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This is an exact reproduction of the original 289 emblems, but with a 351 twist. Featuring a show-quality chrome-plated die-cast body. mounting hardware is included.
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Phosphorus (P) is an essential nutrient for the plant life cycle. The agricultural management of phosphorus is complicated by the inefficient use of phosphorus by plants, consequent environmental losses, and the rapid consumption of slowly renewed phosphate rock (PR). These issues represent a huge environmental burden and jeopardise food production. In this study, we proposed the combination of this fertiliser with food-processing by-products such as olive pomace, barley spent grain, and citrus pomace to increase phosphate rock solubility and the efficient use of P. Phosphate rock, by-products, and mixtures of phosphate rock and by-products were placed into litterbags and buried in sand. Periodically, one replicate per treatment was collected for the destructive measurement of total and water-soluble phosphorus. In parallel, pH, organic matter, and ash content were measured to investigate the mechanisms behind changes in P content. The mixtures’ P-release values ranged between 80% and 88%, whereas phosphate rock lost 23% of its P over 30 days. Phosphate rock showed a constant water-soluble P fraction at the four sampling times, whereas the mixtures exhibited a highly water-soluble P fraction that tended to decrease over time. Specifically, citrus pomace led to the significant and rapid release of phosphorus, barley spent grain maintained the highest water-soluble fraction over 30 days, and olive pomace was not the best-performing product but still performed better than pure phosphate rock. Moreover, the increased solubility of phosphate rock in mixtures was significantly (p < 0.001) ascribed to the reduction in pH. The results of this experiment are promising for in vivo trials and suggest the possibility of simple and easily achievable solutions for more sustainable production systems and effective P-fertilisation strategies. Proposing such easily applicable and inexpensive solutions can reduce the distance between research achievements and field applications.
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Although soil may have a high total P concentration, it is barely available because of the ease of formation of insoluble complexes with cations [1]. This makes P the least accessible macronutrient and one of the most deficient nutrients in agricultural soil [2].
Following Liebig’s law of the minimum, which has been validated by various experiments [3, 4, 5, 6], insufficiency of P in soils becomes a limiting factor for crops in terms of their ability to exploit other nutrients efficiently and to attain optimised growth. To increase yields, overcome P deficiency, and compensate for the retrogradation phenomenon, farmers in the past century have tended to overuse fertilisers [7], causing damage to natural ecosystems [8, 9, 10]. Only a small portion of the P used in agriculture is efficiently used for food production, while the rest contributes to eutrophication. Most of the current efforts towards reversing this trend focus on the recovery of P contained in plant residues and the reduction of run-off [11]. A new line of research has successfully explored the potential of chemical strategies to increase phosphorus use efficiency, for example through the use of humic–metal–phosphate acid complexes [12, 13]. However, these strategies are not yet available for organic agriculture. In this context, there is a shortage of work and research on increasing the efficient use of available P resources.
For decades now, the most widely used P fertiliser has been phosphate rock, due to its relatively low cost [2, 14, 15]. Although this resource is renewable, the speed with which it is being consumed is leading to its depletion, and the
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