Alternatives to Slash and Burn Agriculture

2015 ◽  
pp. 33-39
Author(s):  
P. A. Sanchez
Keyword(s):  
Slash And Burn ◽  
Slash And Burn Agriculture

scholarly journals Changes in soil properties following slash and burn agriculture in the humid forest zone of Cameroon

2013 ◽  
Vol 8 (18) ◽  
pp. 1990-1995 ◽  
Author(s):  
F O Tabi ◽  
Ze A D Mvondo ◽  
A Boukong ◽  
R J Mvondo ◽  
G Nkoum
Keyword(s):  
Soil Properties ◽  
Forest Zone ◽  
Humid Forest ◽  
Slash And Burn ◽  
Slash And Burn Agriculture ◽  
Humid Forest Zone ◽  
Changes In Soil Properties

scholarly journals Integrating Stand and Soil Properties to Understand Foliar Nutrient Dynamics during Forest Succession Following Slash-and-Burn Agriculture in the Bolivian Amazon

PLoS ONE ◽  
2014 ◽  
Vol 9 (2) ◽  
pp. e86042 ◽  
Author(s):  
Eben N. Broadbent ◽  
Angélica M. Almeyda Zambrano ◽  
Gregory P. Asner ◽  
Marlene Soriano ◽  
Christopher B. Field ◽  
...  
Keyword(s):  
Soil Properties ◽  
Nutrient Dynamics ◽  
Forest Succession ◽  
Slash And Burn ◽  
Slash And Burn Agriculture ◽  
Bolivian Amazon ◽  
Foliar Nutrient

scholarly journals Aspects of Land Use in Slash and Burn Agriculture

2003 ◽  
Author(s):  
Amitrajeet A. Batabyal ◽  
Dug Man Lee
Keyword(s):  
Land Use ◽  
Slash And Burn ◽  
Slash And Burn Agriculture

scholarly journals Slash-and-burn agriculture and tropical cyclone activity in Madagascar: Implication for soil fertility dynamics and corn performance

2017 ◽  
Vol 239 ◽  
pp. 207-218 ◽  
Author(s):  
J.M. Gay-des-Combes ◽  
B.J.M. Robroek ◽  
D. Hervé ◽  
T. Guillaume ◽  
C. Pistocchi ◽  
...  
Keyword(s):  
Tropical Cyclone ◽  
Soil Fertility ◽  
Tropical Cyclone Activity ◽  
Cyclone Activity ◽  
Slash And Burn ◽  
Slash And Burn Agriculture

Dominant drivers of runoff in a slash-and-burn affected catchment in upland Eastern Madagascar

2021 ◽  
Author(s):  
Bob W. Zwartendijk ◽  
H.J. (Ilja) van Meerveld ◽  
Ryan J. Teuling ◽  
Chandra P. Ghimire ◽  
L. Adrian Bruijnzeel
Keyword(s):  
Soil Moisture ◽  
Overland Flow ◽  
Quantitative Information ◽  
Forest Loss ◽  
Runoff Generation ◽  
Catchment Scale ◽  
Valley Bottom ◽  
Antecedent Soil Moisture ◽  
Slash And Burn ◽  
Slash And Burn Agriculture

<p>In many tropical areas slash-and-burn agriculture is an important driver of forest loss. In areas where slash-and-burn agriculture has been practiced for decades, land cover is typically a mosaic of patches of remnant forest, fields under active cultivation, fallows in various stages of regrowth (ranging from young shrub to semi-mature), and degraded fire-climax grasslands. Although runoff generation mechanisms are expected to be different for these different patches, little quantitative information is available in this regard, particularly at the catchment scale and over longer time-scales (i.e., multiple slash-and-burn cycles).</p><p>We re-instrumented a 31 ha catchment in upland Eastern Madagascar, where slash-and-burn agriculture has been practiced for more than 70 years in 2015; it had been monitored between 1963 and 1972 as well<sup>1</sup>. We measured streamflow at two locations and overland flow and soil moisture for four hillside plots (0.05 – 1.93 ha): one plot under repeatedly coppiced and burned <em>Eucalyptus</em> and three plots under young shrub and tree fallows. One of the plots underwent rudimentary terracing in the past. We analysed the rainfall-runoff dynamics for 50 rainfall events (median 12 mm, maximum 71 mm).</p><p>For 60% of the events, the stormflow coefficient (minimum contributing area) was <3%, which is the proportion of valley-bottom wetlands and rice paddies in the catchment. Stable isotope sampling for five storm runoff events indicate a maximum total event-water contribution of 16%. However, instantaneous event-water contributions were as high as 66%. The hillside plot runoff response was dominated by saturation-excess overland flow and showed strong threshold behaviour in terms of the antecedent soil moisture storage in the upper 30 cm of the soil plus the event total rainfall amount (ASI + P). Average threshold values for overland flow occurrence ranged from 87 mm for the coppiced <em>Eucalyptus</em> to 137 mm for the young fallow plots (regardless of terrace presence). Stormflow also increased after an ASI+P-threshold was exceeded (100 mm based on the soil moisture sensors for the <em>Eucalyptus</em> plot and 150 mm for the sensors at the tree fallow plots).</p><p>These results indicate an increased hydrological connectivity between hillslopes and valley bottom under wetter conditions and that stormflow in the study catchment is strongly affected by variations in seasonal rainfall. The results will be used to validate a hydrological model to determine the net effect of concurrent changes in soil infiltrability and vegetation water use associated with forest loss and recovery on stormflow totals and the seasonal flow regime.</p><p><strong><sup>1</sup></strong>Bailly, C., de Coignac, G.B., Malvos, C., Ningre, J.M., and Sarrailh, J.M. (1974). Étude de l'influence du couvert naturel et de ses modifications á Madagascar. Expérimentations en bassins versants élémentaires. Cahiers Scientifiques, 4. Centre Scientifique Forestier Tropical, Nogent-sur-Marne, France, 114 pp.</p>

Slash-and-Burn Agriculture, Effects of

2001 ◽  
pp. 269-284 ◽  
Author(s):  
Stefan Hauser ◽  
Lindsey Norgrove
Keyword(s):  
Slash And Burn ◽  
Slash And Burn Agriculture
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