Biochar application as a tool to decrease soil nitrogen losses ( NH 3 volatilization, N 2 O emissions, and N leaching) from croplands: Options and mitigation strength in a global perspective

2019 ◽  
Vol 25 (6) ◽  
pp. 2077-2093 ◽  
Author(s):  
Qi Liu ◽  
Benjuan Liu ◽  
Yanhui Zhang ◽  
Tianlong Hu ◽  
Zhibin Lin ◽  
...  
2015 ◽  
Vol 5 (8) ◽  
pp. 705-706 ◽  
Author(s):  
Qing Zhu ◽  
William J. Riley

2014 ◽  
Vol 94 (2) ◽  
pp. 109-127 ◽  
Author(s):  
Sogol Rasouli ◽  
Joann K. Whalen ◽  
Chandra A. Madramootoo

Rasouli, S., Whalen, J. K. and Madramootoo, C. A. 2014. Review: Reducing residual soil nitrogen losses from agroecosystems for surface water protection in Quebec and Ontario, Canada: Best management practices, policies and perspectives. Can. J. Soil Sci. 94: 109–127. Eutrophication and cyanobacteria blooms, a growing problem in many of Quebec and Ontario's lakes and rivers, are largely attributed to the phosphorus (P) and nitrogen (N) emanating from intensively cropped agricultural fields. In fact, 49% of N loading in surface waters comes from runoff and leaching from fertilized soils and livestock operations. The residual soil nitrogen (RSN), which remains in soil at the end of the growing season, contains soluble and particulate forms of N that are prone to being transported from agricultural fields to waterways. Policies and best management practices (BMPs) to regulate manure storage and restrict fertilizer and manure spreading can help in reducing N losses from agroecosystems. However, reduction of RSN also requires an understanding of the complex interactions between climate, soil type, topography, hydrology and cropping systems. Reducing N losses from agroecosystems can be achieved through careful accounting for all N inputs (e.g., N credits for legumes and manure inputs) in nutrient management plans, including those applied in previous years, as well as the strategic implementation of multiple BMPs and calibrated soil N testing for crops with high N requirements. We conclude that increasing farmer awareness and motivation to implement BMPs will be important in reducing RSN. Programs to promote communication between farmers and researchers, crop advisors and provincial ministries of agriculture and the environment are recommended.


2003 ◽  
Vol 33 (4) ◽  
pp. 535-548
Author(s):  
Lucerina Trujillo ◽  
Johannes Lehmann ◽  
Manoel da Silva Cravo ◽  
André Luiz Atroch ◽  
Firmino José do Nascimento Filho

Fruit tree production is gaining an increasing importance in the central Amazon and elsewhere in the humid tropics, but very little is known about the nutrient dynamics in the soil-plant system. The present study quantified the effects of fertilization and cover cropping with a legume (Pueraria phaseoloides (Roxb.) Benth.) on soil nitrogen (N) dynamics and plant nutrition in a young guarana plantation (Paullinia cupana Kunth. (H.B. and K.) var. sorbilis (Mart.) Ducke) on a highly weathered Xanthic Ferralsol. Large subsoil nitrate (NO3-) accumulation at 0.3-3 m below the guarana plantation indicated N leaching from the topsoil. The NO3- contents to a depth of 2 m were 2.4 times greater between the trees than underneath unfertilized trees (P<0.05). The legume cover crop between the trees increased soil N availability as shown by elevated aerobic N mineralization and lower N immobilization in microbial biomass. The guarana N nutrition and yield did not benefit from the N input by biological fixation of atmospheric N2 by the legume cover (P>0.05). Even without a legume intercrop, large amounts of NO3- were found in the subsoil between unfertilized trees. Subsoil NO3- between the trees could be utilized, however, by fertilized guarana. This can be explained by a more vigorous growth of fertilized trees which had a larger nutrient demand and exploited a larger soil volume. With a legume cover crop, however, more mineral N was available at the topsoil which was leached into the subsoil and consequently accumulated at 0.3-3 m depth. Fertilizer additions of P and K were needed to increase subsoil NO3- use between trees.


2001 ◽  
Vol 18 (2) ◽  
pp. 81-89 ◽  
Author(s):  
Ross M. Tabachow ◽  
J. Jeffrey Peirce ◽  
Daniel D. Richter

2010 ◽  
Vol 125 (1) ◽  
pp. 25-33 ◽  
Author(s):  
Tao Ren ◽  
Peter Christie ◽  
Jingguo Wang ◽  
Qing Chen ◽  
Fusuo Zhang

2008 ◽  
Vol 88 (1) ◽  
pp. 61-78 ◽  
Author(s):  
R. De Jong ◽  
B. Qian ◽  
J Y Yang

Projected climate change in Canada and its impact on crop yield and production have been studied, but the impacts on soil and water quality are less well known. The objective of this study was to model and evaluate the potential impacts of climate change on soil nitrogen (N) leaching in Prince Edward Island. Residual soil nitrogen (RSN), the quantity of inorganic soil N at the time of harvest, was calculated from an annual N budget, based on Census of Agriculture data. RSN was "added" to the soil in the fall and subject to leaching until the start of the next growing season. Water and N movement in and through the soil were calculated with a modified version of the Versatile Soil Moisture Budget. The provincial averages of RSN and N leaching under historic (1971–2000) climate and management conditions were calculated to be 30.8 kg N ha-1 and 27.9 kg N ha-1, i.e. , 91% of the RSN was lost via leaching. With no changes in agricultural practices, N leaching under four climate change (2040–2069) scenarios remained very similar (± 1%) to that simulated under historic climatic conditions. With agricultural intensification, in response to climate change and economic conditions, RSN levels increased to 35.7 kg N ha-1 and estimates of soil N leaching increased by 5 to 30% beyond historic levels. Key words: Residual soil nitrogen, versatile soil moisture budget, climate change impacts, agricultural adaptation, water contamination


1995 ◽  
Vol 25 (8) ◽  
pp. 1346-1355 ◽  
Author(s):  
Chris E. Johnson

Previous research on chronosequences of even-aged northern hardwood stands has suggested that forest clearing is accompanied by large losses of nitrogen from the forest floor. The timing of the losses and the fate of a large fraction of the lost nitrogen are unclear. The purpose of this investigation was to study these questions through direct measurement of soil nitrogen concentrations and pools through time on an experimental catchment cleared in a whole-tree harvest in 1983–1984. Nitrogen losses from the forest floor at the site, the Hubbard Brook Experimental Forest, New Hampshire, were lower than predictions based on previous research. The mean forest floor nitrogen pool was 17% lower 8 years after clear-cutting of the site (P = 0.18). Predictions based on chronosequence studies suggest that 25–40% of the forest floor nitrogen would be lost after 8 years. Mechanical disturbance during logging may play a role in limiting short-term nitrogen losses. The steep midsection of the catchment experienced the greatest losses of nitrogen and carbon, while pools in the relatively flat spruce-fir zone at the upper elevations were unchanged. Carbon was preferentially lost from soil organic matter, relative to nitrogen, resulting in significant decreases in the C/N and C/organic matter ratios in the soil. The N/organic matter ratio was generally unchanged. Nitrogen losses can be limited after clear-cutting by minimizing organic matter losses and promoting rapid regrowth.


2015 ◽  
Vol 53 (3) ◽  
pp. 145-157 ◽  
Author(s):  
Asafor Henry CHOTANGUI ◽  
Koji SUGAHARA ◽  
Mayuko OKABE ◽  
Shigemitsu KASUGA ◽  
Katsunori ISOBE ◽  
...  

2019 ◽  
Vol 111 (5) ◽  
pp. 2493-2503
Author(s):  
Claudia Marcela Giletto ◽  
Nahuel Reussi Calvo ◽  
Hernán Echeverría

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