Evaluation of the Tibia as a Source of Autogenous Cancellous Bone in the Horse     

MICHAEL J. BOERO DVM  MS    J. EUGENE SCHNEIDER DVM    JACOB E. MOSIER DVM  MS  DiplomateACVIM    MARK M. GUFFY DVM  MS  DiplomateACVR    HUGH C. BUTLER DVM  MS  DiplomateACVS  HORST W. LEIPOLD PhD 《Veterinary surgery : VS》1989,18(4):322-327

A 1 cm defect was created in the proximal medial cortex of 12 tibiae, cancellous bone was removed from the site, and the bones were fractured by loading in torsion. The fractures did not occur through the donor sites and the fracture patterns and loads to fracture were similar for the treated tibiae and their untreated mates. Cancellous bone was harvested from the proximal medial aspect of both tibiae in nine adult horses. The soft tissue wounds were monitored for more than 10 days in seven horses and healing of the osseous defects was evaluated radiographically at regular intervals to month 6 in two horses. The site provided convenient access with the horses in lateral or dorsal recumbency, the anatomic landmarks were reliable, and the surgical procedure was simple and short. Complications occurred in only three incisions.  相似文献   

Pharmacokinetics of probenecid in sheep     

V. H. GUERRINI  L. J. FILIPPICH  P. B. ENGLISH  JENNY SCHNEIDER  G. R. CAO  D. W. A. BOURNE 《Journal of veterinary pharmacology and therapeutics》1985,8(2):128-135

Six Merino ewes were given 1 g (27 g/kg) probenecid by the intravenous (i.v.), intramuscular (i.m.) and subcutaneous (s.c.) routes. After i.v. injection, the biological half-life was 1.55 h and apparent volume of distribution at the steady state (Vdss) 0.18 l/kg. Body clearance (ClB) and renal clearance (ClR) were 0.12 l/h/kg and 0.03 l/h/kg, respectively. Approximately 28% of unchanged probenecid was excreted in urine. Plasma probenecid concentrations after i.v., i.m. and s.c. injections were 133, 37, and 31 micrograms/ml, respectively, at 15 min; 76, 36, and 34 micrograms/ml at 1 h; and 43, 23 and 34 micrograms/ml at 2 h. The average bioavailability of probenecid given by i.m. and s.c. injection was 46% and 34%, respectively. However, after 2 h, probenecid plasma concentrations remained higher when it was given subcutaneously than when it was given intramuscularly. Urine output was correlated positively (P less than 0.05) with kel and ClB. Urine pH increased significantly (P less than 0.01) for the first 2 h, and then steadily declined over the subsequent 6 h. The results suggested that probenecid in sheep was rapidly eliminated because it was rapidly excreted in the normal but alkaline urine. Subcutaneous administration of probenecid in animals may be a useful alternative to oral or i.v. administration.  相似文献   

Some x-ray cristallographic data on DDT     

FANKUCHEN L  SCHNEIDER M  SINGER J 《Science (New York, N.Y.)》1946,103(2662):25-26

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Translocation of particles within plants     

MITCHELL JW  SCHNEIDER IR  GAUCH HG 《Science (New York, N.Y.)》1960,131(3417):1863-1870

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The effect of incubation at 56 C. on the tube agglutination test for bovine brucellosis     

MORSE EV  SCHNEIDER DW  McNUTT SH 《American journal of veterinary research》1955,16(59):269-273

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Solution of tobacco mosaic virus in the aqueous phase of a chloroform-water emulsion and application of this phenomenon in virus assay     

SCHNEIDER IR 《Science (New York, N.Y.)》1953,117(3028):30-31

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功能膜覆盖好氧堆肥过程氨气减排性能研究   总被引：8，自引：0，他引：8  

马双双  孙晓曦  韩鲁佳  李仁权  UWE Schlick  黄光群 《农业机械学报》2017,48(11):344-349

畜禽粪便高温好氧堆肥过程中氨气的排放不仅污染环境,而且会降低有机肥氮素含量。因此,控制好氧堆肥过程中氨挥发是降低氮损失及减少堆肥周边环境恶臭的关键。为研究膜覆盖对畜禽粪便好氧堆肥过程氨气挥发的影响,以猪粪和小麦秸秆为试验原料,采用具有选择渗透性的Gore膜作为覆盖材料,在实验室好氧堆肥反应器系统中进行了为期27 d的好氧堆肥试验。试验设置覆膜组和对照组,采用开启1 h、关闭1 h间歇通风方式,通风速率为3 L/min,重点监测堆肥过程堆体温度、氧浓度和NH3排放速率等。研究表明:覆膜组比对照组高温期持续时间略长,更有利于杀死堆体有害病原菌;相比于对照组,覆膜组NH3排放量减少18.87%;相比于温度峰值出现的时间,两组试验NH3峰值出现时间均延后,且覆膜组延后时间更长。  相似文献   

Lack of abnormal hemoglobins in Alaskan Eskimos,Indians, and Aleuts     

SCOTT EM  GRIFFITH IV  HOSKINS DD  SCHNEIDER RG 《Science (New York, N.Y.)》1959,129(3350):719-720

In an examination of the blood of 708 Eskimos, 200 Aleuts, and 44 Indians in Alaska for abnormal types of hemoglobin, only normal hemoglobin A was detected. It may be concluded that abnormal hemoglobins in these races are rare if they occur at all.  相似文献   

Influence of soil solution Ca concentration on short-term K release and fixation of a loamy soil   总被引：1，自引：0，他引：1  

A. SCHNEIDER 《European Journal of Soil Science》1997,48(3):513-522

The Ca concentration of the soil solution influences K plant nutrition by its influence on K concentration of the soil solution and on soil buffer power through ion exchange and K release or fixation. The effects of the imposed solution Ca concentration on the estimates of these parameters and on these two phenomena were studied on a loamy soil. Potassium sorption and desorption experiments were conducted for 16 h at five initial Ca concentrations (from 0 to 10^?1 M) and followed by the measurement of soil exchangeable K (ammonium acetate extraction). Soil K-Ca exchange properties and the contributions of exchangeable K and non-exchangeable K to K dynamics of the soil-solution system were estimated. The‘Ratio Law’ applied for the medium range of Ca concentrations, i.e. 10^?1 M to 10^?3 M. But, it failed for some experiments at small initial Ca concentrations (0 M and 10^?4 M). This failure went with a decrease of the number of sites of great affinity for K in K-Ca ion exchange and/or a decrease of the amount of K not in exchange equilibrium with Ca but extracted by M ammonium acetate. Release of K increased and fixation of K decreased when Ca concentration increased. The relation between the change in the amount of non-exchangeable K during the experiment and the initial constraint (ø) was curvilinear on the large range of ø investigated. But, this relation was independent of Ca concentration. The K concentration of the solution for which neither sorption of K by the soil nor desorption of K from the soil occurred decreased and the slope of the sorption-desorption curve at this K concentration increased when the solution Ca concentration decreased. These two parameters can be considered the K concentration of the soil solution of the soil and the buffer power of the soil, respectively, only if the initial Ca concentration imposed during the sorption-desorption experiments is close to the Ca concentration of the soil solution of the soil. A predictive model of the soil buffer power based on ion exchange and release-fixation properties is proposed. Despite some discrepancies at very low Ca concentrations (<0·5 mM Ca) when‘Ratio Law’did not apply the agreement between calculated and observed values was good. The model permits the correction of the experimentally obtained buffer power for the bias related to the great solution volume: soil weight ratio commonly used during the sorption-desorption experiments.  相似文献   

Short-term release and fixation of K in calcareous clay soils. Consequence for K buffer power prediction     

A. SCHNEIDER 《European Journal of Soil Science》1997,48(3):499-512

Non-exchangeable K always contributes to some degree to plant nutrition. To understand this contribution and to deduce a predictive buffer power model the release and fixation of K was studied on a range of 44 calcareous clay soils. Short-term K sorption and desorption experiments (16 h) were followed by the measurement of soil exchangeable K (ammonium acetate extraction). Soil K-Ca exchange properties and the contributions of exchangeable K and non-exchangeable K to K dynamics of the soil-solution system were estimated. The change in the amount of non-exchangeable K during the experiment was generally proportional to the initial constraint imposed to the soil-solution system (ø), i.e. the solution: soil ratio multiplied by the difference between the solution K concentration imposed at the beginning of the experiment and the solution K concentration for which neither sorption nor desorption of K would occur. The proportionality coefficient (β) called the 'soil ability for K release and fixation’ was identical for release and fixation for 36 soils, whereas eight soils showed some difference between their ability for fixation and their ability for release of K. When β was considered identical in the release range and in the fixation range for all soils it was inversely proportional to the initial K saturation ratio of the CEC corrected for the amount of ammonium extractable K which was not in exchange equilibrium with Ca. This quantity of ammonium extractable K which is not in equilibrium with Ca probably contributes only partially to plant nutrition. For the studied soils this quantity contributed a large proportion of exchangeable K (26–65%) especially in soils with a small K content. Due to the contribution of non-exchangeable K to soil-solution K dynamics the buffer power of the system does not only depend on exchange properties but also on soil release and fixation properties. When β was taken into account buffer power was better estimated than when it was deduced from ion exchange alone.  相似文献