首页> 外文期刊>Revista Brasileira de Ciência do Solo >Biological Properties and Organic Matter Dynamics of Soil in Pasture and Natural Regeneration Areas in the Atlantic Forest Biome
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Biological Properties and Organic Matter Dynamics of Soil in Pasture and Natural Regeneration Areas in the Atlantic Forest Biome

机译:大西洋森林生物群落中草场和自然更新区土壤的生物学特性和有机质动态

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ABSTRACT The removal of original vegetation for crops and pasture production and then followed by natural regeneration is a standard practice in the Atlantic Forest, which has produced patches with different degrees of degradation and regeneration across the landscape. The aim of this study was to evaluate the effects of replacement of native forest by pasture and natural regeneration of vegetation on soil and on soil organic matter (SOM) dynamics in the dry and rainy season in an Atlantic Forest fragment in Passa Vinte, Minas Gerais (MG), Brazil. Soil samples were collected in the rainy and dry season, at a depth of 0.00-0.05 m. The variables determined were total organic carbon (TOC) and particle-size fractions of SOM [particulate organic carbon (POC) and mineral-associated organic carbon (MOC)]; microbial activity by basal respiration (BR) and microbial biomass carbon (MBC); species richness (SR) and spore abundance (SA) of arbuscular mycorrhizal fungi (AMF); and total and easily extractable glomalin-related soil protein (T-GRSP and EE-GRSP, respectively). The conversion of native forest into pasture reduced TOC, POC, MOC, AMF-SA, T-GRSP, and EE-GRSP. However, it did not reduce MBC and BR. The fallow period in the area under natural regeneration was not long enough to restore soil TOC, POC, MOC, BR, MBC, T-GRSP, and EE-GRSP to levels approaching those observed in the forest area. Nevertheless, natural regeneration of vegetation stimulated the production of seedlings (spores) of arbuscular mycorrhizal fungi, which are important for the establishment of plant species and advance of ecological succession. Seasonality affected some of the biological soil properties and SOM dynamics.
机译:摘要在大西洋森林中,通常的做法是先去除原始植物以进行农作物和牧草生产,然后再进行自然更新,这种做法在整个景观中产生了不同程度退化和再生的斑块。这项研究的目的是评估干旱和雨季米纳斯吉拉斯州帕萨温特的大西洋森林片段中,牧场和植被的自然再生替代天然林对土壤和土壤有机质(SOM)动态的影响。 (MG),巴西。在雨季和旱季收集土壤样品,深度为0.00-0.05 m。确定的变量为总有机碳(TOC)和SOM的粒径分数[颗粒有机碳(POC)和矿物相关有机碳(MOC)];通过基础呼吸(BR)和微生物生物量碳(MBC)产生的微生物活性;丛枝菌根真菌(AMF)的物种丰富度(SR)和孢子丰度(SA);以及总的和易于提取的gloomalin相关的土壤蛋白(分别为T-GRSP和EE-GRSP)。原始森林向牧场的转化减少了TOC,POC,MOC,AMF-SA,T-GRSP和EE-GRSP。但是,它并没有减少MBC和BR。自然更新地区的休耕期不足以恢复土壤TOC,POC,MOC,BR,MBC,T-GRSP和EE-GRSP的水平,使其接近森林地区的水平。然而,植被的自然再生刺激了丛枝菌根真菌的幼苗(孢子)的产生,这对于建立植物物种和促进生态演替至关重要。季节性影响某些生物土壤特性和SOM动态。

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