法：以浸膏得率、盐酸小檗碱和京尼平苷酸为评价指标，将溶剂倍数、溶剂种类、提取时间、浸泡时间等作为考察因素，通过正交试验优选出前列舒康片的提取工艺。结果：优选出前列舒康片中黄柏醇提工艺为黄柏粗粉加乙醇回流提取2次，第1次加7倍量60%乙醇提取1.5h，第2次加6倍量60%醇提取1h；车前子等药材水提工艺为加水煎煮2次，1次加8倍量水，浸泡1h，煎煮2h；第2次加6倍量水，煎煮1.5h。结论：通过正交试验优选出的前列舒康片提取工艺合理可行、重复性良好，可为前列舒康片的工艺研究提供参照。 相似文献
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目的：优选补肾健骨凝胶的制备工艺。方法：采用正交试验法,以干膏得量、补骨脂素、异补骨脂素含量为评价指标,优选最佳提取工艺;以外观形态、凝胶初黏度、pH值、指标成分累积渗透量为指标,分别将空白基质、中和剂及促渗剂进行筛选。结果：最佳提取工艺为按处方比例,称取除龙血竭外的补骨脂等5味药材,提取3次,第1次加8倍量80%乙醇,第2、3次分别加8倍量水,每次提取1 h。卡波姆、三乙醇胺、月桂氮卓酮的用量分别为制成量的1%、2%、2%。结论：制得的凝胶质地光滑细腻、药物分散良好。 相似文献
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The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ～200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ～380 km from the coast at a depth of ～250 m above the sea level. 相似文献
12.
We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances
using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium
partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and
in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority
accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative
abundances of organic and inorganic carbon as an index of the carbon cycle stability. 相似文献
13.
We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the
Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of
rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the
transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic
regime of the sea.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
14.
V. A. Ivanov S. P. Lyubartseva N. Mikhailova N. B. Shapiro 《Physical Oceanography》2001,11(6):509-524
We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an
ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics
is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of
a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic
elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as
a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water
area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the
shelf zone and open sea.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
15.
Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east 总被引：2，自引：0，他引：2
A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry
dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly
goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with
the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then
passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state. 相似文献
16.
Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m3 from 1 km of coast in the wide tidal flats and <50 m3 on the steep coasts) are delivered to the water area. 相似文献
17.
I. E. Timchenko A. A. Primalenny V. D. Yarin E. F. Vasechkina E. M. Igumnova 《Physical Oceanography》2001,11(4):367-378
We use many-year archival observations of hydrologic and hydrobiologic state of the Sea of Azov for the identification of
the structure of a model of its ecosystem. The ecosystem model, supplemented with expert estimates of bioresource consumption
(fish reserve), contamination level, and possible ecologic fines for violation of the sea natural state, is formalized by
the method of system dynamics. Hereat, the major part of influence functions is found in terms of observational data with
application of self-organization algorithms. We also present the results of simulated experiments with the model of the ecosystem,
which enable us to analyse scenarios of its behaviour under the influence of various external factors (wind, river discharge,
water exchange with the Black Sea, etc.).
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
18.
E. L. Vinogradova 《Oceanology》2008,48(4):483-492
The spatiotemporal variability of the hydrochemical composition of the riverine runoff in nearmouth areas is presented using the example of selected rivers of the Arctic Basin. The temporal dynamics of the riverine nutrient runoff are mainly determined by the seasonal and interseasonal variations in the drainage basins. The spatial variations in the chemical composition of riverine waters in the near-mouth areas are mainly caused by the dynamics of the water flow and the river bed relief and, to a lesser degree, by biochemical processes. It is shown that the variations in the nutrient composition of the waters in near-mouth areas are comparable in magnitude to those at the river-sea geochemical barriers. 相似文献
19.
The methodology and the first results of the computations of the volumes, masses, and growth rates of the sedimentary body of the buried Black Sea basin are presented. Their temporal evolution reflects the regional paleogeodynamics, in particular, the reorientation of the vector of the relative movement of the Arabian and Eurasian lithospheric plates and the related intensification of their collision in the late Miocene-Pliocene. 相似文献
20.
Izvestiya, Atmospheric and Oceanic Physics - Analysis of the temporal variations of the virtual heights of the sporadic E layer (h?ES) determined from ionograms with increased accuracy (1... 相似文献