Bruna Emanuele Schiebelbein, R. Bordonal, C. Cerri, D. Oliveira, M. Cherubin
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In each area, a LUC chronosequence was evaluated: native vegetation (NV), pasture (PA), short-term sugarcane (SC1), the area analyzed during the sugarcane plant cycle; long-term sugarcane (SC2), area analyzed during the ratoon sugarcane cycle. In each use, undisturbed and disturbed samples were collected and macroaggregates and microaggregates were obtained by wet sieving and soil samples. In these samples, the physical fractionation of the SOM and the calculation of the C contained in each fraction of the SOM and C total stock of each use were performed. The conversion of NV to PA increased C stocks by more than 50 %, mainly in the MAOM fraction, and maintenance of macroaggregates (more than 80 %) in sandy site; and reduction of C stocks by more than 30 %, mainly MAOM in the clayey area. These benefits acquired from grazing on sandy area were lost with the expansion of sugarcane, a reduction of more than 20 % in macroagregation and C stocks. The sugarcane expansion into pasture with clayey site resulted in C accumulation (more than 2 Mg C ha -1 yr -1 ) and recovery of stocks on a SC2 basis. Expanding sugarcane areas into low-productivity pasture areas can be considered a sustainable strategy, especially in clayey soils, in which multiple gains occur through C sequestration and improved soil quality, as well as the reduction of CO 2 emissions through the diversification of the energy matrix with the production of ethanol.","PeriodicalId":21215,"journal":{"name":"Revista Brasileira De Ciencia Do Solo","volume":"1 1","pages":""},"PeriodicalIF":1.9000,"publicationDate":"2023-07-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Mineral-associated and particulate organic matter in aggregates as a proxy for soil C changes in pasturesugarcane land use transitions\",\"authors\":\"Bruna Emanuele Schiebelbein, R. Bordonal, C. Cerri, D. 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In each area, a LUC chronosequence was evaluated: native vegetation (NV), pasture (PA), short-term sugarcane (SC1), the area analyzed during the sugarcane plant cycle; long-term sugarcane (SC2), area analyzed during the ratoon sugarcane cycle. In each use, undisturbed and disturbed samples were collected and macroaggregates and microaggregates were obtained by wet sieving and soil samples. In these samples, the physical fractionation of the SOM and the calculation of the C contained in each fraction of the SOM and C total stock of each use were performed. The conversion of NV to PA increased C stocks by more than 50 %, mainly in the MAOM fraction, and maintenance of macroaggregates (more than 80 %) in sandy site; and reduction of C stocks by more than 30 %, mainly MAOM in the clayey area. These benefits acquired from grazing on sandy area were lost with the expansion of sugarcane, a reduction of more than 20 % in macroagregation and C stocks. 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引用次数: 0
摘要
为了满足对乙醇等生物能源日益增长的需求,甘蔗种植面积已经扩大,特别是在目前被粗放型低生产力牧场占据的地区。然而,从牧场到甘蔗的土地利用变化(LUC)意味着土壤结构的变化和土壤有机质(SOM)的变化。本研究旨在量化土地利用对不同质地土壤中有机质组分-颗粒有机质(POM)和矿物相关有机质(MAOM)的影响,并探讨土壤团聚体的可能变化与碳(C)储量和有机质组分的影响之间的相关性。该研究在巴西中南部的两个地区进行,一个是粘土土,另一个是沙土。每个区域的LUC时序分析为:原生植被(NV) -草地(PA) -短期甘蔗(SC1) -甘蔗植物周期分析区域;长期甘蔗(SC2),面积分析在再生甘蔗周期。在每次使用中,收集未扰动和扰动的样品,并通过湿筛和土壤样品获得大团聚体和微团聚体。在这些样品中,对SOM进行了物理分馏,并计算了SOM每个馏分中所含的C和每种用途的C总存量。NV向PA的转化增加了50%以上的碳储量,主要是在MAOM部分,并维持了沙质场地的大团聚体(80%以上);碳储量减少30%以上,主要是粘土区的MAOM。这些从沙地放牧中获得的收益随着甘蔗种植的扩大而丧失,大聚集体和碳储量减少了20%以上。甘蔗扩展到具有粘土场地的牧场,导致碳积累(超过2 Mg C / ha -1年-1)和种群在SC2基础上的恢复。将甘蔗种植面积扩大到低生产力的牧场地区可以被认为是一种可持续的战略,特别是在粘土土壤中,通过碳封存和改善土壤质量,以及通过生产乙醇使能源基质多样化来减少二氧化碳排放,可以获得多重收益。
Mineral-associated and particulate organic matter in aggregates as a proxy for soil C changes in pasturesugarcane land use transitions
To meet the growing demand for bioenergy such as ethanol, the area cultivated with sugarcane has expanded, especially in areas currently occupied by extensive pastures with low productivity. However, land-use change (LUC) from pasture to sugarcane implies changes in soil structure and variations in organic matter (SOM) stored in the soil. This study aimed to quantify the impact of LUC on organic matter fractions – particulate organic matter (POM) and mineral-associated organic matter (MAOM) – in soils with contrasting textures, and to explore the correlations between possible alterations in soil aggregation and the effects on carbon (C) stocks and SOM fractions. The study was conducted in two areas in Central-Southern Brazil, one with clayey soil and the other with sandy soil. In each area, a LUC chronosequence was evaluated: native vegetation (NV), pasture (PA), short-term sugarcane (SC1), the area analyzed during the sugarcane plant cycle; long-term sugarcane (SC2), area analyzed during the ratoon sugarcane cycle. In each use, undisturbed and disturbed samples were collected and macroaggregates and microaggregates were obtained by wet sieving and soil samples. In these samples, the physical fractionation of the SOM and the calculation of the C contained in each fraction of the SOM and C total stock of each use were performed. The conversion of NV to PA increased C stocks by more than 50 %, mainly in the MAOM fraction, and maintenance of macroaggregates (more than 80 %) in sandy site; and reduction of C stocks by more than 30 %, mainly MAOM in the clayey area. These benefits acquired from grazing on sandy area were lost with the expansion of sugarcane, a reduction of more than 20 % in macroagregation and C stocks. The sugarcane expansion into pasture with clayey site resulted in C accumulation (more than 2 Mg C ha -1 yr -1 ) and recovery of stocks on a SC2 basis. Expanding sugarcane areas into low-productivity pasture areas can be considered a sustainable strategy, especially in clayey soils, in which multiple gains occur through C sequestration and improved soil quality, as well as the reduction of CO 2 emissions through the diversification of the energy matrix with the production of ethanol.
期刊介绍:
The Revista Brasileira de Ciência do Solo is a scientific journal published by the Brazilian Society for Soil Science (SBCS), founded in 1947, and is responsible for the propagation of original and inedited technical-scientific work of interest for Soil Science.
Contributions must not have been previously published or submit to other periodicals, with the only exception of articles presented in summarized form at professional meetings. Literature reviews are accepted when solicited by the Editorial Board.