Sentence examples for main inflow from inspiring English sources

To retain the nutrients from the lake, the Kis (small -Balaton Water Protection small -Balaton Wateresigned on the lower Protectione main inflow, the River Zala.

The main inflow to the North Sea consists of Atlantic water following the 200 m depth contour north of Shetland before passing along the western edge of the Norwegian Trench (Fig. 1) with a smaller flow, the Fair Isle Current, following the 100 m depth contour (Fig. 1).

The results illustrated that the sources that contributed the most to the faecal contamination at the water intake in Lake Rådasjön were the discharges from the on-site sewers and the main inflow to the lake – the river Mölndalsån.

ODP 1123 provides a record of sediment drift deposition under the Deep Western Boundary Current, the main inflow of deep water to the Pacific Ocean since the Early Oligocene, though a major hiatus spans the late Early Oligocene to the Early Miocene.

◦ High-resolution measurement of the nitrate-N concentrations and flow rate at the main inflow of the Zeulenroda reservoir (Laewitz gauging station).

For this purpose, the results of the main inflow performance relations (IPR), i.e., Vogel (1968), Standing (1971) and Fetkovich (1973), have been compared with field data and the Vogel equation (i.e., correlation 2) eventually resulted in the best match, used as the IPR relationship.

The upper section of the eastern boundary is Gate Up Gill, one of the main inflows of Grimwith Reservoir.

Groundwater discharge constitutes the main water inflow of many coastal wetlands.

The main water inflow into the system occurs at points W1, T1 and MK1 as shown in Fig. 1.

The main water inflow into the basin is through the Waipawa, the Makeretu and the Tukituki rivers, in addition to rainfall within the basin.

Samples of the dominating macrophyte of the littoral zone (Cyperus laevigatus) and allochthonous plant detritus particles from the main river inflow (River Njoro) were collected for stable isotope analysis to evaluate the contribution of non-pelagic sources to the planktonic food web.