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View article: Combining long-term ICP Forests monitoring data with the Yasso carbon cycling model at the European scale
Combining long-term ICP Forests monitoring data with the Yasso carbon cycling model at the European scale Open
Forests form a major organic carbon reservoir, both above- and belowground. In the course of global change, predicting possible changes in these carbon reservoirs is essential. To this end, the Horizon Europe PathFinder project aims to dev…
View article: Long-term variations in nitrate leaching from ICP Forests Level II plots
Long-term variations in nitrate leaching from ICP Forests Level II plots Open
Forests in Europe have been exposed to an increase in atmospheric deposition of nitrogen in the second half of the 20th century that potentially lead to nitrogen saturation and elevated leaching of nitrogen from forest soils potentially im…
View article: Soil organic carbon mineralization is controlled by the application dose of exogenous organic matter
Soil organic carbon mineralization is controlled by the application dose of exogenous organic matter Open
Substantial input of exogenous organic matter (EOM) may be required to offset the projected decline in soil organic carbon (SOC) stocks in croplands caused by global warming. However, information on the effectivity of the EOM application d…
View article: Comment on egusphere-2024-107
Comment on egusphere-2024-107 Open
Abstract. Substantial input of exogenous organic matter (EOM) may be required to offset the projected decline in soil organic carbon (SOC) stocks in croplands caused by global warming. However, information on the effectivity of EOM applica…
View article: Soil organic carbon mineralization is controlled by the application dose of exogenous organic matter
Soil organic carbon mineralization is controlled by the application dose of exogenous organic matter Open
Substantial input of exogenous organic matter (EOM) may be required to offset the projected decline in soil organic carbon (SOC) stocks in croplands caused by global warming. However, information on the effectivity of EOM application dose …
View article: Biogeochemical consequences of agricultural soil contamination with Sulfamethoxazole (SMX)
Biogeochemical consequences of agricultural soil contamination with Sulfamethoxazole (SMX) Open
Agricultural soils are increasingly polluted by antibiotics, and this makes them a source of antimicrobial resistance (AMR). However, antibiotics may also change microbial communities in soils, and so alter microbiological processes. Given…
View article: Effect of organic carbon addition on paddy soil organic carbon decomposition under different irrigation regimes
Effect of organic carbon addition on paddy soil organic carbon decomposition under different irrigation regimes Open
Anaerobic decomposition of organic carbon (OC) in submerged rice paddies is coupled to the reduction of alternative soil electron acceptors, primarily Fe3+. During reductive dissolution of Fe3+ from pedogenic oxides, previously adsorbed na…
View article: Reply on RC1
Reply on RC1 Open
Abstract. Anaerobic decomposition of organic carbon (OC) in submerged rice paddies is coupled to the reduction of alternative soil electron acceptors, primarily Fe3+. During reductive dissolution of Fe3+ from pedogenic oxides, previously a…
View article: Reply on RC2
Reply on RC2 Open
Abstract. Anaerobic decomposition of organic carbon (OC) in submerged rice paddies is coupled to the reduction of alternative soil electron acceptors, primarily Fe3+. During reductive dissolution of Fe3+ from pedogenic oxides, previously a…
View article: Comment on bg-2021-53
Comment on bg-2021-53 Open
Abstract. Anaerobic decomposition of organic carbon (OC) in submerged rice paddies is coupled to the reduction of alternative soil electron acceptors, primarily Fe3+. During reductive dissolution of Fe3+ from pedogenic oxides, previously a…
View article: Soil texture can predominantly control organic matter mineralization in temperate climates by regulating soil moisture rather than through direct stabilization
Soil texture can predominantly control organic matter mineralization in temperate climates by regulating soil moisture rather than through direct stabilization Open
<p>Soil organic carbon (OC) levels generally increase with increasing clay and silt content under a similar climatic zone because of increased association of OC to clay minerals and stronger occlusion inside aggregates. Surprisingly …
View article: Effect of organic carbon addition on paddy soil organic carbondecomposition under different irrigation regimes
Effect of organic carbon addition on paddy soil organic carbondecomposition under different irrigation regimes Open
Anaerobic decomposition of organic carbon (OC) in submerged rice paddies is coupled to the reduction of alternative soil electron acceptors, primarily Fe3+. During reductive dissolution of Fe3+ from pedogenic oxides, previously adsorbed na…