Tag:rain profiles

№03|2023

WASTEWATER DISPOSAL SYSTEMS

UDC 628.221
DOI 10.35776/VST.2023.03.07

Volkov Sergei, Luk’ianchuk Maksim, Zhitenev A. I., Kuz’min Valentin, Rublevskaya O. N., Hyamyalyainen M. M., Gvozdev V. A., Erofeev Vasilii, Kostenko I. G., IGNATCHIK V. S., Ignatchik S. Iu., Kuznetsova N. V., Seniukovich Mikhail

Methods and results of estimating calculated rain parameters
for the surface runoff disposal systems of Saint-Petersburg
Part 1. For hydraulic calculations while designing

Summary

Municipal systems of surface runoff disposal must be adapted to the conditions of the changed climate with account of the local conditions and specific circuit designs. In accordance with the world practice, one of the stages of the work package in this area is the justification of the calculated rain parameters for the considered climate area. At the same time, to solve design problems, it is enough to adjust the standard climatic parameters. When substantiating their calculated values, the method of adaptation of the complex parameter A is applied to the group of scaling methods. It was established that for St. Petersburg, the dynamics of change in parameter A for the period ∆τ = 50 years was 9.1%. The result obtained using this method was verified by comparing it with the results of other studies: cited in the third estimation report on climate changes and their consequences in the Russian Federation; obtained by the FSBI «Main Geophysical Observatory named after A. I. Voeikov»; obtained by the classical method that provided for processing of the primary experimental information.

Key words

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№04|2023

WASTEWATER DISPOSAL SYSTEMS

UDC 628.221
DOI 10.35776/VST.2023.04.07

Volkov Sergei, Luk’ianchuk Maksim, Zhitenev A. I., Kuz’min Valentin, Rublevskaya O. N., Gvozdev V. A., Erofeev Vasilii, Kostenko I. G., IGNATCHIK V. S., Ignatchik S. Iu., Kuznetsova N. V., Seniukovich Mikhail

Methods and results of estimating calculated rain parameters for the surface runoff disposal systems of Saint-Petersburg Part 2. For hydraulic calculations in simulation

Summary

Urban surface runoff disposal systems need to be adapted to the changing climate with account of local conditions and schematic design features. In line with the world practice, one of the stages of the works in this area is the substantiation of the calculated parameters of rain for the considered climatic region. At the same time, to fulfill the design tasks adjusting the specified climatic parameters will be sufficient. However, justifying the solutions on the upgrade of the drainage systems using computational models, substantiating the profiles of calculated rains constituting the graphs of the temporal variations of their intensity is needed. While substantiating these profiles, the following requirements were taken into account: the maximum 10-minute amount of precipitation that can cause flooding in the wastewater disposal networks; the accumulative amount of atmospheric precipitation during 1 hour that can cause flooding in the tunnel sewers. It has been established that under these requirements, the temporal variation of the rain intensity representing the design rain profile can be expressed as a continuous analytical function with two parameters: i0 – the maximum instantaneous rain intensity (mm/h) and the empirical parameter φ (min–1). It has been experimentally determined that for St. Petersburg, for example, with a return period of p = 1 year, φ = 0.1837 min–1, i0 = 40.21924 mm/h.

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№06|2023

WASTEWATER DISPOSAL SYSTEMS

UDC 628.221
DOI 10.35776/VST.2023.06.05

Volkov Sergei, Luk’ianchuk Maksim, Zhukova Anastasiia, Zhitenev A. I., Kuz’min Valentin, Rublevskaya O. N., Gvozdev V. A., Erofeev Vasilii, Kostenko I. G., IGNATCHIK V. S., Ignatchik S. Iu., Kuznetsova N. V., Fes’kova A. Ia.

Methods and results of estimating calculated rain parameters for the surface runoff disposal systems of Saint-Petersburg
Part 3. For hydraulic calculations in designing and modeling with account of the uneven distribution of rain intensities areally

Summary

Municipal surface runoff disposal systems need to be adapted to the changing climate with account of local conditions and schematic design features. In line with the world practice, one of the stages of the research in this area is the substantiation of the calculated parameters of rain for the considered climatic region. Herewith, to solve design problems, adjusting the standard climatic parameters is sufficient, whereas, to solve the problems related to the justification of decisions on the upgrade of wastewater disposal systems using calculation models, justifying the design rain profiles constituting graphs of the intensity variations over time is required. In addition, justifying the calculated parameters of rains with account of the spatial variability is needed. Beyond that, for large areas, the design rainfall parameters must be converted to average values. In world practice, this is done by multiplying the average rainfall intensity for a given duration, frequency and area by the appropriate reduction factor – areal reduction factor (ARF). In domestic practice, while designing, a similar reduction factor is also used called a correction factor that takes into account the uneven rainfall areally. However, the reliability of the values of these correction factors is very doubtful, since, for example, with a runoff area of less than 4km2, the values are available only for the conditions of Moscow, whereas the origin of the values for a runoff area of more than 4km2 is not known. For these reasons, in St. Petersburg, along with the assessment of the actual and prospective parameters of calculated rains used in design and modeling, the regularities of the distribution of rain intensity areally were additionally determined. As a result of the research, the hypothesis that areal and point precipitation have the same probability of exceeding was confirmed, as well as the type and parameters of the dependence were substantiated for estimating the actual values of the correction factors that take into account the unevenness of rainfall areally.

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