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Evaluation of Contaminant Mixing in Rainwater Harvesting First Flush DivertersMechell, Justin K. 14 January 2010 (has links)
As the world population increases, the demand increases for quality drinking
water. The harvesting of rainwater has the potential to assist in alleviating pressures on
current water supplies and storm water drainage systems. Diversion of a portion of the
collected water away from storage is a technique used to improve harvested rainwater
water quality prior to storage. Six configurations of a downspout first flush diverter
were constructed and tested in the laboratory. The configurations of diverters were
evaluated for their affinity to allow diverted water in the diverter chamber to interact
with the flow of water to storage. Experiments were conducted at flow rates ranging
from 0.76 L/min to 113.56 L/min. This range of flow rates adequately represents a wide
range of common storm intensity patterns across the United States to which downspout
first flush diverters are subjected.
The diverter chamber to downspout transition fittings tested on a 10.16 cm
diameter diverter chamber, upward and downward oriented sanitary and straight tee, do
not have a significant impact on the mean difference in initial and final total dissolved
solids concentrations observed at multiple sample ports. No statistical difference was observed when comparing upward and downward oriented sanitary tees used as diverter
chambers to downspout transition fittings on 10.16 and 15.24 cm diverter chambers.
Utilizing a straight tee as a transition fitting with a floating ball, acting as a barrier
between water collected in the diverter chamber of a downspout first flush diverter and
the flow passing through the transition fitting, limited diverted water from interacting
with the subsequent flow of harvested rainwater. There is not a significant difference
between the use of a downspout first flush diverter with diverter chamber diameters of
10.16 and 15.24 cm utilizing upward and downward oriented sanitary tees as downspout
to diverter chamber transition fittings. Tests at flow rates less than or equal to 12.11
L/min exhibited limited changes in total dissolved solids concentrations in the
downspout first flush diverters with 15.24 cm diameter diverter chambers. Tests at flow
rates less than or equal to 1.51 L/min exhibited limited changes in total dissolved solids
concentrations in the downspout first flush diverters with 10.16 cm diameter diverter
chambers. The diverter chamber drain flow rate and volume impacts the observed
differences in initial and final TDS concentrations at all sample ports on the diverter
chamber of a downspout first flush diverter regardless of flow rate. The diverter
chamber drain flow rate impacts the flow rate of water entering the diverter chamber
through the transition fitting.
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ASSESSING THE RELIABILITY OF ROOFTOP RAINWATER HARVESTING FOR DOMESTIC USE IN WESTERN KENYAMundia, Clara 01 May 2010 (has links)
In many developing countries, the stress of rapidly growing populations, mismanagement of resources and changing climate has created a burden on already compromised water resources. In Africa, where a significant proportion of the population is without access to improved water source, the urgency for clean available water sources to sustain healthy and productive human and natural populations has become a priority. As a water scarce country, Kenya has seen an increased investment in rainwater harvesting (RWH) projects to harness the vastly untapped rainwater resource, particularly in rural areas. Most of RWH literature is centered on the potential and implementation of rainwater harvesting systems, however not much focus has been placed on examining the demand satisfaction of these systems. This study investigates the reliability of rooftop rainwater harvesting (RRWH) as a key priority source of water supply for domestic use in three towns in Western Kenya: Kisumu, Nakuru and Lodwar. This was done using two approaches (1) the fraction of time water was available and (2) the fraction of time that a minimum demand was met, with acceptable reliability of 0.95 or higher. Actual rainfall data and RRWH parameters were used to produce supply/demand simulations of the system under Constant-Demand and Responsive-Demand scenarios over ten years. It was observed that all towns achieved acceptable reliability values for RRWH in terms of water availability however Lodwar only achieved demand satisfaction below 0.95. This study concluded that though RRWH cannot satisfy the minimum demand requirement through all days of the year, it is more than able to provide an alternative water supply for the domestic household in periods of long dry spells or when primary water source are inadequate.
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Tank sizing from rainfall records for rainwater harvesting under constant demandAllen, Jacqueline Elsa 17 April 2013 (has links)
M.Ing. (Civil Engineering Science) / In recent years, there has been an international trend towards installing rainwater tanks in an attempt to save water. However, there are no clear guidelines for determining the optimal size of such a tank in South Africa. This study investigates the possibility of simplifying the process of sizing a rainwater tank for optimal results. It utilises daily data from four rainfall stations, namely Kimberley, Mossel Bay, Punda Maria and Rustenburg, obtained from the South African Weather Services. The water use is considered to be for indoor purposes only, therefore assuming a constant daily demand to be extracted from the tank. The required size of a rainwater tank is influenced by the MAP, the area of the roof draining into the tank, the water demand (both the average demand and seasonal variations), the desired reliability of supply, and the rainfall patterns. The first step in simplifying the process is to consolidate the above variables. The tank volume is expressed as the number of days it could supply the average daily water demand. Another variable is created which provides the ratio of the total water volume which could theoretically be harvested from the roof in an average year, to the total water demand, from the tank, for a year. This has the effect of consolidating the MAP, the roof area, the water demand and the tank volume into two variables only and eliminates the need to consider numerous demand values. Using simulations over 16 years for each location, the relationships between these variables were determined to ensure 90%, 95% and 98% assurance of supply.
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Controls on the geochemistry of speleothem-forming karstic drip watersTooth, Anna F. January 2000 (has links)
Research was performed at Crag Cave, Castleisland, southwest Ireland, and P8 Cave, Castleton, Derbyshire, in order to determine the main factors responsible for modifying rainwater geochemistry during flow through soil and karstic aquifer zones. Monitoring was performed on a daily basis in summer and winter at Crag Cave, and on a monthly basis over one year at P8 Cave. At both sites, biannual peaks in karst system Ca2+concentrations occurred due to: (i) promotion of microbial C02 production by increased summer temperatures, and (ii) retardation of gaseous exchange by ponding of elevated winter rainfall input leading to an unseasonable build up in soil zone C02. Therefore, speleothems at both sites may form biannual bands in hydrological years subject to elevated winter rainfall input. In addition to variations in carbonate weathering due to fluctuations in C02 levels, cation yields in Crag Cave matrix soil water were controlled by dolomite dissolution (Mg2+), plant uptake (K+), and evapotranspiration balanced by enhanced winter marine aerosol input (Na+). Strontium isotope analysis indicates that S~+ was derived from a 50:50 silicate/carbonate mixture, whilst the relatively light 313C signal was related to direct evolution of C02 into the aqueous phase in waterlogged pores. Within the Crag Cave aquifer variations in karst water geochemistry were controlled by dilution, flow switching, prior precipitation of calcite and dolomite dissolution along the flow path. Strontium isotope analysis indicates that dissolution in the aquifer dominated, with S~+ being sourced from a 25:75 silicate/carbonate mixture. Light karst water 313C values were constrained by the supply of light soil gas to the aquifer. Elevation in the Mg/Ca and Sr/Ca ratios in the Crag Cave speleothem record compared to present day analogues indicates that the former Holocene climate was drier, whilst heavier 87Sr/86Srratios and 813C values suggest variation in soil hydrology over time.
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RainScapesDaily, Cado, Wilkins, Cyndi 02 1900 (has links)
2 pp. / RainScapes are the ultimate in water efficient landscaping. RainScapes are beautiful landscapes that once established rely entirely on rain and stormwater (gray water too if available)while preserving tap water for indoor and drinking water needs.
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Harvesting Rainwater for Landscape UseWaterfall, Patricia January 2006 (has links)
56 pp. / Second Edition, October 2004 / In the arid Southwest, rainfall is scarce and evapotranspiration rates are high. Only natives and some desert-adapted plants can live on 10 or 11 inches of annual rainfall. Other plants require some supplemental irrigation and harvesting rainwater can reduce the use of drinking water for landscape irrigation. This publication discusses the water requirements for some plants and the way to collect rainwater. Its topics include:
- Water Harvesting System Components
- Simple Water Harvesting System Design and Construction
- Complex Water Harvesting Systems
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The effect of polyacrilamide based soil conditioners on structural sealing at sub-process levelSimmons, Robert William January 1998 (has links)
No description available.
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The promotion of rainwater harvesting as a supplementary source of domestic water in Kigali, Rwanda- A feasibility studySully, Robert Peter 14 February 2007 (has links)
Student Number : 7336898 -
MSc (Eng) research report -
School of Civil and Environmental Engineering -
Faculty of Engineering and the Built Environment / Theme and Context
Despite being the source of two of Africa’s greatest rivers, the Nile and the Congo,
Rwanda is a water scarce country and 50% of the citizens of the capital, Kigali, do not
have access to safe drinking water. Rwanda’s tragic history of violent social upheaval
combined with regional macro-economic factors and the effects of globalization have
made this tiny country one of the poorest on the African continent.
Aim and Objectives of this Study
The aim of this report is to establish the value that Rainwater Harvesting holds as a
supplementary water source for the city of. To evaluate this potential intervention, the
suitability of the climate for the harvesting of rainwater is reviewed as well as the
availability of the required resources and the effect that the prevailing social environment
may have on an implementation program.
The current developments in the practice of Rainwater Harvesting are researched and
ways in which Rainwater Harvesting could be utilized are explored as well as the
possible impediments that might be encountered.
Scope and Methodology Adopted
The scope of the report includes:
1. Providing an overview of the country both geographically as well as socially.
2. Establishing the need for alternative water sources by:
a. Reviewing the present water supplies for the city particularly with regard
to their vulnerability to the rapid environmental degradation being
experienced within the country,
b. Reviewing the prevailing water/health nexus.
3. Investigating metrological records, specifically rainfall patterns, and the quality of
the statistics.
4. Review international trends and research in rainwater harvesting specifically in
poor countries.
5. Considering obstacles to implementing a wide-ranging scheme to harvest
rainwater.
The methodology adopted includes:
1. Reviewing published research on the subject of Rainwater Harvesting
techniques and implementation.
2. Attending symposia on the subject.
3. Meeting with water practitioners both in the public sector as well as in NGOs
to establish the current status of water availability, quality and consumption.
4. Conducting on-site research into water sourcing problems in and around
Kigali.
5. Designing, sizing and costing hypothetical installations suitable for local
conditions.
Summary of Main Findings, Conclusions and Recommendations
Although the climate and topography are very favorable to the use of Rainwater
Harvesting, this report finds that the promotion of Rainwater harvesting is just one of
a number of possible interventions which should be pursued in order to improve the
availability of water to the citizens of Kigali
The cost and sophistication of Rainwater Harvesting schemes vary considerably but
at the lower end of the scale the technology would be affordable to most Kigali
residents and the community has the potential human resource to be trained to
execute the work. Obstacles to this approach include ignorance about the safety of
storing water, the comparative low cost of municipal water the perception that water
collection is the responsibility of a family’s women and children. This report also
found that a household using a Rainwater Harvesting scheme is likely to require
some supplementary water on occasions. Furthermore, as the potential to catch
sufficient water is a function of the ratio of a dwelling’s roof area to the number of
inhabitants, its efficacy is limited in densely inhabited poor communities.
Strong leadership and coordination would be necessary for a successful wideranging
Rainwater Harvesting implementation project. In addition a coordinated
educational programme will have to be conducted to dispel myths about stored water and to create the required skills base. The statutes and bylaws regarding water
would also have to be reviewed to avoid legal impediments.
This report concludes that rainwater harvesting cannot be relied upon to fulfill all the
communities’ water needs but it can go a long way to improving the general access
to safe water and in so doing reduce the time and labour presently demanded,
mainly of women and children, in the carrying of heavy loads of water.
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Contour ridge modelling using fuzzy logic and process based approaches for improved rainwater harvestingMhizha, Alexander January 2017 (has links)
A thesis submitted to the Faculty of Engineering and the Built Environment, University of the Witwatersrand, Johannesburg, in fulfilment of the requirements of the degree of Doctor of Philosophy.
Johannesburg, February 2017 / Rainwater harvesting is used as a way of improving crop yields in rain fed agriculture by
capturing excess rainfall and storing it in-situ or in reservoirs for use during dry spells.
Contour ridges are one of the many rainwater harvesting technologies that are used
although little is known about their effectiveness. Contour ridges harvest runoff generated
in the cropped field upstream of the ridges.
The traditional contour ridge type in Zimbabwe was introduced by the government in the
1950s to control soil erosion through safely draining away runoff from cropped fields and
is commonly referred to as graded contour (GC) ridges. In the 1990s the country
experienced severe and more frequent droughts leading stakeholders to experiment on
contour ridges that retain the runoff instead of draining it away which are known as dead
level contour (DLC) ridges. There was therefore the need to find out if there are benefits
derived from this change and assess conditions under which benefits would be
experienced. Previous studies have shown that rainwater harvested by contour ridges
can improve water availability in downstream fields. However these studies did not
investigate the conditions under which such benefits are realised. In addition no attempt
to model water harvesting by contour ridges have been made in Zimbabwe while the
contour ridges are widely being used for soil and water conservation. This research
investigated the effect of contour ridges by comparing soil moisture between plots with
DLC and GC ridges using plots with no contours as a control.
Experimental work was carried out in Zhulube, in Matebeleland South Province of
Zimbabwe. Matebeleland South Province falls within the semi-arid area in which rainfall
is characterised by mid-season dry spells leading to frequent crop failure. In addition, the
area often receives high rainfall intensities leading to soil erosion and sedimentation of
rivers. DLC and GC ridges were constructed in farmers’ fields where maize crops were
planted. Soil moisture measurements were done using a micro gopher soil moisture
profiler while runoff plots were used to measure runoff generation. A fuzzy model was
developed using data from this experiment and a previous study in Masvingo Province of
Zimbabwe to simulate runoff generation at field scale while a process based water
balance model was also developed to simulate soil moisture changes within the root zone
of the cropped area.
The results from this study indicate that DLC are effective in clay and loamy soils where
runoff generation is significant and not in sandy soils due to insignificant generation of
runoff under the rainfall regimes of semi-arid areas. Fuzzy logic was found to be a useful
method of incorporating uncertainty in modelling runoff at field scale. A mass water
balance model developed on process based principles was able to model soil moisture
in the root zone reasonably well (NSE =0.55 to 0.66 and PBIAS=-1.3% to 6.1%) and could
help to predict the water dynamics in contour ridged areas as would be required in
determining the suitable dimensions and spacing of contour ridges. Further research is
required to improve the fuzzy component of the model for estimation of runoff when more
data becomes available. In addition experiments to validate methods of estimating macro
pore fluxes and lateral transfer of water from the contour ridge channel to the downslope
field are also recommended. The model structure can be improved by adopting the
representative elementary watershed approaches to include momentum and energy
balances in addition to mass balance that was used in this study. / MT2017
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Consumption of Rainwater and Diarrheal Disease in Children Under Five in the Dominican Republic from 2002 to 2007Mpogui, Andrea 07 August 2012 (has links)
Background: With the MDG 7 target deadline approaching to halve the global population lacking access to improved water and sanitation by 2015, many nations find the need to explore alternative water sources. Rainwater may be a viable alternative water source. However, there have been concerns raised in recent decades as to the quality of rainwater harvested for potable use.
Methods: Data from the Demographic and Health Surveys database which included 50,579 household surveys between 2002 and 2007 from the Dominican Republic were examined. STATA 8 was used for data analysis. Descriptive statistics were computed, and logistic regression analysis was used to compare toilet type, water source, and type of place of residence with prevalence of diarrheal disease in children under five.
Results: This study found that rainwater presents less risk for diarrheal disease when compared to all other water sources (excluding bottled water). In 2002, people who consumed all other sources of water (excluding bottled) were 1.28 times more likely to have diarrhea in children under 5 (95% CI 1.05-1.57) compared to those who consumed rainwater. They were 1.33 times more likely to have diarrhea in children under 5 (95% CI 1.08-1.65) in 2007 and 1.31 times more likely in both years combined (95% CI 1.13-1.51).
Discussion: This study concluded that consuming rainwater presents a decreased risk for diarrheal disease compared to all other sources (excluding bottled water). More studies are needed to add more evidence to the existing literature regarding health risks associated with rainwater consumption.
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