基于光学传感的水系沉积物速率估算

B. Saranga, U. Premarathne, B. Atapattu
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引用次数: 2

摘要

河流携带的沉积物导致水库容量减少,影响水力发电,影响社区和农业部门的有效灌溉管理。经济有效的测量工具对于准确预测沉降速率在我国是至关重要的。本文介绍了一种基于光学传感的沉降速率估计机制的发展。总悬浮物(TSS)与浊度(NTU)之间的相关性是在传感器标定阶段发展起来的。在25天的时间内收集了经验数据样本(从Uma oya分支到斯里兰卡的Rantambe水库)并用于校准。在实验室条件下,线性回归分析结果表明,浊度与TSS的关系为1NTU = 1.5 mg/l。采用ISO 7027浊度法测定水样中悬浮颗粒的浓度,并采用光学传感机构进行检测。建立了浑浊度与传感器值之间的相关性,并确定了含沙量(mg/s)。利用光学传感机制,对短期泥沙速率进行了较为准确的估计。
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Stream Sediment Rate Estimation using Optical Sensing
Sediments carried by the rivers cause capacity reduction in reservoirs which impacts the hydro-power generation, effective irrigation management for communities and agricultural sectors. Cost effective measurement tools for accurate prediction of the sedimentation rate is vital in our country. This paper describes the development of an optical sensing based sedimentation rate estimation mechanism. Correlation between Total Suspended Solid (TSS) and turbidity (NTU) is developed during sensor calibration stage. Empirical data samples (from the Uma oya limb to Rantambe reservoir in Sri Lanka) were collected over a period of 25 days and used for calibration. Under laboratory conditions, the results from the linear regression analysis revealed that the relationship of the Turbidity and the TSS is 1NTU is equal to 1.5 mg/l. The ISO 7027 Turbidity Technique method was used to determine the concentration of suspended particles in water samples and tested using the optical sensing mechanism. Correlation between turbidity and sensor value was developed and the quantity of sediment in mg/s was determined. Using the optical sensing mechanism, the results evidenced reasonably accurate for short term sediment rate estimation.
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