Sand dune - Auroville Green Practices
Transcription
Sand dune - Auroville Green Practices
Prashant Hedao & Lata Iyer Auroville TN SOURCE: NCGIA, UC Santa Barbara CIESEN, Columbia University Backwaters, Sand Dunes & Mangroves Sand Dunes Sand Dunes PONDICHERRY CHENNAI Sand Dunes Backwaters Backwaters Backwaters Mangroves Sand dune ecosystem Indigenous fringe forests …all of these have suffered as humans move closer to the sea • Grows in water by trapping silt • Needs right combination of salt & fresh water • Roots above water level for aeration SOURCE: UNEP / WCMC Sand dune may be simply defined as a mound or ridge formed by the deposition of sand. These geologic landforms develop when an abundance of sand combines with wind, vegetation and geography SOURCE: Design with Nature by Ian L. Mcharg Established primary and secondary dune Salt Spray is reduced by primary dune and ground level rises Xeric thickets replace dune grass Secondary dune is stabilized. Dune grass is replaced by plants not requiring sand deposition Fringe forests established behind the stabilized secondary dune In case of Tamil Nadu coast it is “Tropical Dry Evergreen Forest” SOURCE: Conservation Science Program, World Wildlife Fund - US SOURCE: USAMS & Survey of India, 1954 Vegetation on Sand Dunes View of Sand Dunes from Agricultural Fields View of Agricultural Fields from top of Sand Dunes • Indegenous / native species should be planted • High tolerance to any disturbance, have built-in defense mechanisms • Low and/or no maintenance once it stabilizes • No threat of attacks by pests • May take longer, but it is worth the wait • Species diversity is the key • Should plant at all levels: (ground covers, shrubs, understory, keystone species) • Less chance of getting wiped out in case of a disease outbreak … this will ensure long term survival of the ecosystem and hence protection to communities RED - 0 – 5 m GREY –above 5m BLUE – Below MSL Characteristics • Very difficult conditions • Very little land available that is 5m above mean sea level (MSL); lot of land is actually below MSL • Therefore ideal for growing paddy as lot of stagnant water is available • All development of residential areas should be in north-south direction • Very important that existing drainage channels are preserved Road SOURCE: Google Earth SOURCE: Pacific Disaster Center, Hawaii / DigitalGlobe SOURCE: Pacific Disaster Center, Hawaii / DigitalGlobe SOURCE: Pacific Disaster Center, Hawaii / DigitalGlobe Garbage Blocking Channels Large Channels but Narrow Culverts Orange Line - Watershed / Catchment Boundary Raised roads act as watershed dividers and block the natural water flow When roads are built in rural areas, they are raised above the surrounding land (to avoid flooding) and normally cut across agricultural fields Over time the road gets “Pucca” . Now because of trapped water natural vegetation thrives there and ground water recharge improves Continued… But after sometime strip development (shops / houses) starts on both sides of the road. People raise their land above the road level. This is to avoid water from entering into their property. Built-up area increases; which results in less ground water recharge and increased surface run-off If the culverts / bridges provided under the road for free flow of water are not large enough or not provided at all, there will be bottle-necks and flooding will result. Water is trapped by the roads and has nowhere to go – hence FLOODING • Higher elevations; NOT in low lying area as it will be prone to flooding • NOT in the natural or man-made drainage channel which may flood in monsoons • NOT on steep slopes that are prone to erosion • NOT on aquifer/Groundwater recharge areas • Should maintain & ensure linkages for livelihood needs, social networks, caste issues and primary / secondary economic networks … all this information should be collected and used in the planning process Not Much Intact Ecosystems in Gangetic Plains SOURCE: Conservation Science Program, WWF-US SOURCE: Conservation Science Program, WWF-US SOURCE: WWF-Nepal & WWF-US Bombay Floods SOURCE: Global Land Cover Facility, University of Maryland / NASA (glcf.umiacs.umd.edu/index.shtml) Thank you [email protected] [email protected]