Ondiri Wetland

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Ondiri Wetland or Ondiri Swamp is a protected wetland and peatbog that is the source of the Nairobi River near Kikuyu, Kenya in Kiambu County. [1] [2] The wetland is under pressure because of water extraction, deforestation and accelerated erosion. [1] [3] Listed in 2021, the project's conservation is part of a larger initiative by the Kenyan government to reduce pollution to major waterways that provide water supply to Nairobi as part of the Thwake Dam project. [4] [5] [6] The waterway is also important for local greenhouse agriculture. [4] Ondiri Wetland covers 3,713,549 square feet and is a source to 40 springs, which provide water to the local community. [7]

Ondiri was heavily polluted with pesticides and dumping. In 2004, a study found as few as 41 bird species. [8] Around 2020, there were 76 species of birds living in Ondiri. [9] In 2016, the Friends of Ondiri Wetland Kenya (FOWK) was established to rehabilitate and protect the bog; they run awareness campaigns, plant trees, and hold community events. . [9] "The biggest challenge I face is convincing people about the importance of the wetland. And in awareness creation, you convert polluters into consververs," says David Wakogi, co-creator of this FOWK in a documentary about his work. [10] Wakogi says there are now 76 species of birds in the wetland, [11] compared to a 2004 assessment of 44 species. [12]

Kenya's 2022 national celebration of World Wetland Day was held in Ondiri to highlight the importance of the country's largest highland bog. [7] "More than 10,000 seedlings have been planted in the swamp through efforts of Kenya Forest Service (KFS) and NEMA. I am happy to report that the survival rate of the seedling is very impressive,” stated Cabinet Secretary for Environment and Forestry Mr Keriako Tobiko.

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<span class="mw-page-title-main">Swamp</span> A forested wetland

A swamp is a forested wetland. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates periodic inundation or soil saturation. The two main types of swamp are "true" or swamp forests and "transitional" or shrub swamps. In the boreal regions of Canada, the word swamp is colloquially used for what is more formally termed a bog, fen, or muskeg. Some of the world's largest swamps are found along major rivers such as the Amazon, the Mississippi, and the Congo.

<span class="mw-page-title-main">Peat</span> Accumulation of partially decayed vegetation

Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. Sphagnum moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. Soils consisting primarily of peat are known as histosols. Peat forms in wetland conditions, where flooding or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity.

<span class="mw-page-title-main">Wetland</span> Land area that is permanently, or seasonally saturated with water

A wetland is a distinct ecosystem that is flooded or saturated by water, either permanently for years or decades or seasonally for a shorter periods. Flooding results in oxygen-free anoxic processes prevailing, especially in the soils. The primary factor that distinguishes wetlands from terrestrial land forms or water bodies is the characteristic vegetation of aquatic plants, adapted to the unique anoxic hydric soils. Wetlands are considered among the most biologically diverse of all ecosystems, serving as home to a wide range of plant and animal species. Methods for assessing wetland functions, wetland ecological health, and general wetland condition have been developed for many regions of the world. These methods have contributed to wetland conservation partly by raising public awareness of the functions some wetlands provide. Constructed wetlands are designed and built to treat municipal and industrial wastewater as well as to divert stormwater runoff. Constructed wetlands may also play a role in water-sensitive urban design.

<span class="mw-page-title-main">Fen</span> Type of wetland fed by mineral-rich ground or surface water

A fen is a type of peat-accumulating wetland fed by mineral-rich ground or surface water. It is one of the main types of wetlands along with marshes, swamps, and bogs. Bogs and fens, both peat-forming ecosystems, are also known as mires. The unique water chemistry of fens is a result of the ground or surface water input. Typically, this input results in higher mineral concentrations and a more basic pH than found in bogs. As peat accumulates in a fen, groundwater input can be reduced or cut off, making the fen ombrotrophic rather than minerotrophic. In this way, fens can become more acidic and transition to bogs over time.

<span class="mw-page-title-main">Bog</span> Type of wetland with peat-rich soil

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<i>Chamaecyparis thyoides</i> Species of plant

Chamaecyparis thyoides, a species of Cupressaceae, is native to the Atlantic coast of North America and is found from southern Maine to Georgia and along the Gulf of Mexico coast from Florida to Mississippi. It is one of two species of Chamaecyparis found in North America. C. thyoides resides on the East Coast and C. lawsoniana can be found on the West Coast. There are two geographically isolated subspecies, treated by some botanists as distinct species, by others at just varietal rank: Chamaecyparis thyoides thyoides and Chamaecyparis thyoides henryae (H.L.Li) E.Murray The species grows in forested wetlands where they tend to dominate the canopy. The trees are associated with a wide variety of other wetland species because of their wide north-south range. The remaining populations are now found mostly in remote locations that would be difficult to harvest, so its popularity as a source of lumber has decreased.

The Green Belt Movement (GBM) is an indigenous grassroots organization in Kenya that empowers women through the planting of trees. It is one of the most effective and well-known grassroots organisations addressing the problem of global deforestation. Professor Wangari Maathai established the organization in 1977 under the auspices of the National Council of Women of Kenya (NCWK). GBM's successes in forest conservation, education, and women's economic empowerment have gained the organisation worldwide acclaim. It is also noted for its advocacy of human rights, democratisation of access to public lands, and environmental justice issues such as the role of women's traditional ecological knowledge in addressing environmental degradation and desertification.

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<span class="mw-page-title-main">Aberdare Range</span> Mountain range in Kenya

The Aberdare Range is a 160 km (99 mi) long mountain range of upland, north of Kenya's capital Nairobi with an average elevation of 3,500 metres (11,480 ft). It straddles the counties of Nyandarua, Nyeri, Muranga, Kiambu and Laikipia. The mountain range is located in west central Kenya, northeast of Naivasha and Gilgil and lies just south of the Equator. The mountain range is called Nyandarua among the Agikuyu people in whose territory this forest and mountain range is located. The name Nyandarua comes from the Kikuyu word rwandarua meaning a drying hide, due to the distinctive fold of its silhouette.

<span class="mw-page-title-main">Nairobi River</span> River in Kenya

The Nairobi River is a river that flows across Nairobi, the capital city of Kenya. It is the main river of the Nairobi River Basin, with several parallel streams flowing eastward. All of the Nairobi basin rivers join east of Nairobi and meet the Athi River, which eventually flows into the Indian Ocean. The rivers are mostly narrow and highly polluted, though recent efforts to clean the rivers have improved water quality.

<span class="mw-page-title-main">Kiambu County</span> Place in Kenya

Kiambu County is a county in the former Central Province of Kenya. Its capital is Kiambu and its largest town is Thika town. Kiambu County is the second most populous county in Kenya after Nairobi County. Kiambu County borders Nairobi and Kajiado Counties to the South, Machakos to the East, Murang'a to the North and North East, Nyandarua to the North West, and Nakuru to the West. It has a population of 2,417,735.

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<span class="mw-page-title-main">Carska Bara</span> Largest individual bog in Serbia

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<span class="mw-page-title-main">Freshwater biology</span> The scientific study of freshwater ecosystems and biology

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<span class="mw-page-title-main">Wetland conservation</span> Conservation of wet areas

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Tatu City is a 5,000 acres (2,000 ha) special economic zone (SEZ) located 20 kilometres (12 mi) North of Nairobi Central Business District (CBD) in the Ruiru Municipality area of Kiambu County. It sits within the greater Nairobi Metropolitan region and is a flagship project of the Kenya Vision 2030 blueprint.

References

  1. 1 2 "Friends of Ondiri Wetland Kenya | Home". friendsofondiriwetlands.org. Retrieved 2021-07-27.
  2. Obura, Fredrick. "Increased human activities threaten source of Nairobi River - FarmKenya Initiative". Farm Kenya Initiative. Retrieved 2021-07-27.
  3. Muchiri, Nancy W. (2012). The impact of human activities on Wetlands: a case study of Ondiri Wetland in Kiambu County, Kenya (Thesis thesis). University of Nairobi, Kenya.
  4. 1 2 "Saving Kenya's Capital City Water Source, The Ondiri Wetland". Africa Climate Conversations. 19 July 2021. Retrieved 2021-07-27.
  5. Mugo, George (25 July 2021). "Ondiri Wetland water levels rises after fencing". The Star. Retrieved 2021-07-27.
  6. Koech, Gilbert. "Ondiri Swamp to be gazetted soon, says Nema". The Star. Retrieved 2021-07-27.
  7. 1 2 "The World Wetlands Day held at Ondiri Swamp". Kenya News. February 3, 2022. Retrieved Aug 26, 2022.
  8. Mungai, Naftali. "Why resource rich Ondiri Swamp must be conserved". The Standard. Retrieved 2022-08-26.
  9. 1 2 May 21, 2020, Thursday (2020-09-19). "Greening Ondiri, the resource-rich Old Lake". Business Daily. Retrieved 2022-08-26.{{cite web}}: CS1 maint: numeric names: authors list (link)
  10. Wetland Warrior | 52 Documentary , retrieved 2022-08-26
  11. Wetland Warrior | 52 Documentary , retrieved 2022-09-07
  12. Mungai, Naftali. "Why resource rich Ondiri Swamp must be conserved". The Standard. Retrieved 2022-09-07.