Leaky sewer systems: Influence of soil properties and sewer failure characteristics on the shape of contaminant plumes

Author(s):  
Martin Binder ◽  
Christian Engelmann ◽  
Afshin Sadeghikhah ◽  
Mario Schirmer ◽  
Peter Krebs ◽  
...  

<p>At the current time, cities harbor more than 4 billion inhabitants. According to the United Nations’ projections, an increment by 2.5 billion is expected until mid-century. This will create enormous stresses to the water resource management in urban regions, including detrimental impacts on both groundwater quantity and quality. For instance, leakages from aging urban sewer network systems may lead to uncontrolled recharge and contamination. Sewer-borne contaminants cover a broad bandwidth of substances including pathogenic microbiota, nutrients and emerging contaminants. These substances may be highly persistent and accumulate in the subsurface over time. This, in turn, may pose a long-term threat to urban ecosystems. Hence, understanding the spatiotemporal distribution of sewer-borne plumes within the subsurface is of strategic importance. Sewer failures may include, among others, pipe blockades, local collapses and smaller cracks, as well as leaking joints between pipe segments. The intensity of sewer exfiltration to the soil and eventually to the aquifers depends on a variety of influencing factors, including pipe diameter and failure type as well as pipe burial depth and distance to the groundwater table. In this context, this study’s specific aim is to investigate the effect of selected vadose zone and aquifer properties and of failure characteristics on the final shape of sewer contaminant plumes to eventually delineate groundwater contamination characteristics solely from sewer network properties.</p><p>Results from two numerical studies, employing the HYDRUS 3D software code for variably saturated flow and transport simulation, will be presented. First, a small-scale principal model setup with a single pipe defect was designed to investigate the effect of soil type, colmation layer properties, pipe water level, defect shape and natural groundwater recharge on the shape of the plume in the vadose zone and at the aquifer table. Hereby, the simulations included both constant and varying pipe water levels. To define a de-facto worst-case scenario, continuous water injection as well as conservative transport (i.e., no decay or sorption) were assumed for most simulation runs. Besides the pipe water level, the intensity of precipitation was found to be a major influencing factor on the contaminant plume dimensions. In a second step, an intermediate-scale model involving a long pipe was conducted to further investigate overlay effects of multiple contaminant plumes. Here, multiple defects were positioned along the pipe in various distances, starting from a quasi-continuous line source and ending at a rather broad interval. It was found that the plume shapes on larger scale were very similar for most defect positionings, if the averaged injection rate remains the same. The direction of groundwater flow was altered in addition to the variation of the defects’ positions. Here, the contaminant plumes became slightly skewed.</p><p>The presentation will also give a short outlook to future works which will include simulations on city district scale employing HPC-capable codes such as ParSWMS, ParFlow and/or OpenGeoSys, and a comparison to simplified modeling approaches.</p>

Author(s):  
Alahyar Koochekali ◽  
Behrouz Gatmiri ◽  
Amirabbas Koochekali

True estimation of soil response during pipeline upheaval buckling is a key parameter in the safe design of subsea buried pipeline. In this paper the effects of sea mean water level over the buried pipeline and the effects of pipe burial depth on the soil response during vertical buckling are investigated. For that purpose a numerical modeling of pipeline upheaval buckling in clayey backfill has been conducted. Different sea mean water levels are considered to simulate the pipeline shore approach. In addition, various pipeline burial depths are considered to predict the soil uplift resistance and the soil failure mechanism. In order to model the large penetration of pipeline into the soft clay, Arbitrary Eulerian Lagrangian (ALE) method is employed. The results reveal that in the shallow water the sea mean water level may have considerable effects on the soil failure mechanism and soil uplift resistance. In addition, as the sea mean water level and pipe burial depth increases, a new transitional failure mechanism can be observed. The mechanism is a combination of vertical sliding block mechanism and the flow-around mechanism.


1974 ◽  
Vol 188 (1) ◽  
pp. 239-244
Author(s):  
I. G. Crow

Factors influencing the longitudinal variation of water level in the drums of circulating boilers are discussed with reference to the results of cold-circulation trials performed on a 500 MW assisted-circulation boiler. Numerical computation and small-scale model tests in support of the field trials are also presented. This information, together with evidence from further work on the operating boiler, has shown that small cold-water models provide an accurate analogue of drum operation at working pressures and temperatures.


2020 ◽  
Author(s):  
Mo Xu ◽  
Jihong Qi ◽  
Yige Tang ◽  
Xiao Li ◽  
JIan Guo

<p>Due to the inhomogeneity of the carbonate rocks and discreteness of the karst water, delineation of the groundwater flow within karst area remains a challenging task as yet. Based on KunCheng tunnel of a water diversion project in KunMing, multi-scale groundwater flow models were set upto simulate the groundwater flow. Large scale model was used to obtain the boundary conditions and hydrogeological parameters, which were then assigned to the small scale model.The small scale model was generalized as an equivalent continuous medium, and two karst pipelines are established  by module River. After then,  the multi-scale numerical modelswere used to simulate the  groundwater seepage field and predict the recovery of groundwater after tunnel construction. The main results and conclusions are as follows.</p><p>(1)Black karst pipeline and white karst pipeline systems share one recharge source but have two independent discharge systems. The recharge source is the exposed karst rock in the northeast part of study area. Obstructed by aluminum clay rock of P<sub>1</sub>d, groundwater discharge is divided into two parts during the runoff process.</p><p>(2)During the tunnel construction process, the water level at the exit of White karst pipeline reduced 9m in pipe model B<sub>1</sub> while reduced 10m in the solution fissure model B<sub>2</sub>, both two models suggest that the tunnel construction will cause the drainage of White karst pipeline exit. The water level at the exit of black karst pipeline reduced 1m in pipe model B<sub>1</sub> while reduced 4m in the solution fissure model B<sub>2</sub>.</p><p>(3)In model B<sub>1</sub>, total water discharge during tunnel construction is 69876m<sup>3</sup>/d, in model B<sub>2</sub> , the total water discharge is 95817 m<sup>3</sup>/d  and  is much larger than model B<sub>1</sub> due to the quick groundwater transporting and exchange in karst pipeline..</p><p>(4)After the tunnel construction, exits of two pipelines and observation well see the water level recovery because of the formation sealing . The recovery trend is relatively rapid in the early stage, and slow in the later stage. It takes 8.5 years and 10 years for the exits of black and white pipelines and observation wells to reach the original water level, respectively. During the recovery process, groundwater exchange form was changing from pipe supplying aquifer to aquifer supplying pipe, which made model B<sub>2</sub> recovered faster than model B<sub>1</sub> in early stage, and vice versa.</p><p>Using large scale model combining with secondary scale model, and the module River to generalize karst pipeline can reflect the flow dynamic characteristics of karst pipeline effectively.</p>


Author(s):  
Normann Vikse ◽  
Ove T. Gudmestad ◽  
Per R. Nystro̸m ◽  
Pavel Liferov

There are several challenges related to Arctic offshore oil and gas field developments. Among these is the design of pipelines transporting hydrocarbons in the field or to shore. Special considerations must be carried out to take into account the Arctic conditions. One of the most critical concerns for pipelines in shallow waters is the possible damage due to ice ridge gouging. The ice ridge keels can in some areas of the Arctic be as deep as up to 30 meters, ref. Gudmestad et al., (1999), and may damage the pipeline even if that is trenched below the mudline. Laboratory small scale tests executed to establish qualitative figures of the soil and buried pipe behavior below the gouge are reported in this paper. The tests were conducted at 1g and aimed to visualize the effects of gouging on the soil below and the buried pipe segment. A box (115 × 50 × 40 cm) filled with different types of soils (sand and silty sand) was used for the tests. The model ice keel was made of a steel plate hanging from a wooden frame and mounted on top of the box such that only horizontal translation was allowed. For several of the tests, pipe segments were embedded into the soil. The performed tests indicated the presence of subgouge soil deformations and their dependence of several gouge-related parameters. It was observed that the pipes experienced cyclic movements, being first dragged forward-downwards as the model keel approached the pipeline and then re-bounding when the keel passed over. The tests showed that the maximum pipe displacement decreases exponentially with the pipe burial depth. Naturally formed soil mound in front of the keel during gouging showed to influence vertical pipeline displacement. Furthermore, horizontal pipe movements were larger at lower attack angles of the ice keel. The authors are by no means the first to ponder the subject of subgouge soil deformations and pipeline response. Many researchers have reported their studies before; see e.g. Woodworth-Lynas et al. (1996), Nixon et al. (1996), Yang and Poorooshasb (1997), Phillips et al. (2005) and Konuk et al. (2006). The authors are also fully aware of the challenges related to scaled testing of the soil-structure and do not assume the obtained results to be scaled up. Nevertheless, the reader may find some observations to be of interest while evaluating the present (disputed) approach to the problem.


2002 ◽  
Vol 122 (6) ◽  
pp. 989-994
Author(s):  
Shinichiro Endo ◽  
Masami Konishi ◽  
Hirosuke Imabayashi ◽  
Hayami Sugiyama

Author(s):  
Krum Videnov ◽  
Vanya Stoykova

Monitoring water levels of lakes, streams, rivers and other water basins is of essential importance and is a popular measurement for a number of different industries and organisations. Remote water level monitoring helps to provide an early warning feature by sending advance alerts when the water level is increased (reaches a certain threshold). The purpose of this report is to present an affordable solution for measuring water levels in water sources using IoT and LPWAN. The assembled system enables recording of water level fluctuations in real time and storing the collected data on a remote database through LoRaWAN for further processing and analysis.


2013 ◽  
Vol 14 (2) ◽  
Author(s):  
Noor Fachrizal

Biomass such as agriculture waste and urban waste are enormous potency as energy resources instead of enviromental problem. organic waste can be converted into energy in the form of liquid fuel, solid, and syngas by using of pyrolysis technique. Pyrolysis process can yield higher liquid form when the process can be drifted into fast and flash response. It can be solved by using microwave heating method. This research is started from developing an experimentation laboratory apparatus of microwave-assisted pyrolysis of biomass energy conversion system, and conducting preliminary experiments for gaining the proof that this method can be established for driving the process properly and safely. Modifying commercial oven into laboratory apparatus has been done, it works safely, and initial experiments have been carried out, process yields bio-oil and charcoal shortly, several parameters are achieved. Some further experiments are still needed for more detail parameters. Theresults may be used to design small-scale continuous model of productionsystem, which then can be developed into large-scale model that applicable for comercial use.


Sign in / Sign up

Export Citation Format

Share Document