Metal(loid)s remobilization and mineralogical transformations in smelter-polluted savanna soils under simulated wildfire conditions

2021 ◽  
Vol 293 ◽  
pp. 112899
Author(s):  
Marek Tuhý ◽  
Vojtěch Ettler ◽  
Jan Rohovec ◽  
Šárka Matoušková ◽  
Martin Mihaljevič ◽  
...  
Keyword(s):  
Soil Research ◽  
2020 ◽  
Vol 58 (4) ◽  
pp. 335
Author(s):  
Stan J. Rance ◽  
David M. Cameron ◽  
Carl R. Gosper ◽  
Emlyn R. Williams

Agriculture and forestry in savanna soils worldwide are often constrained by multiple soil limitations. We measured the effect of fertilisation on growth of Pinus caribaea var. hondurensis in order to improve savanna soil productivity in the Northern Territory, Australia. Growth responses to nitrogen, potassium, sulfur and a combined trace element treatment (abbreviated to N × K × S × T) with basal phosphorus (P) application on three soils, and N × P × K × S × T on another three soils, were examined in glasshouse factorial experiments. Without P, there was little response to N, S or T. Growth was usually greatest on N + P + S treatments. The P applications increased soil pH and growth, while N and S applications decreased pH. Growth was consistently poor at soil pH < ~5.2; a pH where exchangeable cations can be leached from the soil and aluminium can become more mobile. Responses to P, N, S and K, and likely also to zinc, were consistent with savanna soils with a long history of nutrient losses due to fire and weathering. Establishing productive plantations or agriculture will require detailed knowledge of soil properties, careful attention to soil pH and balanced fertiliser applications so as not to produce perverse outcomes. Long-term protection from fires could improve soil conditions, to be balanced against the risks of crop loss through unplanned fire.


1992 ◽  
Vol 72 (4) ◽  
pp. 481-488 ◽  
Author(s):  
L. Seiny-Boukar ◽  
C. Floret ◽  
R. Pontanier

The purpose of this study was to characterize and quantify the degradation of Vertisols of savannas in Northern Cameroon. The work was carried out in a region with mean annual rainfall of 800 mm. It is a climate with 9 months theoretical drought and one raining season. The area is heavily populated and farmers use fallow to rejuvenate the soil. The post-cultural savannas (fallows) are subjected to fire, intensive grazing and cutting of fire wood. Three soil types at different stages of degradation were subjected to a study of their soil moisture regime including quantification of runoff during a three-year period. Physico-chemical characteristics are discussed, as well as variations in water reserves as a function of stages of degradation. Maximum wetting front varied from 30 to 80 cm. The most degraded soil lacked plant available moisture for 10 months as compared to 5 months for the least degraded. A model is presented of the dynamic relationships that may exist among the stages of degradation of these Vertisols. Key words: Savanna, Vertisol, water regime, degradation, soil dynamics


1999 ◽  
Vol 22 (1) ◽  
pp. 93-102 ◽  
Author(s):  
G. K. Korndörfer ◽  
L. E. Datnoff ◽  
G. F. Corrêa
Keyword(s):  

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