Wetlands
Wetlands (Kinyarwanda terms, “Ibishanga n’ibibaya” or “ubutaka buhehereye”) play a vital role in maintaining water resources and are part of the green infrastructure of healthy catchments. They protect water quality, maintain water supplies by replenishing rivers and streams during the dry season, and more importantly, reduce the risk of flooding, sequester carbon and play many critical roles in Rwandan ecosystems. In addition, Rwandan wetlands offer habitat for a vast array of biological diversity that cannot survive elsewhere.
Number of wetlands
935
Surface area
5176 337 ha
RAMSAR site
Rugezi wetland
Wetlands Buffer Zone
20m
Wetlands are classified according to characteristics such as soil type, vegetation, hydrology and climate zone.The biggest wetlands are floodplain wetlands of low altitude associated with major lakes such as Lake Cyohoha, Rweru, Mugesera, Nasho, and rivers, such as Nyabarongo, Akanyaru, Mukungwa, Base, Nyabugogo, among others.
Despite their importance, some wetlands in Rwanda face pressure from inappropriate forms of agriculture (uncontrolled fertilizers and pesticides), soil erosion, peat extraction, illegal mining, illegal infrastructure, pollutants from industrial wastewater discharge (organic waste, pathogens and heavy metals) among others. Wetlands degradation and pollution has a significant impact on water quality and quantity. The declining capacity for wetlands to provide critical ecosystem services has resulted in increased flooding – and attendant damage to infrastructure, lives, reduced productivity, and silting of water bodies.
Climate change, coupled with population growth, are additional threats to wetlands and freshwater resources. Therefore, sustainable practices which support healthy wetlands to perform their functions and provide goods and services to sustain human life, are therefore coming to the fore. Rwanda has shown commendable political will and taken tangible actions to address wetlands degradation and unsustainable use of water resources.
Rwanda recognizes the importance of wetlands and the need to manage them proactively. For example, current legislation classifies wetlands into total protected wetlands, or non-protected wetlands . The latter category is further divided into those with status of use under specific conditions, and those with a status of use without conditions.
These conditions are documented in the Prime Minister’s Order gazetted in 2017, which lists all swamp lands, their characteristics, boundaries and determining modalities of their use, development and management
To ensure sustainable utilisation of wetlands:
Description and Facts
Both natural processes and human activities, including the methane exploitation, lead to changes in Lake Kivu. Such changes could potentially increase the risk of a gas eruption, they could deteriorate the water quality and lake ecological integrity, or they could negatively affect the methane exploitation. The lake monitoring aims at detecting such changes as early as possible before they develop into larger problems. The lake management and methane exploitation strategy can then be adapted to either avert a negative development, or at least to reduce its negative
impacts.
Created in 2008 with the operationalization of KPI (Kibuye Power One) pilot plant, Lake Kivu Monitoring Programme (LKMP) was a special entity within “Energy Development Corporation Limited” of the Rwanda Energy Group (REG). In 2021 Lake Kivu monitoring activities were transferred in Rwanda Environment Management Authority (REMA) after the government decision under the Official Gazette n° 32 bis of 19/10/2020 that compose the Division of Environment Analytics and Lake Kivu Monitoring. LKMP has been mandated to monitor the impact of methane gas extraction on the Lake by protecting the Lake’s stability, its environment and by ensuring that the socio-economic benefit to the population is maximized. The concession for Methane Gas extraction today has been granted to different companies mainly for electricity production and other uses. Companies are Kivuwatt, Shema Power Lake Kivu Ltd, Gasmeth, Magma Energies Ltd. Currently, only Kivuwatt is operational with 26 MW electricity production since 2015 other operators are expected to start soon.
For that, Lake Kivu monitoring activity under REMA ensures that methane gas operators comply with the Managements Prescriptions for Development of Lake Kivu Gas Resources (MPs), which is a set of prescriptions developed by a group of international experts on Lake Kivu for the sustainable and environmentally friendly Methane gas extraction.
Environment analytics and Lake Kivu monitoring (EA&LKM) division collaborate on regular basis with international, region and local research institutions to promote research on Lake Kivu by developing a strong and effective research network on Lake Kivu.
Objectives of Lake monitoring
Lake Kivu is an ancient rift lake. Around 12 000 years B.P., lavas flow from the Virunga volcanoes dammed its former outflow to the Nile. By 9 500 years B.P., Lake Kivu had become a deep lake with an overflow via the Ruzizi River to Lake Tanganyika. The lake became strongly stratified about 5 000 years B.P. when volcanism and hydrothermal activities began.
Only 31 fishes species live in Lake Kivu. The Tanganika sardine (Isambaza) was introduced in the 1960s, to fill the empty pelagic zone. The Isambaza sustain traditional fisheries and is an important source of protein for the local population. The food web of Lake Kivu is simple: phytoplankton are eaten by zooplankton, which are fed by Isambaza fish.
Catchment area: 5097 km 2 (excluding the Lake), relatively small compared to the Lake surface.
5 Basins around Idjwi Island: Main Basin, Kalehe Basin, Ishungu Basin, Bukavu Bay and Kabuno Bay.
Rivers: ~200 small inflowing rivers, but no surface water in the volcanic region of Goma Internal sub-aquatic springs: in the north, at different depths mainly at 180 and 250 m. Annual Lake level fluctuations: 0.17 to 1.17 m
The water column is characterized by increasing temperature, salinity, and gas concentrations with depth and by several sharp gradients resulting from subaquatic springs. The annual deep mixing occurs during the dry season (June to September). The mixing depth varies annually but is limited to a maximum depth of 70 m. Below this oxygenated zone, the different layers are homogenous and stable. Lake Kivu is therefore permanently stratified.
Carbon dioxide: ~300 km 3 STP, 80% of the gases volume, only 20% of the total gas pressure. Methane: ~60 km 3 STP, 20% of the gases volume, but 80% of the total gas pressure.
These gases are dissolved and trapped below 260 m depth, where they accumulated over ~800 years. This unusual accumulation can be explained by the lake’s permanent stratification and the input of carbon dioxide from the surrounding volcanoes. CO 2 has a magmatic origin. CH 4 is generated biologically by the reduction of magmatic CO 2 (~65%) and the mineralization of organic carbon (~35%).