نقش پساب تصفیه شده شهری بر نرخ فرسایش رسوبات چسبنده در کانال‌های انتقال آب

در حال حاضر بررسی میزان فرسایش رسوبات چسبنده یک بخش مهم در سازه های انتقال آب، با استفاده از پیش بینی و تعیین رفتار رسوبات می باشد. از طرفی در مناطق خشک منابع آب تجدیدپذیر نظیر پساب تصفیه شده شهری به عنوان یک ذخیره آبی مطمئن در برنامه ریزی منابع آب به منظور تامین نیاز بخش صنعت و کشاورزی مورد توجه قرار می گیرد. خصوصیات شیمیایی پساب موجب تغییر رفتار رسوبات چسبنده در کانال های انتقال آب می شود. از این رو در این تحقیق با استفاده از یک فلوم دایره ای به بررسی نرخ فرسایش رسوبات چسبنده در دوره های تحکیم مختلف پرداخته شد. در این راستا آزمایش ها در سه حالت آب خالص، سیال حاوی 30 و 60 درصد پساب انجام و دوره تحکیم رسوبات در بستر فلوم 1، 3، 14 و 28 روز در نظر گرفته شد. نتایج نشان می دهد در تمام دوره های تحکیم در ابتدای زمان اعمال تنش برشی، نرخ فرسایش به دلیل حضور رسوبات سطحی ابتدا افزایش و سپس کاهش می یابد. بیشترین نرخ فرسایش در سیال حاوی 60 درصد پساب و در تنش برشی 35/2 نیوتن بر مترمربع رخ داد. همچنین با افزایش دوره تحکیم اختلاف نرخ فرسایش در پساب 30 درصد، با آب خالص و 60 درصد پساب افزایش می یابد که این امر به دلیل وجود بالاتر بودن شاخص esp بیشتر در شرایط 30 درصد پساب است. در دوره تحکیم های یکسان بیشتر بودن شاخص esp در سیال حاوی 30 درصد پساب که منجر به پخشیدگی بیشتر ذرات، عمق ته نشینی بیشتر و پوکی کمتر گردید.

The role of urban wastewater on the rate of cohesive sediment erosion in water transfer channels

Introduction: Bridge scour is one of the most important challenges in river engineering. Research into local scour has primarily focused on investigating the impact of different hydrodynamic conditions on scour in a bed of uniformly graded material. However, local scour investigations in a bed of uniformly wellgraded material provided knowledge of the underlying processes, field sediment beds are much more complex consisting of nonuniform sediment mixtures (&σ& _&g& &>1.4& ). In the case of complex sediment beds, selective transport of the finer particles due to unequal mobility can make the bed surface to be armored. There have been relatively few studies reported in the literature relating to scour in complex sediment beds, and most of these relate to quite specific situations. With regards to natural river materials (nonuniform sediments) and its great effects on the dimension and the time evolution of scour hole, the interaction of flowstructures with nonuniform sediments is very crucial due to armor layer development. The aim of this study is to improve understanding of scour development and armoring evolution in nonuniform sediment beds for estimating the scour depth in more realistic field conditions. Therefore, the rate of variation of erosion over time around single cylindrical pier is investigated in different bed sediment types. Methodology: The armored layer due to selective transport of the finer particles in nonuniform sediments causes complexity for predicting equilibrium scour depth. The present experiments on local bridge scour were conducted in hydraulic laboratory of the BuAli Sina University (Hamadan, Iran). The pier model with a diameter of 4 cm was put inside a 0.5 m wide, 10.5 m long and 0.5 m depth rectangular tilting flume. In this study, the number of 15 experiments were organized at five different sediment beds, uniform and nonuniform in two steady flow condition (20 and 35 l/s with the same flow intensity of u/uc~0.9) along with an unsteady flow. The duration of tests was fixed at 8 hours in all runs based on the empirical method given by Ettema (1980). Results and Discussion: The experimental results revealed that with increasing flow rate from 20 to 35 l/s (increasing follow shallowness, h/b) at the same sediment bed, not only larger scour depths were recorded, but also the armor layer became coarser. The comparison between the bed configurations with uniform and nonuniform sediments represented dramatical reduction of the scour depth regards with increasing sediment nonuniformity. The effect of nonuniform sediments on scour in a current clear water conditions showed that maximum scour depth was less than scour depth in a uniform sand with the same d50 value. The comparison between these two mentioned bed configurations showed that the change in geometric standard deviation (&σ& _&g& ) from 1.4 to 2 (altering the uniform bed to nonuniform), decreased the maximum depth of scour by 70% and 60% in two corresponding experiments. As the armor layer coarser grains remains at upstream flow bed and at the vicinity of scour hole in the same flow intensity, the scour depth was decreased. Otherwise, there was not remarkable decrease on the scour depth by increasing nonuniformity index, since two sediment beds types were nonuniform. Also, a slight increase on scour depth has been observed by reduction of median grain size in the beds with nonuniform sediments at the same geometric standard deviation. By taking into account of the grain size of the armor layer and ice cover roughness, Wu et al. (2014) analyzed the dimensionless maximum scour depth and they found out that with an increase in grain size of the armor layer, the dimensionless maximum scour depth decreases. Singh et al. (2018) investigated the incipient motion for gravel particles in cohesionless sediment mixtures having silt and sand. The visual observations of the channel bed after the end of incipient motion indicated appearance of gravel particles at the top surface of the sediment bed. The critical shear stress for the gravel particles was found to be lower in the presence of silt. Presence of silt in the mixture affects the critical shear stress for gravel particles. They concluded from the present study that high silt content in the mixture leads to the higher deviation of critical shear stress from the revised Shields curve. They proposed an equation for the determination of critical shear stress of gravel particles in the nonuniform sediment mixture. Conclusion: The results showed that scour depths were reduced dramatically as sediment nonuniformity index (&σ& _&g& ) increase in clear water conditions. The larger particles form an armor layer protecting the bed from eroding. Also, the observation indicated that with increasing flow depth, the armor layer coarsens, and larger scour depths were recorded. However, scour depth increase rate was very different for the various bed sediment types.