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首页> 外文期刊>Estuarine Coastal and Shelf Science >Hydromorphic to subaqueous soils transitions in the central Grado lagoon (Northern Adriatic Sea, Italy)
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Hydromorphic to subaqueous soils transitions in the central Grado lagoon (Northern Adriatic Sea, Italy)

机译:格拉多泻湖中部(北亚得里亚海,意大利)的从水状到水下的过渡

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摘要

The Grado lagoon is among the largest in the Mediterranean sea and is characterized by salt marshes, where tides influenced the development of a complex micromorphology coupled to a micromosaic of vegetation covers. This study represents the first contribution to the understanding of the main processes governing formation, development and spatial transitions between hydromorphic and subaqueous soils in an Adriatic lagoon ecosystem. Physicochemical characteristics and development of soils were investigated in three salt marshes differing for their proximity to the open sea, textural composition and age of formation. Soils of back barrier salt marshes had A/C profiles and were mostly characterized by a sandy coarse texture that allows rapid drainage and subsurface oxygen exchanges. Soil sequences from the inner salt marsh to its submerged border slope or to a brackish waterhole do not simply represent a hydrosequence, but also reflect erosion/sorting/accumulation processes.
机译:格拉多泻湖是地中海最大的泻湖之一,其特征是盐沼,潮汐影响了复杂的微观形态与植被植被的微马赛克的发展。这项研究代表了对理解亚得里亚泻湖生态系统中水状土壤与水下土壤之间形成,发展和空间转换的主要过程的理解的第一贡献。在三个盐沼中研究了土壤的理化特性和土壤的发育,这些盐沼与公海的距离,质地组成和形成年龄不同。背屏障盐沼的土壤具有A / C剖面,其主要特征是沙质粗糙的质地,可以快速排水和进行地下氧交换。从内部盐沼到其淹没的边界坡或到一个咸淡的水坑的土壤序列不仅代表着水力序列,而且还反映了侵蚀/分选/蓄积过程。

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