Abstract
The expected shortage of global phosphate has enforced the search for alternative resources for P fertilizers. Therefore, the present study focuses on the turnover of phosphorus (P) of hydrochars and pyrochars derived from sewage sludge (SS) in soils during plant growth. We designed a pot experiment in which Lolium perenne L. was allowed to grow on a Calcic Cambisol amended with SS-derived chars. Hydrothermal carbonization (HTC) yielded the SS-hydrochars (200 °C, 260 °C; 30 min, 3 h), whereas the SS-pyrochars were obtained after dry pyrolysis (600 °C, 1 h). Increasing severity of HTC lowered the recovery of total P (PT) from the feedstock to 76%. The Olsen-P diminished from 4% PT in the untreated sludge to 1% PT in the hydrochars, whereas the pyrochars exhibited an Olsen-P between 3 and 6%. At the end of the pot experiment, the soils amended with pyrochars and with hydrochars produced at 200 °C contained more Olsen-P than the unamended soils, proving that P-rich chars can indeed serve as a P fertilizer. Part of the P sequestered in the chars turned into a mobile form during the experiment. After addition of our chars, the soil pH remained alkaline, allowing the conclusion that P could not have been solubilized through just abiotic processes. We suggest that biological and biochemical processes are involved in this mobilization. This work demonstrates that, in order to evaluate the efficiency of an organic amendment as a P fertilizer, the knowledge of their P availability alone is not sufficient and a better understanding of the biochemical processes involved in the cycling of its immobilized P is certainly required.
Highlights
The annual phosphorus (P) input required for agriculture in the European Union (EU) was estimated to be 3.85 million tons (P2O5) per year [1]
The solid by-product that results from pyrolysis can be called biochar, if it meets the requirements of the International Biochar Initiative [6] or the European Biochar certificate [7]
Our results indicated a decrease in electrical conductivity (EC) during dry pyrolysis
Summary
The annual phosphorus (P) input required for agriculture in the European Union (EU) was estimated to be 3.85 million tons (P2O5) per year [1]. SS applied on land has to meet with the established standards regarding pollutants and requires a pretreatment destroying potential pathogens and reducing its fermentability This may be achieved by dry pyrolysis or hydrothermal carbonization (HTC). The solid by-product that results from pyrolysis can be called biochar, if it meets the requirements of the International Biochar Initiative [6] or the European Biochar certificate [7] We studied the alteration of the amount of potentially plant available P (Olsen-P) derived from SS hydrochars and pyrochars after their amendment to a sandy loamy soil during an 80-day greenhouse pot experiment with Lolium perenne L. Bearing in mind that soil pH affects P solubility, the pH values of the soils at the end of the experiment were determined
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