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为探索猪肺炎支原体阴性群的培育方法,本试验研究了集成联合用药、SEW和“三点式”饲养管理体系等技术对猪肺炎支原体的净化效果。先通过妊娠母猪的筛选,母猪程序性用药,SEW技术,屏障隔离系统,“三点式”生产饲养管理体系及仔猪程序性用药的培育方法,再通过猪肺炎支原体血清抗体检测和荧光定量 PCR检测鼻拭子的方法对所培育的仔猪进行长达4个月的监测,结果发现新培育的5批猪在35日龄后血清抗体均为阴性,鼻拭子抗原检测全为阴性。结果表明集成联合用药、SEW和"三点式"生产管理体系技术可以有效净化猪肺炎支原体,为国内猪气喘病的控制和净化提供理论基础及临床实践经验。 相似文献
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Inverse models to analyze the spatiotemporal variations of chemical weathering fluxes in a granito-gneissic watershed: Mule Hole, South India 总被引:1,自引:0,他引:1
B. Siva Soumya M. Sekhar J. Riotte Stephane Audry Christelle Lagane Jean-Jacques Braun 《Geoderma》2011,165(1):12-24
Water-rock reactions are driven by the influx of water, which are out of equilibrium with the mineral assemblage in the rock. Here a mass balance approach is adopted to quantify these reactions. Based on field experiments carried out in a granito-gneissic small experimental watershed (SEW), Mule Hole SEW (~ 4.5 km2), quartz, oligoclase, sericite, epidote and chlorite are identified as the basic primary minerals while kaolinite, goethite and smectite are identified as the secondary minerals. Observed groundwater chemistry is used to determine the weathering rates, in terms of ‘Mass Transfer Coefficients’ (MTCs), of both primary and secondary minerals.Weathering rates for primary and secondary minerals are quantified in two steps. In the first step, top red soil is analyzed considering precipitation chemistry as initial phase and water chemistry of seepage flow as final phase. In the second step, minerals present in the saprolite layer are analyzed considering groundwater chemistry as the output phase. Weathering rates thus obtained are converted into weathering fluxes (Qweathering) using the recharge quantity.Spatial variability in the mineralogy observed among the thirteen wells of Mule Hole SEW is observed to be reflected in the MTC results and thus in the weathering fluxes. Weathering rates of the minerals in this silicate system varied from few 10 μmol/L (in case of biotite) to 1000 s of micromoles per liter (calcite). Similarly, fluxes of biotite are observed to be least (7 ± 5 mol/ha/yr) while those of calcite are highest (1265 ± 791 mol/ha/yr). Further, the fluxes determined annually for all the minerals are observed to be within the bandwidth of the standard deviation of these fluxes. Variations in these annual fluxes are indicating the variations in the precipitation. Hence, the standard deviation indicated the temporal variations in the fluxes, which might be due to the variations in the annual rainfall. Thus, the methodology adopted defines an inverse way of determining weathering fluxes, which mainly contribute to the groundwater concentration. 相似文献
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