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首页> 外文期刊>Aquatic Botany >Responses of a fringing Cyperus papyrus L. swamp to changes in water level.
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Responses of a fringing Cyperus papyrus L. swamp to changes in water level.

机译:边缘莎草纸莎草沼泽对水位变化的响应。

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Over a 9-year period (1993-2001), the land-water width of a papyrus fringe on the southern shore of Lake Naivasha, Kenya, varied between 40 and 60 m. Increases in width via rhizome spreading into open water followed the 1997/1998 El Nino flood when water depths rose by about 2 m. Germination of papyrus seeds also responded to water depth with a mean+or-S.E. rate in experiments of 23+or-6% after 21 days when water level was 5 cm below the sediment surface. No germination occurred when sediment was flooded or allowed to desiccate. Rhizome spreading from floating mats appeared to be favoured by deep water with seedling spread favoured on newly inundated, low-gradient slopes in shallow water. Although natural regenerative capacity was influenced by water depth, the height, density, biomass and chemical content of papyrus were not. Total average biomass along a land-water transect was 6950+or-860 g m-2 which was large in relation to nutrient and mineral contents. Culms contained 0.47+or-0.14% N and 0.06+or-0.05% P and rhizomes 0.71+or-0.21% and 0.10+or-0.06%. Sediment underlying the swamp was aerobic and there were small land-water gradients in the BOD of swamp water and sediment. However, chemical gradients were weak compared with wider papyrus swamps elsewhere. Lake and swamp water mixed in the narrow fringe studied and residence times for organic matter may not have been long enough for organic material to mineralise before entering lake water..
机译:在9年期间(1993年至2001年),肯尼亚奈瓦夏湖南岸的纸莎草边缘的陆地水宽在40至60 m之间变化。 1997/1998年的厄尔尼诺洪水之后,由于水深增加了约2 m,通过根茎传播到开阔水域,宽度增加了。纸莎草种子的萌发对水深也有平均值+或-S.E. 21天后,当水位低于沉积物表面5 cm时,实验中的水蒸气流量为23+或6%。当沉积物被淹没或使其干燥时,没有发芽发生。从浮垫上蔓延的根茎似乎受到深水的青睐,而在浅水区新近被淹没的低坡度的斜坡上,幼苗的传播受到了青睐。尽管自然再生能力受水深的影响,但纸莎草的高度,密度,生物量和化学含量不受影响。陆地-水样断面的平均总生物量为6950+或-860 g m-2,相对于养分和矿物质含量而言很大。茎中含有0.47+或-0.14%N和0.06+或-0.05%P和根茎0.71+或-0.21%和0.10+或-0.06%。沼泽下面的沉积物是好氧的,沼泽水和沉积物的生化需氧量中的土地水梯度很小。但是,与其他地方的纸莎草沼泽相比,化学梯度较弱。湖水和沼泽水混合在狭窄的边缘中,有机物的停留时间可能不足以使有机物质在进入湖水之前矿化。

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