Übersetzung für "Lösslehm" in Englisch

The loess loam is generally only about 1 to 1.5 m thick.

The dry Riesling "loess loam" from Oetinger Gutswein shimmers in a delicate shade in the glass.

The vines, which are managed with reduced yields, are rooted on easily heatable soils with loess loam.

The grapes for this white wine come from vines, which are rooted on soils with loess loam.

The fracture zone opening here into the basin from the south, the "Idsteiner Senke" (hollow), is locally known along the Emsbach, which empties into the Lahn, by the name "Goldener Grund" (“Golden Ground”), a reference to the favourable climate and fruitful soil (loess).

In the subsurface are the layers of the Muschelkalk period, on the wide open spaces of layers of the Lower Keuper and are partially covered by loam.

In the area of the Vienna River, there are also loess, and loess loam soils, particularly in the part of Margareten.

The soils of the forest at the Vorskla developed on different parent materials, especially on the loam, which is found in the eastern half of the forest.

The fracture zone opening here into the basin from the south, the Idsteiner Senke (hollow), is locally known along the Emsbach, which empties into the Lahn, by the name Goldener Grund (“Golden Ground”), a reference to the favourable climate and fruitful soil (loess).

The soils of the cultivated areas are just as diverse: from limestone to clay to loess clay, the characteristics of the soil shape the wines produced here and make them incomparable.

The bedrock is coarse, calcareous conglomerate of the Hollenburg-Karlstetten formation and is covered mostly by calcareous, but finely grained, silty clay loess and loess-loam.

Often, these ways have steep walls of loess loam – and sometimes you can find there small snails from the ice age (about 10.000 years old).

The steep southeast slope is characterized by a large number of light and coarse soils of loess clay and weathered sandstone, which give the Riesling a very complex character and a dense structure.

The bedrock is a coarse, calcareous conglomerate, which is mostly covered by calcareous, fine grained loess –derived loam.

The vines are rooted in sandy loess clay with lime, which, in combination with the existing microclimate, gives rise to wines with an extraordinary character.

Loessic loam contains relatively few clayey ingredients (fluxes), owing to which fact our bricks naturally obtain the porous structure after burning.

Advantageous is the addition of clay, bark humus and soluble lean clay.

The loess loam in Table I had a water content of 20.0% and was therefore oversaturated with water.

The middle and deep stony-gritty soils are composed of sericite gneiss with additions of loess loam.

The ice age loess-loam on the plateau of the "Ostrauer Scheibe" enabled the establishment in former times of a German village for seven farmsteads.

It can be seen from Table II that the kf values with riverside loam and flood loam overall are somewhat better than when loess loam is used (Table I).

Good compaction of the soil is given up to a Proctor density of 95%, that is to say the loess loam is easily processible mechanically at water contents of 13.8 to 21.2%.

To demonstrate the favorable influence of dry sludge, in comparison with wet sludge, on the shrinkage behavior of cohesive soils, two parallel test series were conducted, on the one hand with a fine-sandy loess loam with a grain size distribution according to the Figure (originating from Bochum-Kornharpen), and on the other hand with clay from a clay pit at Hunxe with a grain size distribution according to the Figure, specifically, in each case, with TS 90 sludge and TS 30 sludge.

Thus, for example, loess loam (see Table I, lines 4 and 7/8), with a water content of 16.7%, has a shrinkage of 6.7% by volume which, with a water content of 20.0%, rises to 10.1% by volume.

With the loess loam oversaturated with water, mechanically compactible, plastically deformable bodies were obtained by the addition of 10% by weight of dry sludge (KS-TS 90), calculated on sludge dry substance and in relation to soil dry substance.