Soil carbon stock and Plinthosol fertility in smallholder land-use systems in the eastern Amazon, Brazil

被引:9
|
作者
dos Santos, Cealia Cristine [1 ]
de Lima Ferraz Junior, Altamiro Souza [1 ]
Sa, Sandra Oliveira [2 ]
Munoz Gutierrez, Jhonatan Andres [1 ]
Braun, Heder [1 ]
Sarrazin, Max [3 ]
Brossard, Michel [4 ,5 ]
Desjardins, Thierry [6 ]
机构
[1] Univ Estadual Maranhao, Agroecol Program, Cidade Univ Paulo 6, BR-65054970 Tirirical, Sao Luis Ma, Brazil
[2] Univ Estadual Maranhao, Geoenvironm Ctr, Rua Lourenco Vieira da Silva, BR-65055310 Tirirical, Sao Luis Ma, Brazil
[3] US IMAGO, IRD, Lab Moyens Analyt, Route Montabo, F-97323 Cayenne, Guyane Francais, France
[4] UMR Eco&Sols, IRD, BP 90165, F-97323 Cayenne, Guyane Francais, France
[5] Montpellier SupAgro, INRA, CIRAD, UMR Eco&Sols,IRD, 2 Pl Viala, F-34060 Montpellier, France
[6] UMR iEES Paris, IRD, 32 Ave Henri Varagnat, F-93143 Bondy, France
关键词
Soil organic matter; land-use change; mixed fallows; secondary forest; FOREST CONVERSION; ORGANIC-CARBON; NITROGEN STOCKS; DYNAMICS; PASTURE; MANAGEMENT; MATTER; QUALITY;
D O I
10.1080/17583004.2018.1530026
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The soil organic carbon (SOC) stock is an important attribute in the maintenance of ecosystem services by natural and agricultural ecosystems. In the humid tropics, slash-and-burn cultivation for food production and establishment of pastures has frequently led to soil degradation. In the eastern Brazilian Amazonia, we assessed impacts of different land-use systems on the SOC stock and some chemical properties of soils. Four land-use systems were studied: shifting cultivation (SC), pasture (PA), mixed fallow (MF) and secondary forest (SF). In the soils studied, most nutrients were not significantly influenced by land-use changes, and the chemical fertility was low. Similarly, SOC concentration was low, ranging, in the 0-10 cm layer, from 9.54 g kg(-1) in PA to 12.73 g kg(-1) in MF. In the 0-100 cm layer, the SOC stock varied from 42.1 Mg ha-1 in SC to 53.3 Mg ha(-1) in MF, without significant differences between the land-use systems. The SOC stock in the 0-30 cm layer represented 50-56% of that in the 0-100 cm layer. The soils studied have the lowest SOC stocks measured in the Amazonia region. The low organic matter content, associated with soil acidity, a small sum of exchangeable bases and low extractable P, can constrain the productivity and the sustainability of these cropping systems.
引用
收藏
页码:655 / 664
页数:10
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