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Soil considerations in cultivation of plants

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Soil considerations in cultivation of plants. There are analyzed the results of investigations on the effect of tractor outfit traffic over the field on the plant growth conditions. Changes in soil compaction, density and porosity influenced by compacting by wheels are presented in relations to optimal values. The effect of excessive soil compaction on development of root system and absorption of nutrients are presented.
Too intensive management by mowing or grazing or cessation of management both lead to the floristic impoverishment of meadow communities. Soil seed bank can play an essential role in the ecological restoration of species-rich semi-natural grasslands. In Poland, little research has been conducted in this area, particularly refers to Arrhenatherion meadows. The aim of the studies was to determine the density and species composition of the soil seed bank of Arrhenatheretum elatioris meadows as well as the distribution of seeds across four soil levels. The studies were carried out in two habitats: Arrhenatheretum elatioris (code 6510-1) and Poa pratensis – Festuca rubra (code 6510-2). Soil samples were collected up to a depth of 20 cm, divided into four levels: 0-5 cm, 5-10 cm, 10-15 cm 15-20 cm. The size and species composition of the seed bank was determined by extracting seeds from the soil samples. The number of diaspores (seeds and fruits) in the topsoil (0-20 cm) layer was 56,430 seeds·mˉ² (Arrhenatheretum elatioris) and 118,510 seeds·mˉ² (Poa pratensis – Festuca rubra). The soil seed banks were dominated by diaspores of annual dicotyledonous species (above 80%) which were mainly seeds of arable weeds or ruderal plants. The assessed soil seed banks were dominated by Chenopodium album and Stellaria media. In both grasslands, the quantity of Poaceae and Fabaceae diaspores were very low. These results confirmed that most mesic grassland species did not form persistent seed banks and reintroduction of target species seeds is necessary in order to restore the species-rich Arrhenatherion elatioris meadows.
Soil structure depends on several factors, among which are farming system and soil tillage. The state of aggregation determines the water-air relations in soil and influences the thermal conductivity, porosity and density of soil, availability of nutrients, as well as biological processes, etc. In the field experiment with conservation tillage for onion we studied the influence of various methods of conventional tillage, no tillage, and disking as well as the biomass of the inter-harvest plants on the aggregation and structure of soil. Secale cereale and Vicia sativa cultivated as inter-crop cover plants favourably influenced the soil aggregation. It was expressed by greater share of valuable soil aggregates (ø1–5 mm) and better soil structure index in comparison with conventional tillage (CT), without plant mulches. The leaving of mulches from cover plants on the surface of the soil from fall to spring and direct sowing on onion without tillage (NT) decreased soil cloddiness index. The positive influence of plant mulches on soil structure was mainly observed after wintering and in the initial period of onion vegetation. The changes in indicators of soil aggregation under the influence of mulching and simplifications of the soil tillage system for vegetables were predominantly recorded in the soil arable layer of 0–20 cm.
Commonly used gravimetric; method of determining soil density was compared under laboratory conditions with the indicator method developed at the Department of Soil Cultivation and Fertilization Techniques, IUNG Jelcz-Laskowice. The tests were carried out on artificial soil profiles with four degrees of compaction. Differences in the soil density determined with respective methods were in most eases contained within the limits of the measurement error. Discrepancies of the results obtained with the methods compared were decreasing along an increasing degree of soil density and thickness of the layer measured. The results obtained encourage to acknowledge the indicator method tested as an applicable measuring device lbr the density dynamics of soil profile.
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