Loess Soil - Soil of the year 2021
Loess Soil: Soil of the year 2021
Source: BGR
Upon the proposal of BGR loess soil was selected as the soil of the year 2021 by the Advisory board Soil of the Year. BGR, under the patronage of Mrs Elisabeth Winkelmeier-Becker, Parliamentary State Secretary at the Federal Ministry for Economic Affairs and Energy (BMWi), hosted an event on the World Soil Day and organizes further activities on the „Soil of the Year 2021: Loess soil“ .
Loess - dusty gold
Why is loess so special? What are the reasons for loess soils to become so fertile and hence turn them into true natural treasures? How can we preserve loess soils and use them sustainably?
Loess is a predominantly calcareous, homogeneous, pale yellowish sediment that mainly consists of silt-size particles. Silt is finer than sand, but coarser than clay and hence similar to dust. The term loess most probably originates from the Alemannic (Swiss-German dialect) expression Lösch „loose“.
Child of the Ice age
Most of the loess formed during the last ice age between 115 000 to 13 000 years before present. Much of Germany was a cold, tree-less steppe environment, into which glaciers extended from north and south. Glaciers and frost broke down rocks and stones and ground them into mineral dust. The latter was lifted into the air and deposited miles away from the source areas, often on the leeward sides of hills.
In Northern Germany this occurred along the northern fringe of the Central Uplands, today‘s „Börden“ (fertile flatlands) with the Jülich-Zülpicher Börde in the West via the Magdeburger Börde up to the Leipziger Basin and the Saxonian Hills to the East.
In Southern Germany loess was deposited in areas north of the gravel plains of the Alpine rivers, in the Upper Rhine Valley and in the Central Uplands in the wide valleys and basins.
Loess formation in Northern Germany
Source: BGR (after Diercke Weltatlas)
Diversity emerges
Remains of plants form humus that is deeply mixed into loess by soil organisms. When cold winters and summer dryness hamper Humus degradation, Chernozems form. In places where the finest particles of soils - clay particles - are translocated with seepage water into the subsoil, Luvisols form. If topsoil is bleached in this process, Haplic Retisols develop. If seepage water accumulates on top of clay-rich subsoil, Stagnosols and Planosols emerge.
|
The formation of all those soils always starts with a displacement of carbonate deeply into the still unweathered loess. In this process, centimeter-long, rigid concretions may form - the loess dolls.
|
First choice
Easy cultivation and fertile soils have always attracted settlers. In former times such soils were already used for agricultural purposes. This is also known from archeological finds of tools and artifacts from the early Bronze Age, like the Nebra Sky Disc.
The high yield of soils was able to supply many people and thereby contributed to the development of cities. Today, many cities are located in or in the vicinity of loess regions (e.g. Cologne, Magdeburg, Stuttgart). Whenever new construction takes place, precious soil is lost.
|
|
A knight in shining armor
Loess soil is free of stones and very porous. The space between silt particles is just big enough for the loess soil to store and provide water for plant usage and at the same time to be sufficiently conductive. Water may ascend within the soil like within filter paper when plants take up water, and when the rooting area is drier then the root-free zone below. With this, the plant‘s hydric stress during droughts is reduced and the yield increases.
The most water-demanding crops such as sugar beets are therefore preferably cultivated on loess soils. In addition, the rare forest stands on loess profit from a good water supply.
Aside from water, loess soil stores nutrients and contaminants. These can easily adsorb onto the large surface area of the fine soil particles. In this way, nutrients are available for plants.
|
|
| Visualizing flow paths in loess soil using food coloring Source: BGR | |
At the same time, harmful substances may be retained in the soil, which leads to a protection of our groundwater. In order not to overstress the soil and its filter capacity, the infiltrated substances have to be biodegradable. Degradation is performed by microorganisms. Their high activity level in loess soils contributes to a rapid turnover of undesired substances.
A sensitive soul
With all these advantages: such a loess soil is highly sensitive. The material was supplied by the wind, and may as well be (re-)taken away with it - or be easily washed away by water.
|
As loess may not be formed without a new ice age, we need to conserve it. The best protection against erosion is a year-round vegetation cover and as many hedges and trees as possible.
But what can we do if something is lying under the precious soil that we also want to exploit, such as lignite in many places? If after lignite mining the previously removed loess is reapplied with a sophisticated method, we can succeed in regaining vast landscapes for usage.
On these recultivated areas soils redevelop and fulfill important functions for the ecosystem and landscape hydrology.
Loess soil is worth it - because of its excellent features and manifold functions, as a soil it is a
... true jack of all trades.
Generell infomation about the soil of the year can be found here. The BGR webpage also provides information on most of the soils selected in previous years (in German only). Further information can be found on the webpage of the Advisory board Soil of the Year (in German only).
Downloads:
|
|
Contact