Titlebook: Ecology of a Glacial Flood Plain; J. V. Ward (former Head of Limnology),U. Uehlinger Book 2003 Springer Science+Business Media Dordrecht 2

不容置疑

Channel Typology,sensu Junk et al., 1989) is widely recognized as the major force structuring floodplain habitat conditions, even moderate increases in discharge (“flow pulses”) may result in dramatic expansion of inundated area and can be important in sustaining habitat heterogeneity in river flood plains (Tockner et al., 2000).

恃強凌弱

Thermal Heterogeneity,incoming stream flow and losses by radiation or latent heat exchange (Webb & Zhang, 1997). Heat budgets depend on the regional climate and local characteristics such as riparian vegetation, aspect, channel morphology, stream water-groundwater interactions and hydrology (Constanz, 1998; Gu et al., 1998; Hawkins et al., 1997; Ward, 1985).

看法等

Litter Decomposition,le in the litter dynamics of low elevation streams, tropical streams in particular (Flecker, 1996). In concert with various chemical changes, micro-organisms cause transformations in litter quality (e. g., increases in nitrogen and phosphorus concentrations) that influence decomposition dynamics (Webster & Benfield, 1986; Gessner et al., 1999).

自制

,Beendigung des Arbeitsverh?ltnisses,second order glacial stream that flows in a north-northeast direction before it joins the Bernina River near the village of Pontresina. The Roseg valley is part of the catchment of the Inn River, which is the major Alpine tributary of the upper Danube.

遺留之物

embolus

Val Roseg: A High Alpine Catchment,second order glacial stream that flows in a north-northeast direction before it joins the Bernina River near the village of Pontresina. The Roseg valley is part of the catchment of the Inn River, which is the major Alpine tributary of the upper Danube.

過分

Nutrient Limitation,now-cover and low nutrients limit primary production in most stream types in winter (Robinson et al., 2002). Nutrient dynamics also change longitudinally along the main channel because of the increase in tributary and groundwater inputs as one moves downstream (Malard et al., 1999; Tockner et al., 2002).

捏造

irreparable

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