3.1.2.2 - Desert energy and sediment budgets
Trace the energy and sediment that connect desert slopes, channels, fans and dunes, then use a defined sediment cell and budget to explain changing stores.
Energy enables different processes
Insolation supplies energy to heat rock and soil. Temperature changes create stresses that can contribute to weathering, and solar heating drives atmospheric circulation. Wind transfers kinetic energy to loose grains; movement starts only when force overcomes resistance from grain weight, cohesion, moisture or vegetation. Strong wind over a surface with no available sand need not produce large sand transport.
Runoff gains energy from gravity as water moves down a slope. During a short storm, discharge and flow velocity can rise rapidly, enabling erosion and transport of coarse material. A channel can therefore do much geomorphic work during a few floods despite being dry most of the year. Energy varies through time and space, so average annual rainfall alone cannot predict the amount of sediment moved.
Sources, transfers and sediment cells
Weathering breaks rock down in place and supplies fragments. Mass movement transfers them downhill under gravity. Wind or water erosion entrains material, transport moves it, and deposition occurs where carrying capacity falls. These steps can be separated in time: weathered debris may remain on a slope for years before a flood transports it to a fan, where later wind removes sand-sized particles.
Sediment cell
A defined area within which sediment sources, stores and transfer pathways are connected. Its boundaries help distinguish internal transfers from inputs and outputs.
A basin-scale cell may include mountain sources, channel stores, an alluvial fan and a playa. At a smaller dune-field boundary, sand entering from that fan is an input. Moving sand between two dunes is an internal transfer, not a new input. Boundaries can be permeable: windblown dust may leave even when surface drainage is closed.
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