Browsing by Subject "lake sediment"
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Development of sustainable practices for using lake sediment as growing medium for grass production (2023)Anthropogenic activities have resulted in huge accumulation of plant nutrients in lake sediments. These nutrients can be recycled back to the overlying water and sustain eutrophication. The release of phosphorus (P) from sediments, i.e. internal P loading, has often been a reason for delay in improvement of lake water quality, after reduced external nutrient loading. By removing the sediment, the internal lake nutrient load can be effectively reduced, and it is widely used in lake water quality restoration. By redirecting the reclaimed nutrients back to primary agricultural production, the need for using mineral fertilizers and virgin materials can be reduced. Currently there is, however, a lack of field-scale experiments and determination of best practices to enable efficient nutrient uptake and minimized nutrient leaching back into the lakes. A field experiment was conducted to study the effects of using P-rich lake sediment in different application methods for growing a mixture of forage grasses. The study focused on soil fertility, plant growth and nutrition, and species composition over a period of four growing seasons in central Estonia. Treatments for reducing nutrient losses included applying the sediment alone (Sed), with surface-incorporated biochar (Sed+BC), and as incorporated with surface-mixed biochar-topsoil mixture (Sed+Soil+BC). A treatment consisting of sandy loam topsoil was set up as control (Soil). The mean dry mass yield in the sediment treatments exceeded the local average grass yields and the N and P uptake rates in above-ground biomass (AGB) exceeded the international estimates for grasses. The sediment had no significant effect on AGB yield in comparison to the control. Similarly, no effect was observed in the yield of weeds, but temporary changes in weed species composition and an increasing trend particularly in nettle abundance on the sediment treatments were recorded. Apart from a transient increase in the amount of soluble potassium, no relevant effects were induced by the incorporated biochar. In conclusion, the sediment performed well and served as a plentiful source of P for grasses for four years. Based on the sufficient concentrations of P, sulphur, calcium and potassium in the plant tissue, yield increase could have been expected but most likely the good fertility of the control topsoil evened out yield differences between growing medium treatments. Based on this study, similar lake sediments can be advised to be used as soil amendments on grass cultivation on an agricultural field. Due to high nutrient concentrations, a lower rate could be applied on a wider field area to control excess in nutrient supply, given that the need of nitrogen fertilization is ensured to match plant-specific requirements.
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(2023)Nutrients get deposited in lake sediment from agricultural areas and other anthropogenic activities resulting in internal P loading and eutrophication. On the other hand, the situation with P rock (non renewable resource) used for production of mineral fertilizer is alarming that result in the depletion of P rock and increase P fertilizers price. The issue can be minimized by sediment removal and recycling nutrients from sediment for crop production. The existing results on sediment P availability for crops showed contradictory results and suggested that sediment P bioavailability for the crop is influenced by sediment iron to phosphorus mass ratio. However, comprehensive studies confirming their relationship are currently lacking. Hence, the study aims to determine the potential of sediment as fertilizers for crop (ryegrass) from several eutrophic lakes (in Finland and Estonia). The aim is to identify the effect of different lake sediments on ryegrass aboveground biomass and nutrient uptake. The study was conducted on greenhouse for around 6 months. Randomised complete block design was used for the experiment. The experimental treatments include sand with six different lake sediments: Peipsi, Lämmijärv, Kutajärvi, Kymijärvi, Matjärvi and Enonselkä basin of Vesijärvi, mineral fertilizer (positive) and without P fertilizer (negative) control. The biomass (yield) and nutrient uptake by the plants were measured and then analyzed for nutrient content. Significant effect of lake sediment was observed on ryegrass yield and P uptake. The significantly higher yield was observed for Lake Peipsi sediment treatment than in both controls. The ryegrass dry matter yield was greater in sediment treatments than negative control. Also, ryegrass yield was found to be greater in some sediment treatments than positive control. The concentration of nutrients (sulphur, calcium, magnesium, and potassium) was sufficient in ryegrass plant in all lake sediment treatments. The P uptake from Enonselkä sediment treatment was the highest whereas from Kutajärvi sediment treatment was the lowest. The P uptake was the highest (16.3 kg ha-1) in Enonselkä sediment treatment with the lowest Fe:P ratio of 12. Moreover, the result suggests that Fe:P mass ratio is one of the factors/sediment properties that determine P availability to the crops. However, other sediment properties may also affect P availability in the plants as organic P fraction was also used as an additional P source in some cases. The sediment increased C content and organic matter content compared to controls which improved ryegrass growth in sediment treatments. The increase in nutrient uptake and biomass in lake sediment treatments showed that lake sediment can be potential alternatives for fertilizers in nutrient deficient soil.
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