应用于鱼道设计的新疆木扎提河斑重唇鱼的游泳能力测试

为了探究斑重唇鱼的游泳能力，给过鱼设施设计和鱼类游泳行为学研究提供基础参数，本研究以木扎提河野生斑重唇鱼(全长TL=12~16 cm)为研究对象，测定了其在(16.6±1.6) ℃水温下的感应流速、临界游泳速度、爆发游泳速度及持续与耐久游泳能力。结果显示，斑重唇鱼感应流速为(0.18±0.02)m/s，相对感应流速为(1.40±0.23) BL/s (BL为体长)；临界游泳速度为(1.02±0.15) m/s，相对临界游泳速度为(8.58±1.65) BL/s；爆发游泳速度为(1.39±0.17) m/s，相对爆发游泳速度为(10.92±1.86) BL/s；最大持续游泳速度为0.87 m/s，最大耐久游泳速度为1.37 m/s，与平均爆发游泳速度相近。其持续游泳时间与流速呈负相关(${\rm lg}T = - 5.136{{X}} + 8.504$)。当以斑重唇鱼为主要过鱼对象时，建议为吸引鱼类进入鱼道，进口流速设计为1.02~1.39 m/s，休息池主流设计为0.20~1.02 m/s，鱼道竖缝处流速宜低于0.85 m/s。鱼道长度为1 000 m时，鱼道内平均水流速度应低于0.78 m/s。本研究结果可为新疆木扎提河流域鱼类游泳能力研究提供参考，对保护日益减少的鱼类资源具有重要意义。     

Observation of three‐dimensional flow structures and effluent transport around fish cages using a towed ADCP and free‐fall multi‐parameter profiler

A field campaign was conducted around salmon cages, using a combination of a towed ADCP and a free‐fall multi‐parameter profiler, in order to investigate flow structures and the possible distribution of effluent materials. Two transect observations showed that hydrographic conditions changed dramatically within 5 days, from highly stratified open water conditions to weak stratification. Three‐dimensional observation revealed that flow was blocked behind the cages and that the blockage was reduced as the distance from the cages increased. The flow speed was positively correlated with the intensity of the backscattering signal. The R² value was high immediately behind the cages and decreased with distance from the cages. The flow time series behind the cages exhibited a k^–2 power law spectrum that was consistent with a typical internal wave spectrum. This suggests that eddies shed from the cages were highly influenced by stratification. We estimated the rate of kinetic energy dissipation, , from YODA Profiler data based on the Thorpe scale approach. We also estimated the eddy diffusivity coefficient, . Both and followed a lognormal probability density function. The mean was consistent with a one‐dimensional diffusion model assessed from the R² values of flow speed and backscatter intensity.     

MacCormack算法在长输管道瞬变流动仿真中的应用

为了提高长输管道仿真精度和速率,基于MacCormack格式基本原理和流动方程建立了长输液体管道水力瞬变流动仿真模型。以某管道为例,分别采用该仿真算法和特征线法模拟了阀门关闭和流量增加引起的瞬变流动,并探讨了MacCormack格式中不同边界条件处理方法及Courant常数值对模拟结果的影响。结果表明:MacCormack格式可用于精确仿真长输管道瞬变流动过程,采用特征线法求解预估层边界参数后,其振荡幅度、收敛速度均优于特征线仿真方法;同时,采用特征线法处理MacCormack格式边界条件较线性外插法更易收敛。研究成果可为长输管道瞬变流动仿真提供参考。     

横轴流脱粒分离装置的数学模型的建立与试验

横轴流脱粒分离装置滚筒长度限制了其脱粒分离能力,仅被应用于中小型联合收割机。为研究横轴流脱粒分离装置脱粒滚筒转速、喂入量、脱粒间隙等因素对脱粒分离性能的影响,优化装置结构,利用概率学理论建立了横轴流脱粒分离装置的未脱净率和夹带损失率数学模型。对模型正确性验证试验表明,模型对未脱净率的预测相对误差为8.23%,对夹带损失率的预测相对误差为2.90%。仿真分析和试验表明,该模型可反映籽粒轴向分布和脱粒滚筒转速、喂入量、脱粒间隙等参数对脱粒分离性能的影响。     

不同叶顶间隙下斜流泵内部 流动特性的数值模拟

为研究轮缘叶顶间隙对斜流泵性能和流动不稳定特性的影响,基于SST k-ω湍流模型对某斜流泵选取了0, 0.25, 1.00, 2.00 mm 4种尺寸的叶顶间隙进行数值计算,分析间隙区域内压差分布、泄漏量、叶顶泄漏涡旋强度以及进口轴面速度分布.结果表明:不同运行工况下,斜流泵泄漏量从叶轮进口到叶轮出口先增大后减小,其与间隙区内压差变化趋势相吻合.叶顶泄漏量随着间隙尺寸的增大而增大,导致泵的能量损失增大.经对比发现,间隙尺寸是影响叶顶泄漏量的主要因素.小流量工况下,随着叶顶间隙尺寸的增大,叶顶泄漏流与主流卷吸作用形成的泄漏涡强度逐渐增强.部分泄漏流进入相邻叶片通道,导致其流动失稳.随着叶顶间隙的增大,斜流泵能量损失明显增多,且内流不稳定性明显加剧.增大流量后,不同间隙下叶顶泄漏涡旋转强度均逐渐降低.     

某高铁隧道小口径井抽水试验探讨

指出了在某高铁隧道勘察中采用小口径抽水试验方法,具有操作简单便捷,成本低的优势。通过小口径井抽水试验查明场地的水文地质条件,得出了水文地质原始数据资料,根据单孔稳定流承压水非完整井的水文地质实际情况,选取合适的公式分别计算出了隧道岩层渗透系数及影响半径,为高铁隧道的勘察设计及顺利施工提供参考。     

Performance and welfare of Atlantic salmon,Salmo salar L. post-smolts in recirculating aquaculture systems: Importance of salinity and water velocity

Producing a larger post-smolt in recirculating aquaculture systems (RAS) could shorten the production time in sea cages and potentially reduce mortality. Knowledge of the biological requirements of post-smolts in closed-containment systems is however lacking. In the present study, the effects of salinity and water velocity on growth, survival, health, and welfare of Atlantic salmon reared in RAS were examined. Salmon smolts were stocked in three separate RAS with salinities of 12, 22, and 32‰ and subjected to high (1.0 body lengths per s⁻¹) or low (0.3 body lengths second⁻¹) water velocity. Growth performance, survival, welfare, and physiological stress responses were monitored until the fish reached a bodyweight of around 450 g. Growth rate was higher at lower salinity and higher water velocity generally had a positive effect on growth in all salinities. Feed conversion ratio was lower at 12‰ compared to the 22 and 32‰ when the fish were between 250 and 450 g. Higher mortality, elevated plasma cortisol levels, higher incidence of cataract, and a higher expression of stress-induced genes in the skin (iNOS, Muc5ac-like) indicated a negative effect of higher salinity on fish welfare. Male maturation was low (<1%), and not affected by salinity or water velocity.     

考虑水文变异的水库生态流量研究

为探讨水文变异对生态流量影响,确定最佳水库生态流量推求方法,针对尼尔基水库生态问题,采用Mann-kendall突变检测法、滑动T检验法和有序聚类法,结合序号总和理论和Spearman相关系数计算对水文时间序列作综合识别,确定水库发生水文变异年份为1963年和1999年。利用NGPRP法和逐月频率年内展布计算法分别计算天然状态、次天然状态、现状和不考虑水文变异条件下最小生态流量和适宜生态流量。参考Tennant法评价结果表明水库生态系统退化主要受人类扰动影响,观察次天然状态和不考虑变异状态下生态径流过程,最小生态流量占多年平均流量百分数相差9.21%和1.70%,适宜生态流量相差3.04%和1.47%。研究应更多考虑次天然生态径流过程,其最小生态流量仅可作为生态流量下限。     

Hydrological and water cycle processes of inland river basins in the arid region of Northwest China

The increasing shortage in water resources is a key factor affecting sustainable socio-economic development in the arid region of Northwest China(ARNC). Water shortages also affect the stability of the region's oasis ecosystem. This paper summarizes the hydrological processes and water cycle of inland river basins in the ARNC, focusing on the following aspects: the spatial-temporal features of water resources(including air water vapor resources, runoff, and glacial meltwater) and their driving forces; the characteristics of streamflow composition in the inland river basins; the characteristics and main controlling factors of baseflow in the inland rivers; and anticipated future changes in hydrological processes and water resources. The results indicate that:(1) although the runoff in most inland rivers in the ARNC showed a significant increasing trend, both the glaciated area and glacial ice reserves have been reduced in the mountains;(2) snow melt and glacier melt are extremely important hydrological processes in the ARNC, especially in the Kunlun and Tianshan mountains;(3) baseflow in the inland rivers of the ARNC is the result of climate change and human activities, with the main driving factors being the reduction in forest area and the over-exploitation and utilization of groundwater in the river basins; and(4) the contradictions among water resources, ecology and economy will further increase in the future. The findings of this study might also help strengthen the ecological, economic and social sustainable development in the study region.     

Influence of salinity and moisture on the threshold shear velocity of saline sand in the Qarhan Desert,Qaidam Basin of China: A wind tunnel experiment

Determination of the threshold shear velocity is essential for predicting sand transport, dust release and desertification. In this study, a wind tunnel experiment was conducted to evaluate the influence of salinity and moisture on the threshold shear velocity of saline sand. Saline sand samples (mean particle size of 164.50-186.08 μm and the total silt, clay and salt content of 0.80%-8.25%) were collected from three saline sand dunes (one barchan dune and two linear dunes) in the Qarhan Desert, Qaidam Basin of China. Original saline sand samples were placed in two experimental trays for wet and dry processing to simulate deliquescence and desiccation, respectively. Surface moisture content ranging from 0.30% to 1.90% was generated by the steam method so that the saline sand can absorb water in a saturated water vapor environment. The motion of sand particles was determined by the observers with a solid laser. The laser sheet (0.80 cm thick), which was emitted by the solid laser, horizontally covered the sand surface and was bound to the sand. Results show that the cohesion of saline sand results from a combination of salt and water. The threshold shear velocity increases exponentially with the increase in crust thickness for the linear sand dunes. There is a positive linear correlation between the original moisture content and relative threshold shear velocity. The threshold shear velocity of dewatered sand is greater than that of wet sand with the same original moisture content. Our results will provide valuable information about the sand transport of highly saline soil in the desert.