Phase 2 of the Hidden Crisis fieldwork is underway – right on schedule. The work has started in Ejere, a Woreda about 100 km north of Addis in Ethiopia. In this major survey of 50 poorly functioning rural waterpoints, we spend two days dismantling and testing each water point to work out what the main […]
The physical sciences longitudinal studies have kicked off in Uganda this week. The aim of these longitudinal studies is to capture the time-based hydroclimatic and hydrogeological processes of the groundwater system at selected hand pumped boreholes (HPBs). These temporal datasets provide valuable information to understanding HPB functionality that could not be addressed from the two […]
A comprehensive and efficient environmental monitoring network has been set up for the study area collecting relevant, timely and cost-effective data on rainfall, river flow and groundwater level and recharge. Data will be used in the development and running of a Groundwater Risk Management Tool, which will include a hydrogeological model. The model will be able to simulate and predict the effects of different levels of extraction and rainfall on the system, helping Kwale County to make plans to ensure that it has a good and sustainable water supply for people and industry.
The project is making use of data on temperature, rainfall, humidity, air pressure, wind speed and direction from a number of automatic weather stations (AWS) installed in the project region. Much of the instrumentation has been provided by the Trans-African Hydro Meteorological Observatory (TAHMO) project, hosted in this region by Kenya Meteorological Services.
River Flow Monitoring and Measurement
To understand the amount of water available in rivers and dams in the study area, various water level and discharge monitors have been installed. In particular, streamflow on the Mukurumudzi and Ramisi Rivers is being monitored to determine the water balance of the rivers at different points, enabling the researchers to understand and model groundwater inputs along these water courses.
River monitoring has been a great example of cooperation between project partners. As well as the existing staff gauge used by WRMA and Base Titanium to monitor flow in the Mukurumudzi River, the project has installed automatic water level loggers (Heron Logger) at two locations on the Mukurumudzi ((3KD06 – Shimba Hills – upstream and Irrigation Intake Works near Bomani Shopping Centre – downstream) and one on the Ramisi River at Eshu Bridge. These are complemented with manual staff gauges provided by WRMA Sub-regional Office in Mombasa. The instruments and staff gauges were installed jointly with WRMA/WRUA, Base Titanium, KENHA and the community. Flow in Ramisi River used to be monitored at Mwachande Bridge (3KD01) stage gauge by WRMA but the gauge has been vandalized and is not in operation.
River Cross Section and Topographical Survey
A topographical survey was carried out at the river flow monitoring points at the Irrigation Intake Works (on the Mukurumudzi River) and at Eshu Bridge (on the Ramisi River) and measurements of cross section of the river were taken.
The information will be used to facilitate flow measurement and permit the researchers to develop a Flow Rating Equation and Curve for each site, a key element of the hydrological model.
Surveyors and Survey Equipment at Eshu Bridge during cross section and topographical survey, May 2016 Cross-section of 3KD06 Weir on Mukurumudzi River, Shimba Hills. The figure below is the result of the river cross-section survey at the weir where water
flow is monitored and estimated for the Mukurumudzi River (by Base Titanium, WRMA
and Gro for Good) to aid water resources planning and decision-making. The weir structure also enables the consented abstraction of water by Shimba Hills Community Water Supply project which provides water to Shimba Hills shopping centre and its environs.
The chemical composition of groundwater provides useful information about the flow of water into and through the underground aquifers. Chemical and biochemical analysis also allow us to monitor substances which affect the safety and taste of drinking water. Three groundwater sampling campaigns have now been completed, involving the collection and analysis of water from open wells, rivers, handpumps and deep boreholes.
The first campaign was in September 2015 (wet season after the short rains; 81 sampling sites), the second was in March 2016 (dry season, fewer points sampled due to some wells/boreholes being dry) and the final sampling campaign in June 2016 at the end of the wet season (long rains), thus providing information about seasonal variation in water quality and on the process by which the aquifers are recharged following rain. A total of 43 groundwater sites are under fortnightly monitoring for groundwater static level, pH, temperature and conductivity.
Sample pH, electrical conductivity, temperature, dissolved oxygen and redox potential (ORP) were measured during fieldwork using a flow cell so that the water did not come into contact with air. Other parameters analysed in situ were alkalinity, ammonia levels and faecal bacteria. Samples were also taken to Spain for laboratory analysis to indicate major ions, trace metals, water isotopes (deuterium and oxygen 18) and Total Organic Carbon.
Only very few points contained ammonia, nitrates or trace metals. However, most of the open wells contained high levels of faecal bacteria. The results will be explained in detail in the next newsletter.
by Julius Odida, PhD candidate, University of Nairobi
Geophysical methods (ground-based physical sensing techniques) are used to provide information about sub surface geology. The Gro for GooD project is using both electrical resistivity tomography (ERT) and vertical electric sounding (VES) to identify and characterize the aquifers (water-saturated sub-surface rocks) which lie beneath Kwale County. Over the past year, a number of geophysical surveys have been conducted by a team from University of Nairobi, WRMA and Rural Focus Ltd. The study involved four phases: planning/desktop studies, reconnaissance, actual data acquisition and report writing. Lower resistivity may indicate water saturation and/or fracture zones in the rock. We present a preliminary interpretation of some results below.
by Prof. Dan Olago, University of Nairobi in Gro for Good newsletter 2 2016
Welcome to the second edition of our project newsletter. There has been a lot of activity in recent months including: the completion of the installation and commissioning of the climate and hydrological monitoring network; two groundwater sampling campaigns in March and June; geophysical surveys to define the aquifer geometry and structure using both electrical resistivity tomography (ERT) and vertical electric sounding (VES) approaches; an anthropological survey related to determinants of use/non-use of the shallow wells installed with smart hand-pumps; compilation of a list of data sets for the project; and stakeholder engagement, both within the county and with stakeholders such as the Kenya Meteorological Department (KMD) and Water Resources Management Authority (WRMA) at the national level. I will, however, here focus on the geophysical surveys.
The project team has been collaborating with WRMA personnel in carrying out the geophysical survey. The WRMA kindly made its ABEM SAS1000 Terrameter available to enable this exercise to proceed. The ERT surveys which were carried out in three phases in December 2015, January 2016 and May 2016 are now completed. The VES survey which started in mid July will be completed in early August. The main aim of the geophysical survey is to get a better handle on the aquifer geometry and structure, with a focus on where geological understanding is poor, and to delineate the shallow and deep groundwater systems. The outcomes of this activity will provide critical inputs to the hydrogeological flow model that is already under development. This model will be integrated into the groundwater risk management tool to promote improved groundwater governance balancing economic growth, groundwater sustainability and poverty reduction, and taking into account the competing demands for domestic, agricultural and industrial uses of the resource.
The fieldwork has not been without incident; some unknown person cut off and went away with about 70m of cable and this slowed down the working pace, and we had to take on more local personnel to guard the cable layout to avoid any further losses. Heavy rains at times also meant that work had to be delayed or stopped altogether on some days. Overall, these incidents notwithstanding, it has been a great team building experience. The daily interaction between the team members fostered valuable knowledge exchanges and lifelong skills enhancement in geophysical surveying.
By: Obed Minkah
Final fieldwork activities in Dodowa included the establishment of monitoring network which consist of 40 wells to monitor groundwater fluctuation and to help us determine the groundwater flow direction. In order to know the groundwater flow direction, the monitoring wells were levelled to each other using a total station. It was daunting task to level wells scattered on about a 13.5kmsq area but the task was done within 3 days with support from my colleagues (Isaac and Eric) from The Hydrological Services Department. The water levels of these wells were also measured weekly to know the groundwater levels change over time and from the monitoring it was observed that water levels in the wells were decreasing gradually over the course of fieldwork.
Obed working during the levelling of the monitoring wells
Continue reading Finalising Obed’s fieldwork in Dodowa
By: Carlos Enrique Aponte Rivero on T-group.science
Yes! It is very interesting for these kids, obviously amazed by the strange equipment put into the water. As soon as I started to set up the probes and to do the water quality measurements, I was suddenly surrounded by children, getting closer and closer trying to find out what is this about. It was in Osunyai Street, where I took a sample from a borehole close to Sombetini Primary School. The children are students of this school and they were just walking around when I arrived to continue with my data collection. The T-GroUP Project gave me the opportunity to mix my technical background in chemistry and water quality with social science, an exciting challenge with an interesting experience working in the field.
By: Shona Jenkins (from t-group.science)
By the end of February, I will have spent 3 weeks conducting interviews with community members, community leaders and representatives from the local government across 11 communities in Dodowa. Throughout the interview process, I have attempted to better understand the water reality in each community: what sources of water are used and for what purpose(s) and how this impacts their day-to-day lives. As the interviews progress, I have tried to identify pressing problems in each community, which sometimes includes access to water and quality of water, but is not always the most pressing issue identified. As the interviews conclude, I have tried to gain a better understanding of whom community members look to for solutions to pressing community issues and I have tried to identify both formal and informal actors in each community who are critical in undertaking any community improvement project.