4.7 Article

Responses of grassland ecosystem carbon fluxes to precipitation and their environmental factors in the Badain Jaran Desert

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Summary: Mega-dunes in the lake group area of the Badain Jaran Sand Sea in China are taller and have steeper slopes compared to those in the non-lake group area. The study proposes a conceptual model suggesting that moisture exchange between lakes and soil via non-rainfall water could explain the formation of abnormally tall dunes in the lake group area. This research provides new insights into the basis of dune formation and groundwater utilization in deserts.

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