The Brazilian semiarid region has been subjected to strong man-made actions since the 1970s, which have resulted in landscape transformation. The scientific literature presents several studies on the soil properties or microclimate of different types of landscapes; however, less attention was having been paid to the surface contrast between native vegetation and bare soil. The objective of this research was to evaluate the soil properties and microclimate of two common landscapes in the Brazilian semiarid region, a seasonally dry tropical forest (Caatinga) and a deforested area. Soil and microclimate data were obtained from two sites, both located in the State of Pernambuco, Brazil. Soil samples were collected on six dates and from layers, ...
The main objective of this work is to evaluate soil physical properties affected by cover crop rota...
Introduction the evaluation of soil fertility in already placed agroforestry systems allows inferenc...
In this study, the microclimate changes in silvopastoral systems are quantified at different time an...
Deforestation of Caatinga and inadequate land use of these dry environments have impacted soil quali...
Accelerated land use changes have been observed in Brazil. In Northeast, the Caatinga (native vegeta...
Accelerated land use changes have been observed in Brazil. In Northeast, the Caatinga (native vegeta...
ABSTRACT The Seridó Desertification Region is a result of inadequate management of the native Caatin...
International audienceCaatinga is a Brazilian dry ecosystem that occupies around 1 million km2 and i...
Studies show that soil organic carbon (SOC) decreases between 3 % and 9 % in degraded grasslands in ...
The Brazilian semi-arid tropics occupies an area of 969,589 km2 that represents 11% of the national ...
Desertification is recognized as the land degrada - tion in arid, semiarid, and dry sub-humid zones,...
The Caatinga Domain is exclusively Brazilian, covered by vegetation exhibiting a great diversity of ...
The objective of this work was to investigate the relationship between soil water content and rainfa...
Land use affect soil C and microbial structure, especially in tropical dry areas. The objective of t...
Anthropogenic activities have altered the atmospheric composition since the industrial era, especial...
The main objective of this work is to evaluate soil physical properties affected by cover crop rota...
Introduction the evaluation of soil fertility in already placed agroforestry systems allows inferenc...
In this study, the microclimate changes in silvopastoral systems are quantified at different time an...
Deforestation of Caatinga and inadequate land use of these dry environments have impacted soil quali...
Accelerated land use changes have been observed in Brazil. In Northeast, the Caatinga (native vegeta...
Accelerated land use changes have been observed in Brazil. In Northeast, the Caatinga (native vegeta...
ABSTRACT The Seridó Desertification Region is a result of inadequate management of the native Caatin...
International audienceCaatinga is a Brazilian dry ecosystem that occupies around 1 million km2 and i...
Studies show that soil organic carbon (SOC) decreases between 3 % and 9 % in degraded grasslands in ...
The Brazilian semi-arid tropics occupies an area of 969,589 km2 that represents 11% of the national ...
Desertification is recognized as the land degrada - tion in arid, semiarid, and dry sub-humid zones,...
The Caatinga Domain is exclusively Brazilian, covered by vegetation exhibiting a great diversity of ...
The objective of this work was to investigate the relationship between soil water content and rainfa...
Land use affect soil C and microbial structure, especially in tropical dry areas. The objective of t...
Anthropogenic activities have altered the atmospheric composition since the industrial era, especial...
The main objective of this work is to evaluate soil physical properties affected by cover crop rota...
Introduction the evaluation of soil fertility in already placed agroforestry systems allows inferenc...
In this study, the microclimate changes in silvopastoral systems are quantified at different time an...