Translation of "Bodenbildung" in English

Diagnostic properties are typical results of soil-forming processes or reflect specific conditions of soil formation.

Terrestrial soils are differentiated according to their respective determining soil formation processes.

For actual bottom formation, the part being folded is provided with glue before folding.

Here, however, a bottom formation is emerging.

A bottoming-out and self-stabilisation of the economic cycle are not in sight.

The soil formation processes described above determine the grain size composition of mineral soil particles.

Soil erosion is a major part of the process of soil formation at the hillslope scale.

This imperils natural 'services' such as soil formation for food production or pest control.

Soil composition and formation are considered to be dependent on the existence and activities of this diverse community of soil organisms.

The following examples illustrate the essential role played by these organisms in the humus and soil formation process:

But recent data support the view that the housing sector could be in the process of establishing a bottom, albeit an elongated one.

As the climate cooled, soil formation slowed down, and a flora and fauna that would, millions of years later, be familiar to the first human inhabitants began to emerge.

As soil formation is an extremely slow process, soil can be considered essentially as a non-renewable resource.

Where the relevant information is available, a Member State may instead use the following definition: ‘At risk of soil erosion’ shall mean any plot with a predicted loss of soil exceeding the rate of natural soil formation, whether or not anti-erosion measures (e.g., soil cover or crop rotation) have been taken on it.

Soil formation is a very slow process (it takes centuries to build up a centimetre), so soil sealing causes significant damage to soil and often results in permanent loss.

From a geomorphological standpoint, there is a distinction made between steilhänge not simply on the basis of their gradient and rock type, but especially on their aspect (i.e. their orientation), their rotundity or roughness (small shapes, flexion, steps, terraces, drainage etc.), the vegetation on the mountainsides or hillsides and the soil formation.

However, basically, the zig-zag steps according to the invention for the bottom formation open up new possibilities for the production of envelopes, bags, and shipping pouches.

After the filling process is conducted through the open end of the bottom 2, the bottom end 2 can be closed off as part of the filling process by a simple folded, rolled up or similar bottom, without the formation of the bottom being complicated by the side folds 20 and 21.

Given the very slow rate of soil formation, any soil loss of more than 1 tonne per hectare per year can be considered as irreversible over a time span of 50–100 years.

Paper bags, e.g., for packaging cement or other powdered or granular materials of high solidity, are manufactured of multilayered tube sections, the individual layers of which are glued together at their edges during the formation of the tube, wherein the individual layers lie on top of one another at the ends of the paper bags such that their cut edges are aligned (straight cut) or preferably only overlap one another in a partially staggered formation, so that the layers are also glued together individually during the formation of the base of the bag.

Due to Glacier Peak's proximity to Image Lake, volcanic ash is quite common in the area, and plays a major role in the formation of soil.