scholarly journals The effects of organic and mineral fertilizers on carbon sequestration, soil properties, and crop yields from a long-term field experiment under a Swiss conventional farming system

2018 ◽  
Vol 29 (4) ◽  
pp. 926-938 ◽  
Author(s):  
Alexandra Maltas ◽  
Hedi Kebli ◽  
Hans Rudolf Oberholzer ◽  
Peter Weisskopf ◽  
Sokrat Sinaj
1960 ◽  
Vol 40 (2) ◽  
pp. 136-145 ◽  
Author(s):  
L. B. MacLeod ◽  
R. F. Bishop ◽  
L. P. Jackson ◽  
C. R. MacEachern ◽  
E. T. Goring

In a field experiment, conducted from 1936 to 1957, a rotation of swedes, oats and hay was followed and treatments included commercial fertilizers and manure.Changes in the chemical composition of the soil during the experiment included significant decreases in soil organic matter, total nitrogen and cation exchange capacity. In no case was the initial content of exchangeable potassium maintained and although changes in adsorbed and easily acid-soluble phosphorus were negligible with a number of treatments only one resulted in a significant increase.The treatments were applied in the swede year and yield differences with this crop were greater than for either the oats or hay. Data for the latter two crops indicated that with most of the treatments there was a tendency for yields to decline as the experiment progressed. This was not the case with swedes where variation in yields with rotation cycles was greater than it was in the case of oats or hay. There was a considerable residual effect from manure, and phosphorus had a greater effect on yields than either nitrogen or potassium.


2020 ◽  
Vol 120 ◽  
pp. 126132
Author(s):  
Holger Kirchmann ◽  
Gunnar Börjesson ◽  
Martin A. Bolinder ◽  
Thomas Kätterer ◽  
Faruk Djodjic

2017 ◽  
Vol 236 ◽  
pp. 21-29 ◽  
Author(s):  
Deirdre E. Griffin ◽  
Daoyuan Wang ◽  
Sanjai J. Parikh ◽  
Kate M. Scow

1962 ◽  
Vol 42 (1) ◽  
pp. 49-60 ◽  
Author(s):  
R. F. Bishop ◽  
L. B. MacLeod ◽  
L. P. Jackson ◽  
C. R. MacEachern ◽  
E. T. Goring

Treatments in a field experiment, conducted from 1936 to 1957, included commercial fertilizers and manure. A rotation of potatoes, oats and hay was followed.Application of manure at 30 tons per acre every third year practically maintained initial levels of total nitrogen and soil organic matter. Marked decreases occurred with lower rates of manure and various commercial fertilizers applied at 1 ton per acre. Increases and decreases in adsorbed and easily acid-soluble phosphorus were directly related to the amounts of phosphatic fertilizer applied. Although the situation with respect to exchangeable potassium was not comparable there was some evidence that final values were influenced by the amounts of potassium applied.All treatments were applied for potatoes, and yield differences were much greater for this crop than for either oats or hay. Rate of fertilizer application was of primary importance for potatoes, and residual effects on the oat and hay crops from 500 or 1000 pounds of commercial fertilizer per acre were generally slight. They were much more marked from manure and where commercial fertilizer was applied at a ton per acre. Irrespective of the treatment applied, linear regression coefficients, showing yield trends with advancing rotation cycles, were positive for potatoes and negative for hay. In the case of oats they were generally negative for the lowest rates of fertilizer used and positive for the highest.


2021 ◽  
Author(s):  
Roberta Pulcher ◽  
Enrico Balugani ◽  
Maurizio Ventura ◽  
Nicolas Greggio ◽  
Diego Marazza

<p>In the context of climate change mitigation, technologies for removing the CO<sub>2</sub> from the atmosphere are key challenges. Most recent scenarios from integrated assessment models require large-scale deployment of negative emissions technologies (NETs) to reach the 2 °C target. Among them, technologies for increasing organic carbon content in soils (SOC) have been developed. In the 15<sup>th</sup> IPCC special report on Global Warming of 1.5 °C, biochar and pyrogenic carbon capture and storage have been credited as promising negative emission technology. In fact, soil carbon sequestration (SCS) and biochar have a large negative emission potential (each 0.7 GtCeq. yr<sup>-1</sup>) and they are expected to have lower impact on land, water use, nutrients, albedo, energy requirement and cost, and thus fewer disadvantages than many other NETs.</p><p>SCS can be assessed using soil carbon dynamic models, such as RothC, as suggested by IPCC. However, studies on the inclusion of biochar in RothC are still scarce. Furthermore, most of these studies are based on the results of laboratory experiments and do not account for the effects of biochar on SOC degradation (the priming effect). The use of laboratory data can be problematic, since they may not adequately represent field conditions, especially due to the lack of long-term field studies.</p><p>The aim of this work was to assess and predict how biochar influences the soil C dynamics, by modifying the RothC model to simulate the findings of a long-term field experiment on biochar application to a short coppice rotation in Italy. We first modified the model to include two stocks of C input into the soil: the labile and the recalcitrant biochar pools. We also included a parametrized function to account for the priming effect on SOC dynamics in the soil. Secondly, we calibrated the model parameters with the data obtained from the field experiment. Finally, we validated the model results by estimating the remaining biochar amount in the site after 10 years from application, using an isotopic mass balance.</p><p>The results confirm that biochar degradation can be faster in field conditions in comparison to laboratory experiments; nevertheless, it can contribute to substantially increase the C stock in the long-term. Moreover, the modified RothC model allowed to assess the SCS potential of biochar application in soils, at least in the specific conditions examined, and could represent a flexible tool to assess the effect biochar as a SCS strategy in the long-term. We are exploring the possibility to use data from other long-term field experiment to move in that direction. The results of this study could be added to the Italian biochar database, providing new knowledge about a topic that needs to be explored.</p>


Author(s):  
V. А. Shevchenko ◽  
A. V. Nefedov ◽  
A. V. Ilinskiy ◽  
А. Е. Morozov

Long-term observations of the drained soil of peat-podzolic-gley light loam on ancient alluvial sands state on the example of the meliorative object "Tinky-2" showed that under the influence of agricultural use in the soil, the organic matter mineralization processes are accelerated. During the drainage process, the soil evolutionarily suffered the following changes: the peat layer was compacted, humified and mineralized, which was a reason of the transformation them into the humus horizon. Based on the monitoring studies results it was established that during 21 intensive use years the peat layer thickness was decreased by 74.5% and amounted to 5.51 inch, which in the following 20 years was decreased to a layer of 1.18 inch, and for another 14 years it became a homogeneous humus horizon containing difficulty identifiable plant remains. For half a century, the bulk density increased by 6 times and the total moisture capacity of the soil decreased by 3.6 times. Other indicators were changed significantly. So, the ash content by 2016 increased from 11.2% to 52.7%. It was a reason of the plough-layer decreasing and it mixes with the mineral sand horizon during plowing. It should also be noted that the total nitrogen content in the soil decreased by 1.13%, and total carbon by 15.3% from 1982 to 2016. The dynamics of changes in the soil acidity, phosphorus and potassium content is associated with the introduction of calcareous, organic and mineral fertilizers in the 1980s. The unsystematic exploitation of such soils leads to decrease in the agricultural products productivity and increase in energy costs. When planning these soils usage in agricultural production, it is necessary to develop and implement modern melioration technologies and techniques aimed to increase soil fertility.


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