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排序方式: 共有476条查询结果,搜索用时 15 毫秒
1.
The aim of this prospective study was to evaluate the Clinitek status™ analyser using Multistix10SG™/Microalbustix™ dipsticks (all: Siemens Dx) for canine urine (n = 101) compared to reference methods: visual reading (Combur9 dipstick, Roche), refractometry, microscopy, and quantitative protein/creatinine analysis (Pentra400, AxonLab). The automated analyses were done twice and visual tests were performed by two examiners.An excellent to good concordance was demonstrated between the first/second analysis with the Multistix10SG and the Combur9 dipstick, respectively with Cohen’s κ-values ranging from 0.776 to 1.000. Agreement between both dipsticks was good for glucose (κ = 0.753), blood (κ = 0.793), protein (κ = 0.788), and moderate for bilirubin (κ = 0.431) and ketones (κ = 0.540). In 6/101 specimens, false positive ketone reactions were obtained with the Multistix10SG™. Multistix10SG™ could not be used for determination of pyuria or specific gravity. Semiquantitative/quantitative protein results correlated well (ρ = 0.90) and creatinine measurements moderately (ρ = 0.76). Due to automated data transmission to the laboratory information system, the Clinitek status™ is of advantage in veterinary laboratories/clinics. 相似文献
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为了解干旱区淡水湖泊沉积物微生物在氨氧化中的功能,利用铵盐培养基对博斯腾湖不同深度沉积物进行驯化培养,结合水环境因子分析混合菌株产亚硝酸盐能力,从中分离纯化氨氧化细菌并对其氨转化能力进行试验。结果表明,6个采样位点12个样品中,11号位点深层沉积物(20~40 cm)混合菌株能有效利用铵盐产生亚硝酸盐,且连续6 d稳定维持其质量浓度高达20 mg/L以上。进而,从该混合菌液中分离得到30株单菌,其中有2株呈现出明显的氨氧化细菌特性。通过16S rRNA基因序列比对及形态学分析分别鉴定其为弯曲芽孢杆菌(Bacillus flexus)和赤红球菌(Rhodococcus ruber)。 相似文献
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不同土壤有机碳测定方法的比较 总被引:1,自引:1,他引:0
对土壤碳的准确定量是研究土壤肥力和农业固碳的前提。本文选择我国不同有机碳和无机碳含量的8个代表性土壤/沉积物样品,比较湿氧化法、酸洗法和间接法三类方法对有机碳含量的测定效果。研究结果表明:对有机碳含量为3.4~11.5 g/kg的土壤和沉积物样品,湿氧化法有较低的平均相对误差(0.32%~4.72%)和变异系数(0.40%~1.22%),间接法的平均相对误差(5.16%~20.46%)和变异系数(0.60%~7.00%)都较高,而酸洗法介于这两个方法之间。说明在保持稳定准确的加热温度情况下,湿氧化法对土壤/沉积物有机碳含量的测定比较稳定和准确,且操作简单。对大部分样品,由于酸对土壤无机碳难以充分溶解,造成酸洗法和间接法的有机碳测定值偏高,且变异系数较大。 相似文献
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《Journal Of Applied Aquaculture》2013,25(3):41-49
Abstract Sediment traps were deployed at Fish River Reef (FRR), a relic oyster reef on the eastern side of Mobile Bay, and at Cedar Point Reef (CPR), a productive oyster reef on the western side of Mobile Bay, Alabama, from July through October 1999. Sediment accretion at FRR was two to three times greater than sediment accretion at CPR. The proportions of particulate organic matter and ash in the sediment at the two sites were similar. The proportion of coarse to fine sediment at CPR was greater than at FRR. Also, the sediment at FRR was black and had a sulfide odor suggesting anoxia, while the sediment at CPR was brown and odorless. Various fishes and invertebrates colonized the sediment traps at CPR, while those at FRR were devoid of live organisms. Oyster spat had settled on the shells in the traps at CPR but not on those at FRR. Results suggest that in order to restore oysters at FRR, cultch material should be dispersed during periods of peak larval settlement to prevent inhibitory levels of siltation on cultch before spat settle. 相似文献
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In river channel beds composed of a wide range of grain sizes, the bed material is often arranged in discrete patches discernable by relative texture. These bed material patches are the primary source of entrainable coarse sediment within the channel system and their composition and size have been found to influence the composition and rate of sediment transport. Twelve coarse (gravel–cobble) sediment patches distributed throughout the channel network within a 4.53 ha watershed in southeastern Arizona were monitored for 2 years. Changes in patch area and grain size were measured and painted patch grains were monitored to confirm that patch grains were mobilized during flow. Individual coarse bed material patches exhibited variable persistence during flows with return frequencies ranging from approximately 1 year to 4.6 years. While no patch fully dispersed during the study period, two new patches formed. Most coarse patches remained relatively stable in area and grain-size distribution despite the entrainment of patch grains as lost grains were sufficiently replaced with sediment from upstream. Because of the grain replacement process and the effect of other sediment supply dynamics, the changes in patch area and grain-size distribution display a complex relationship with the magnitude of predicted grain mobilization within each patch. Results indicate that relative stability varies from patch to patch, influenced by the balance of patch grains transported out of the patch and the deposition of new grains into the patch. Predictive models of coarse sediment transport and yield that assume the channel bed is a fixed source of sediment supply may not adequately capture the sediment dynamics within patchy channel beds and should be used with caution when applied to these environments due to the possibility of patch instability as documented in this study. 相似文献
10.
滇池沉积物铵态氮的时空变化特征研究 总被引:4,自引:0,他引:4
沉积物在湖泊氮、磷循环和水体富营养化过程中起着重要作用。本研究应用GPS定位技术,于2003年5月至2004年5月,对滇池海埂、斗南、罗家村、新街、昆阳等5个代表性样点沉积物铵态氮含量进行为期1 a的动态监测,全面分析了滇池不同区域、不同层次、不同时期沉积物铵态氮的动态变化特征。结果表明,滇池沉积物铵态氮平均含量为74.57 mg kg-1,全湖沉积物铵态氮平均含量年变化范围是45.55~170.1mg kg-1。沉积物铵态氮因季节变化其变化幅度很大,各区域沉积物铵态氮含量总体趋势夏季高、冬季低,但不同位点变化高峰和趋势不同。不同层次沉积物铵态氮含量变化随季节而变化,夏季为表层(0~5 cm)中层(5~10 cm)底层(10~20 cm),冬季为中层表层和底层。表层、中层、底层沉积物铵态氮含量的变化范围分别为18.71~172.9mg kg-1、29.55~192.2mg kg-1、19.93~123.8mg kg-1。各区域沉积物铵态氮平均含量以罗家村最高,斗南最低。沉积物铵态氮与水体铵态氮、水体pH呈显著正相关,与沉积物有效磷呈显著负相关,暗示了沉积物铵态氮是水体氮的源和库,并影响着沉积物中磷的释放。 相似文献