scholarly journals Icing phenomena for managed aquifer recharge (MAR) and it’s feflow simulation result

2019 ◽  
pp. 16-31
Author(s):  
Nasanbayar N
Keyword(s):  
Groundwater Recharge ◽  
Water Availability ◽  
Water Source ◽  
Managed Aquifer Recharge ◽  
Cold Period ◽  
Early Winter ◽  
Aquifer Recharge ◽  
Winter Cold ◽  
Recharge Rates ◽  
Natural Recharge

Ulaanbaatar, the capital of Mongolia, shows a highly dynamic urban and industrial development, with a strong increase of population. Thus, water demand is continuously rising while water availability is in general low and less reliable. The semi-arid and cold environment shows a high variability in precipitation and river discharge, with a general tendency towards decreasing water availability due to increasing air temperatures and thus rising potential evaporation. In parallel with the city’s development, the extended groundwater aquifer shows a clear decline, and the groundwater levels drop significantly. Therefore, a groundwater management system based on managed aquifer recharge is proposed and a strategy to implement these measures in the Tuul valley is presented. In this study considered enhancement of natural recharge rates during the early winter cold period, an increase of groundwater recharge through creating ice storages, due to keep water source as in ice form on surface. In dry season March to May ice storage recharge surface and groundwater by melting where Tuul River is non-flow condition. In this paper also written matlab icing code in water supply wells location, limited and unlimited area. The study of icing was processed in feflow simulation scenarios for artificially recharging groundwater resources.In this study considered feflow simulation scenarios for artificially recharging groundwater resources like enhancement of natural recharge rates during the early winter cold period, an increase of groundwater recharge through creating ice storages, due to keep water source as in ice form on surface, drainage canal recharging aquifer from opposite side, constructing underground dam that accumulates groundwater behind. The result shown that one of the possibilities recharge groundwater in dry season is icing method which creates ice sheets over ice and build ice storages in winter, keep water in ice form.

scholarly journals Evaluation of MAR Methods for Semi-Arid, Cold Regions

Water ◽  
2019 ◽  
Vol 11 (12) ◽  
pp. 2548 ◽  
Author(s):  
Nasanbayar Narantsogt ◽  
Ulf Mohrlok
Keyword(s):  
Water Reservoir ◽  
Managed Aquifer Recharge ◽  
Capital City ◽  
Ice Storage ◽  
Aquifer Recharge ◽  
Dry Period ◽  
Groundwater Aquifer ◽  
Recharge Rates ◽  
Semi Arid ◽  
Natural Recharge

Mongolia is a semi-arid, highly continental region with highly variable precipitation and river discharge. The groundwater aquifer located near Ulaanbaatar, the capital city of Mongolia, is the only one source for city water supply consumption, and it is important to ensure that groundwater is available now and in the future. The main watercourse near the capital city is the Tuul River, fed by precipitation in the Khentii Mountains. The semi-arid and cold environment shows high variability in precipitation and river discharge. However, due to absence of precipitation in winter and spring, the riverbed usually runs dry during these times of the year, and weather observations show that the dry period has been extending in recent years. However, in parallel with urban development, the extended groundwater aquifer has shown a clear decline, and the groundwater levels have dropped significantly. Therefore, a groundwater management system based on managed aquifer recharge is proposed, and a strategy to implement these measures in the Tuul River valley is presented in this paper. This strategy consists of the enhancement of natural recharge rates during the wet summer from the northern drainage canal, an additional increase in groundwater recharge through melting the ice storage in the dry period, as well as the construction of underground dams to accumulate groundwater and a surface water reservoir that releases a constant discharge in the outlet. To increase natural recharge rates of groundwater during the early dry period through the melting ice storage period, the MATLAB icing code, which was written for ice storage for limited and unlimited areas, was considered through finite element subsurface FLOW (FEFLOW) simulation scenarios as a water source in ice form on the surface. A study of the artificial permafrost of underground as an ice dam was processed in FEFLOW simulation scenarios for accumulating groundwater resources. The results of these artificial recharging methods were individually calculated, combined, and compared with the surface reservoir, which releases a constant discharge through the dam. In this paper, new ideas are presented involving managed aquifer recharge—MAR methods, and include application to aufeis, a mass of layered ice for groundwater recharge by melting. Additionally, the accumulation of groundwater using artificial permafrost is used as an underground dam. In addition, was considered recharging scenario only with constant release water amount from water reservoir also with all MAR methods together with reservoir combination.

Focused groundwater recharge in a dryland environment: hydrometric and isotopic evidence from central Tanzania

2020 ◽  
Author(s):  
David Seddon ◽  
Japhet J. Kashaigili ◽  
Richard G. Taylor ◽  
Mark O. Cuthbert ◽  
Lucas Mihale ◽  
...  
Keyword(s):  
Groundwater Recharge ◽  
Surface Waters ◽  
Poverty Alleviation ◽  
Managed Aquifer Recharge ◽  
Sub Saharan Africa ◽  
Aquifer Recharge ◽  
Ephemeral Stream ◽  
Groundwater Levels ◽  
Sub Saharan ◽  
Semi Arid

<p>Groundwater, and its replenishment via recharge, is critical to livelihoods and poverty alleviation in drylands of sub-Saharan Africa and beyond, yet the processes by which groundwater is replenished remain inadequately observed and resolved. Here, we present three lines of evidence, from an extensively-monitored wellfield in central semi-arid Tanzania, indicating focused groundwater recharge occurring via leakage from episodic, ephemeral stream discharges. First, the duration of ephemeral streamflow observed from daily records from 2007 to 2016 correlates strongly (R<sup>2</sup> = 0.85) with the magnitude of groundwater recharge events observed and estimated from piezometric observations. Second, high-resolution (hourly) monitoring of groundwater levels and stream stage, established in advance of the 2015-16 El Niño, shows the formation and decay of groundwater mounds beneath episodically inundated adjacent streambeds. Third, stable-isotope ratios of O and H of groundwater and precipitation as well as perennial and ephemeral surface waters trace the origin of groundwater to ephemeral stream discharges. The identification and characterisation of focused groundwater recharge have important implications not only, locally, for protecting and potentially augmenting replenishment of a wellfield supplying the capital of Tanzania through Managed Aquifer Recharge but also, more widely, in understanding and modelling groundwater recharge in dryland environments.</p>

scholarly journals Recycling water in U.S. cities: understanding preferences for aquifer recharging and dual-reticulation systems

Water Policy ◽  
2019 ◽  
Vol 21 (6) ◽  
pp. 1207-1223 ◽  
Author(s):  
David J. Hess ◽  
Brandi M. Collins
Keyword(s):  
Water Supply ◽  
Groundwater Recharge ◽  
Power Plants ◽  
Potable Water ◽  
Water Source ◽  
Water Supply Systems ◽  
Aquifer Recharge ◽  
Recycled Water ◽  
Water Supplies ◽  
Supply Systems

Abstract Recycling of effluent water from urban water-supply systems is often a more sustainable water source than increased use of surface sources, groundwater sources, and desalination. However, water-supply organizations (WSOs) often do not take full advantage of recycled water. Although recycling water for direct potable use is efficient, public concern with safety has tended to cause WSOs to favor other uses for recycled water. This study examines patterns in the degree of utilization of two main indirect uses of recycled water: dual-reticulation systems and groundwater recharge. Drawing on case studies of four U.S. cities that are leaders in the use of recycled water, the study identifies conditions that favor the choice of one option over the other. Where cities are concerned with groundwater recharge of potable water supplies, they tend to prefer non-recycled water if available for recharge projects. However, where non-recycled water supplies are limited, recycled water may be prioritized for aquifer recharge. Otherwise, the preference is for use by large industrial partners such as power plants or for exchanges for higher-quality potable water resources with rural systems. In contrast, dual-reticulation (purple-pipe) systems for direct nonpotable recycling face steep economic and technical challenges.

scholarly journals Monitoring and modeling infiltration-recharge dynamics of managed aquifer recharge with desalinated seawater

2016 ◽  
Author(s):  
Yonatan Ganot ◽  
Ran Holtzman ◽  
Noam Weisbrod ◽  
Ido Nitzan ◽  
Yoram Katz ◽  
...  
Keyword(s):  
Numerical Model ◽  
Groundwater Recharge ◽  
Multiple Scales ◽  
Pressure Sensors ◽  
Managed Aquifer Recharge ◽  
Analytical Models ◽  
Low Permeability ◽  
Aquifer Recharge ◽  
Groundwater Levels ◽  
Infiltration Rates

Abstract. We study the relation between surface infiltration and groundwater recharge during managed aquifer recharge (MAR) with desalinated seawater in an infiltration pond, at the Menashe site that overlies the northern part of the Israeli Coastal Aquifer. We monitor infiltration dynamics at multiple scales (up to the scale of the entire pond) by measuring the ponding depth, sediment water content and groundwater levels, using pressure sensors, single-ring infiltrometers, soil sensors and observation wells. During a month (January 2015) of continuous intensive MAR (2.45 · 106 m3 discharged to a 10.7 hectare area), groundwater level has risen by 17 m attaining full connection with the pond, while average infiltration rates declined by almost 2 orders of magnitude (from ~ 11 to ~ 0.4 m d−1). This reduction can be explained solely by the lithology of the unsaturated zone that includes relatively low-permeability sediments, whereas clogging processes at pond-surface – abundant in many MAR operations – are negated by the high-quality desalinated seawater or negligible compared to the low-permeability layers. Recharge during infiltration was estimated reasonably well by simple analytical models, whereas a numerical model was used for estimating groundwater recharge after the end of infiltration. It was found that a calibrated numerical model with a one-dimensional representative sediment profile is able to capture MAR dynamics, including temporal reduction of infiltration rates, drainage and groundwater recharge. Measured infiltration rates of an independent MAR event (January 2016) fitted well to those calculated by the calibrated numerical model, showing the model validity. The successful quantification methodologies of the temporal groundwater recharge are useful for MAR practitioners and can serve as an input for groundwater flow models.

Community finance and promotion of Managed Aquifer Recharge systems affect uptake and sustainability as a potable water source in southwest coastal Bangladesh: A qualitative study

2020 ◽  
Author(s):  
Fosiul A. Nizame ◽  
Fosiul Alam Nizame ◽  
Md. Abu Naser ◽  
Afsana Sharmin ◽  
Tania Jahir ◽  
...  
Keyword(s):  
Water Quality ◽  
Drinking Water ◽  
Qualitative Study ◽  
Saline Water ◽  
Water Source ◽  
Managed Aquifer Recharge ◽  
Water Infiltration ◽  
Drinking Water Source ◽  
Primary Concern ◽  
Aquifer Recharge

Abstract Background In the south-western coastal region of Bangladesh ground water, normally used for drinking, is excessively saline. Increased salinity in drinking water can have a range of adverse health impacts. Managed aquifer recharge (MAR) systems, which infiltrate rainwater and fresh pond water into aquifers, are adaptive strategies to deliver low-saline water to the affected communities. Several MAR systems have been piloted in these regions. The MAR pilot study demonstrated the potential for increasing freshwater availability and sustainable year-round drinking water supplies. The objective of this study was to identify MAR system management shortcomings and strengths to provide recommendations that are applicable for future MAR systems and engineering driven water management methods in low-income countries.Methods A qualitative study among the 18 pilot MAR communities with access to MAR systems since 2010 was conducted to assess perceptions of drinking MAR water and usage patterns. We conducted in-depth interviews (24), key informant interviews (2) and focus group discussions (3).Results More than half (13) of the respondents reported that drinking saline water causes diarrhea, dysentery, gastritis, digestive or abdominal disorders none described impact on blood pressure. More than two thirds (13/18) of current MAR users reported MAR as their preferred drinking water source. Almost half (11) reported that they were familiar with MAR but don’t understand how it works. A majority of respondents (17) considered MAR water safe because they thought there are no germs present. Nonetheless, respondents mentioned several problems including dissatisfaction with water quality (salinity/iron/smell/dirt in the water), and management (MAR sites found locked for most of the day). MAR installation and management staff and technical supervisors and caretakers thought that water quality was hampered by irregular water infiltration. They reported that management and maintenance issues were their primary concern, which were impeded by limited funds, as users do not pay regularly.Conclusions Though there is a demand for drinking water from MAR systems, the concerns about management related to finance, in addition to the amount collected are the greatest threat to system functionality and sustainability, which requires community-based solutions that will provide regular oversight and maintenance.

Managed aquifer recharge: the widening gap between law and policy in India

2015 ◽  
Vol 15 (6) ◽  
pp. 1159-1165 ◽  
Author(s):  
P. Sakthivel ◽  
L. Elango ◽  
S. Amirthalingam ◽  
C. E. Pratap ◽  
N. Brunner ◽  
...  
Keyword(s):  
Groundwater Recharge ◽  
Water Policy ◽  
Tamil Nadu ◽  
Rainwater Harvesting ◽  
Legal Framework ◽  
Managed Aquifer Recharge ◽  
Groundwater Depletion ◽  
Aquifer Recharge ◽  
Indian States ◽  
Law And Policy

The past decade has witnessed discussions on various options to overcome groundwater depletion, such as rainwater harvesting (RWH) and ‘artificial recharge’ methods. This paper addresses law and policy issues relating to managed aquifer recharge (MAR). Based on an analysis of the National Water Policy of India and water polices and laws of the Indian states, a concrete case study, namely Chennai metropolitan area, has been studied in detail. The city of Chennai and the State of Tamil Nadu provide a favorable atmosphere for groundwater recharge, making, e.g. RWH mandatory. However, the legal framework does not support more systematic approaches towards MAR and the administrative praxis does not ensure that groundwater recharge is offset by an increase of illegal groundwater extraction.

scholarly journals Monitoring and modeling infiltration–recharge dynamics of managed aquifer recharge with desalinated seawater

2017 ◽  
Vol 21 (9) ◽  
pp. 4479-4493 ◽  
Author(s):  
Yonatan Ganot ◽  
Ran Holtzman ◽  
Noam Weisbrod ◽  
Ido Nitzan ◽  
Yoram Katz ◽  
...  
Keyword(s):  
Numerical Model ◽  
Groundwater Recharge ◽  
Multiple Scales ◽  
Pressure Sensors ◽  
Managed Aquifer Recharge ◽  
Analytical Models ◽  
Low Permeability ◽  
Aquifer Recharge ◽  
Groundwater Levels ◽  
Infiltration Rates

Abstract. We study the relation between surface infiltration and groundwater recharge during managed aquifer recharge (MAR) with desalinated seawater in an infiltration pond, at the Menashe site that overlies the northern part of the Israeli Coastal Aquifer. We monitor infiltration dynamics at multiple scales (up to the scale of the entire pond) by measuring the ponding depth, sediment water content and groundwater levels, using pressure sensors, single-ring infiltrometers, soil sensors, and observation wells. During a month (January 2015) of continuous intensive MAR (2.45  ×  106 m3 discharged to a 10.7 ha area), groundwater level has risen by 17 m attaining full connection with the pond, while average infiltration rates declined by almost 2 orders of magnitude (from  ∼  11 to  ∼  0.4 m d−1). This reduction can be explained solely by the lithology of the unsaturated zone that includes relatively low-permeability sediments. Clogging processes at the pond-surface – abundant in many MAR operations – are negated by the high-quality desalinated seawater (turbidity  ∼  0.2 NTU, total dissolved solids  ∼  120 mg L−1) or negligible compared to the low-permeability layers. Recharge during infiltration was estimated reasonably well by simple analytical models, whereas a numerical model was used for estimating groundwater recharge after the end of infiltration. It was found that a calibrated numerical model with a one-dimensional representative sediment profile is able to capture MAR dynamics, including temporal reduction of infiltration rates, drainage and groundwater recharge. Measured infiltration rates of an independent MAR event (January 2016) fitted well to those calculated by the calibrated numerical model, showing the model validity. The successful quantification methodologies of the temporal groundwater recharge are useful for MAR practitioners and can serve as an input for groundwater flow models.

scholarly journals Creating collaboration for contentious projects on managed aquifer recharge: two cases from Finland

2021 ◽  
Author(s):  
Vuokko Laukka ◽  
Tapio S. Katko ◽  
Lasse Peltonen ◽  
Riikka Rajala
Keyword(s):  
Water Source ◽  
Managed Aquifer Recharge ◽  
Aquifer Recharge ◽  
Know How ◽  
Authentic Dialogue ◽  
Stakeholder Workshop ◽  
Considerable Resistance ◽  
Joint Knowledge Production ◽  
Management Approaches ◽  
Multiparty Interaction

AbstractIn Finland, community water supply has increasingly relied on natural groundwater and artificially recharged groundwater as the raw water source. Several managed aquifer recharge (MAR) projects have been co-created with involved parties and have proceeded well, while some cases have raised considerable resistance among the stakeholders. It seems that success or failure in MAR cooperation is related to management cultures and the ways in which various interests are taken into account, from the very beginning and throughout the process. Empirically, this paper builds on comparison between two conflictual case studies in Finland: one in the Tampere region and the other in the Turku region. The study analyses the major constraints of these projects through the lens of collaborative rationality, also drawing upon discourse analysis and negotiation theory. The material is gathered through thematic interviews of stakeholders, newspaper articles and a stakeholder workshop. The results indicate that conventional management approaches, drawing from expert-based instrumental rationality, were insufficient in both cases. The collaborative rationality framework suggests that legitimacy for the groundwater projects should be gained through joint knowledge production and inclusive multiparty interaction for creating options for collaboration. Both cases lacked the tools and know-how for authentic dialogue and collaboration. The emerging paradigm emphasizes more collaborative approaches for natural resources management and urban planning. While MAR projects operate inside these areas and are highly complex in nature, it is essential to embrace the emerging paradigm in order to promote MAR systems along with their huge potential.

Sign in / Sign up

Export Citation Format

Share Document