Improvement House: Change Your Garden

Improvement House: Change Your Garden

The bottom around a house has been a long time before the new owner is being abused. It may be that the ground has been pressed around the foundation to prevent sagging of the finished house. Excavators or trucks can be compacted. It is therefore not surprising that grass is difficult in the thin layer of breeding that is brought back after construction. Also the years of ordinary use make for compaction. Children or adults walk through the lawn, even if the soil is wet. The continuous discharge of the lawn mower along with chemical fertilization causes a gradual loss of humus in the soil. The grass hurts away and moss quickly gets over.

The easiest and most drastic way to restore any garden is soil improvement. Efforts to improve your soil provide quick results in your garden, while building long-term benefits. You will be rewarded with healthy plants, which look better and more even, even in weather-like weather, like drought and cold.

An ideal garden

What is soil? Although the earth seems to be solid under our feet, only half of the soil consists of solid particles. The other half is a combination of air and water. In good ground about half of this is filled with water. In that water, many chemicals have been dissolved, including the nutrients that are essential for plant growth. The remaining space or air is also important: it supplies oxygen to plant roots and soil organisms.

Although you may not realize it, it triggers the ground of the most diverse life forms. Most soil creatures are of microscopic format; Greater species such as worms and ants are better seen. Plants (and gardeners) are dependent on soil organisms for converting nutrients into a form that they can absorb and for recycling nutrients from organic matter. The different life forms in the soil together form a complex ecosystem. One of the basic ways to get super ground is to cherish this ecosystem and prevent it from getting out of balance.

Sand, clay or clay?

One of the most important properties of the soil is the texture. Texture is nothing but the relationship between soil particles of different sizes. Soils contain a mixture of different particle size and are named according to the predominant particle size herein. xlargestuff blog has new stuff to share with people.  Sand particles are 0.05 to 2 mm, usually large enough to be visible. They feel grainy on their fingers. What is bigger than sand is called gravel. Clay particles, however, (0.002 to 0.05 mm) are smaller than sand, and no longer visible to the naked eye. The finest soil particles (clay) are smaller than 0.002 mm. Pure clay particles are smooth and sticky to the fingers. The influence of the texture on the physical soil properties is high. For example, between larger particles is more space. That explains why sandy soils lose rainwater faster than others (good drainage). The smaller the particles, the greater their total external surface that enables them to hold water and nutrients.

Therefore, soil with more clay or clay can also hold more nutrients and water. Of course, different advantages and disadvantages are attached to different textures. Too much clay is a soil with lots of nutrients but also with problems of poor ventilation and slow drainage. Such soils are called heavy. Too much leem can cause drainage problems. Too much sand means drainage problems never occur, but you have to fertilize again because the nutrients also flush away. Such soils are called light. The best soil texture does not consist of all sized particles, but a balanced mix of sand, silt and clay. Generally, the more northerner you are in Flanders, the more sandy the bottom is. Large areas in central Flanders consist of a mixture of sand and loam. Leembodems are especially found in Brabant and South Limburg. Real clay dams are found only in the polders or in the immediate vicinity of some watercourses.

Replies: 0 / Share:

You might also like …

Post Comment

Your email address will not be published. Required fields are marked *