Has experience in Agronomy, focusing on Soil Genesis, Morphology and Classification, Soil Management, Soil Organic Matter, and Ethnopedology. Member of SSSA since 1979, and Head of Soil in Space and Time Division of Brazilian Soil Science Society, from 2011 to July 2019. Member of IUSS WG for developing the World Reference Base for Soil Resources (WRB). Coordinator of the Graduate Program in Science, Technology and Innovation in Agriculture (UFRRJ and Universidad Nacional de Rio Cuarto - UNRC), Brasil-Argentina, from 2009 to 2016. Organizing committee of 21st World Congress of Soil Science, held in Rio in August 2018. Member of the National Executive Committee of PronaSolos (MAPA), 2020 to July 2021. Expert member of the Intergovernmental Technical Panel on Soils (ITPS) - FAO/ Global Soil Partnership (GSP), 2018 - 2025. Lead of ITPS working group - Black Soils Report, 2020_2022. President of Brazilian Soil Science Society (SBCS), 2019 to 2023.
EDUCATION
Graduate in Agronomy from Federal Rural University of Rio de Janeiro - UFRRJ, Master Science in Agronomy from UFRRJ, and Ph.D and Pos-doctorate in Agronomy - Soil Science from Purdue University, USA.
RESEARCH, TEACHING, or OTHER INTERESTS
Soil Science, Agronomy and Crop Science, Multidisciplinary, General Earth and Planetary Sciences
152
Scopus Publications
19151
Scholar Citations
45
Scholar h-index
167
Scholar i10-index
Scopus Publications
Exchangeable cations determined by different methods: Implications for soil classification and evaluation Ademir Fontana, Lúcia Helena Cunha dos Anjos, Vitor Peruzzi de Almeida, Débora Liriel Kerber Kempner, Taciara Zborowski Horst, et al. Revista Brasileira De Ciencia do Solo, 2026 For a comprehensive and global evaluation of soils, it is essential to define common diagnostic properties among classification or interpretative systems. Specifically, in soil taxonomy, the Brazilian Soil Classification System (SiBCS) adopts analytical methods that differ from those used in international systems such as the World Reference Base for Soil Resources (WRB) and the Soil Taxonomy (ST). In the chemical properties, differences are observed in the determination of exchangeable basic cations and potential acidity (H+Al), as well as derived properties such as the sum of bases (SB), cation exchange capacity (CEC pH7 ), and base saturation (V). This study aimed to: (i) to compare the values of H+Al, SB, CEC, and V in Brazilian soils determined by different analytical methods; (ii) to propose regression models to harmonize values of the properties obtained through different analytical procedures; and (iii) to compare the threshold values of diagnostic properties used as classification criteria in the SiBCS with those adopted by WRB and ST. A representative database of Brazilian soils published in the Brazilian Soil Data Repository (SoilData) was used, comprising 2,217 samples from surface horizons and 3,726 from subsurface horizons. Values of SB, CEC, and V for surface and subsurface horizons, obtained using the methods applied in the SiBCS, were lower than those determined by the WRB and ST methods. The difference in the estimated V values was below 5 %, which falls within the analytical error range. Thus, the SiBCS criteria of V ≥50 % for identifying eutrophic character and >65 % for defining a chernozemic A horizon were found to be high, and they tend to underestimate several Brazilian soil classes, particularly those classified as Chernossolos, as well as the misclassification of anthropic and other soils modified by agricultural practices. It is proposed that the SiBCS adopt thresholds similar to those used in WRB and ST for base saturation, or alternatively, apply regression equations to improve correspondence among the systems.
Anthropogenic soils of Sambaqui middens in Maranhão, Brazil: P forms, genesis and classification Amanda Sales Alves, Marcos Gervasio Pereira, Marcelino Silva Farias, Matheus da Silva de Carvalho, Alice Maria Goulart Ribeiro, et al. Revista Brasileira De Ciencia do Solo, 2026 The activities of people who lived on the Brazilian coast since the Holocene have mainly determined the formation of Sambaqui (= shell mound) soils. Residues from shells and other animals and plants used as food by these people were deposited, resulting in soils with high levels of phosphorus (P) and organic carbon, as well as high base saturation. This study aimed to evaluate P fractions, establish possible relationships between P measurement methods in the soil profiles of Sambaqui formations, and contribute to the definition of a soil class in the Brazilian Soil Classification System (SiBCS) that describes anthropogenic pedogenesis. Three soil profiles with records of anthropogenic activity were selected and sampled for this study, all in São José de Ribamar, Maranhão, Brazil. Soil morphology was described, the physical and chemical properties of the horizons were analyzed, and the profiles were classified according to the SiBCS. Available P was extracted by different methods, and P was fractionated. Surface horizons of profiles P2 and P3 were identified as anthropogenic A, with dark colors, presence of shells, high calcium and organic carbon concentrations, high base saturation, and P content greater than 30 mg kg -1 of soil. Of the available P extractants, Mehlich-3 withdrew the highest P concentrations. Olsen method was positively correlated with pH values, shell presence, and calcium carbonate levels. Phosphorus fractionation of the studied profiles indicated highest representation of the occluded and available P fractions (Mehlich-3). According to the SiBCS, the profiles were classified as Cambissolo Háplico Carbonático (P1 and P3) and Cambissolo Háplico Ta Eutrófico (P2), and an anthropogenic subgroup was proposed for P2 and P3. Based on the World Reference Base (WRB), the profiles were classified as Pretic Calcaric Cambisol (P1) and Pretic Anthrosols (P2 and P3). In other words, the WRB classifies these soils at a high hierarchical level (as Anthrosols or by the main qualifier Pretic), in contrast with the SiBCS.
Espodossolos of Brazil: A review of structure and composition of classes Andressa Rosas de Menezes, Ademir Fontana, Lúcia Helena Cunha dos Anjos Revista Brasileira De Ciencia do Solo, 2025 Soil taxonomic systems seek to express pedogenic processes in their classes by choosing attributes or differential characteristics to identify classes at different categorical or hierarchical levels. Due to the advancement of knowledge, classification systems are periodically revised and/or expanded, and this may happen based on the evaluation of the database of these attributes or characteristics for a given class. In this context, the analysis of a broad set of Espodossolos (the equivalent of Spodosols or Podzols) from different pedoenvironments in Brazil is considered relevant to support the improvement of the categorization of this order in the Brazilian Soil Classification System – SiBCS. This study aimed to classify the profiles in the database and, based on their distribution, propose the restructuring of the Espodossolos classes up to the fourth categorical level in the SiBCS. Data from profiles with spodic horizons and the Espodossolos available in the literature, including surveys since 1960, were compiled in an electronic spreadsheet, displaying the morphological, physical, and chemical attributes. In the current edition of SiBCS, there are limitations in clearly separating the Espodossolos at the order and suborder levels due to the definitions adopted for the diagnostic attributes and the control section of the spodic B horizon. From the data base of compiled profiles, at the great group level, the soils are mostly identified in the Órticos class, in the subgroup as espessarênicos, arênicos and típicos, with few profiles or absence of profiles in the êutricos, êutricos arênicos and carbonáticos classes. Based on this assessment, it is proposed, for the order level, the reduction of the control section of the spodic B horizon to start within 2.00 m of depth; for the suborder, a criterion based on the organic carbon contents separating two classes: Humilúvicos and Háplicos. In the great group, based on the criterion of starting depth of spodic B horizon: Hiperespessos, Espessos and Órticos; and in the subgroup to adopt the classes of tiônicos, organossólicos, húmicos, saprolíticos, dúricos, fragipânicos, abrúpticos, hidromórficos, espessarênicos and típicos.
Espodossolos in Brazil: A review of the criteria and conceptualization of the spodic B horizons Andressa Rosas de Menezes, Ademir Fontana, Lúcia Helena Cunha dos Anjos Revista Brasileira De Ciencia do Solo, 2025 The absence of quantitative limits for the diagnostic attributes that define spodic B horizons in the Brazilian Soil Classification System (SiBCS) allows the inclusion of soils in the Espodossolos (the equivalent of Spodosols or Podzols) classes that contradict the classical concepts that define the podzolization process, by including horizons with low organic carbon (C org ) content, and with alkaline pH, high sum of bases and sodic or solodic characteristics. This study aimed to propose quantitative criteria and limits to identify spodic B horizons and to contribute to the hieraquical structure of SiBCS. Morphological, physical and chemical attributes were defined after analyzing a large set of spodic B horizons of profiles classified as Espodossolos in the SiBCS available in the literature. In total, 385 spodic B horizons were identified. From this total, they were identified as following: 93 as Bs(m), 127 as Bh(m) and 165 as Bhs(m). In terms of color, the main hues were 7.5YR and 10YR, while the value and the chroma were ≥4 in Bs(m), <4 in Bh(m) and a wide variation in Bhs(m). The means and medians of the C org contents are 7.5 and 6.7 g kg -1 for Bs(m), 19.8 and 15.1 g kg -1 for Bh(m), and 19.0 and 14.5 g kg -1 for Bhs(m). When the limit of C org content is established as ≥3.0 g kg -1 , 90 % of the spodic horizons are included in this group, with 85 % of the horizons for C org ≥4.0 g kg -1 and 81 % of the horizons for C org ≥5.0 g kg -1 . The pH(H 2 O) had 94 % of the spodic B horizons with values ≤5.9. Around 48 % of the spodic B horizons have Al o and Fe o data and, by calculating the equation Al o + 0.5 Fe o , around 47 % of the horizons have a value ≥0.25 %. The evaluation highlighted the potential for adopting the minimum C org ≥5.0 g kg -1 and pH(H 2 O) ≤5.9 as quantitative limits for defining the spodic B horizon in the SiBCS. It is also suggested to apply a lower requirement for the C org content in spodic horizons with very low clay content that is sand texture classes, using the values of C org ≥3.0 or ≥4.0 g kg -1 as limits. Otherwise, the minimum C org value proposed is 5.0 g kg -1 and the types of spodic B horizons could be differentiated using a second limit of C org , distinguishing the Bs with a content of C org between 5.0 and 15.0 g kg -1 and Bsh ≥15.0 g kg -1 .
Saturated hydraulic conductivity and steady-state infiltration rate database for Brazilian soils Marta Vasconcelos Ottoni, Wenceslau Geraldes Teixeira, Aline Mari Huf dos Reis, Letícia Guimarães Pimentel, Luciana Rodrigues Souza, et al. Revista Brasileira De Ciencia do Solo, 2025 Soil saturated hydraulic conductivity (Ksat) and steady-state infiltration rate (SSIR) are essential and necessary soil properties for different geoscience applications. Values of these hydraulic properties for the Brazilian territory are difficult to access and are dispersed in research efforts carried out around the country. This study developed an easy-to-manipulate, freely accessible database of soil saturated hydraulic conductivity, comprising field and laboratory analyses, and steady-state infiltration rates for Brazilian soils. This database was named Ksat-SSIR-DB. One analysis of the Ksat-SSIR-DB aimed to evaluate its coverage in Brazilian territory and in different soil groups. Average values of these hydraulic properties were also presented for textural classes, with values compared to those reported in international literature, and for other groupings, such as soil class, land use class, and porosity class. The variability of Ksat data in these groupings and in their combinations were also analyzed. The Ksat-SSIR-DB showed broad national coverage, comprising a total of 2,579 records, corresponding to 409 sampling sites, with Ksat and/or SSIR data and other associated soil information. A significant difference was observed between Ksat values for the vast majority of Brazilian clayey and very clayey soils compared to soils from the same textural groups from temperate regions. The two groupings that presented the lowest variability in terms of Ksat standard deviation values were the combination of textural classes with soil classes at the second category level of SiBCS (Brazilian Soil Classification System), and porosity classes with soil classes at the second category level of SiBCS. The Ksat-SSIR-DB has enormous potential for developing and testing Ksat pedotransfer functions in Brazilian soils, serving as a reference source for different geoenvironmental applications and, in particular, for modeling land surface processes. It is open access and can be accessed at https://www.sgb.gov.br/ksat-ssir-dbbase-de-dados-de-condutividade-hidraulica-saturada-e-de-taxa-de-infiltracao-basica-emsolos-brasileiros , which also includes the python script for data analysis.
PEDOTRANSFER FUNCTIONS IN THE ASSESSMENT OF FRAGILE MOUNTAINOUS AREAS: CARBON AND NITROGEN STOCKS IN MOUNTAINS IN SOUTHEASTERN BRAZIL Melania Merlo Ziviani, Elias Mendes Costa, Amanda Sales Alves, Luiz Alberto da Silva Rodrigues Pinto, Marcos Gervasio Pereira, et al. Revista De Gestao Social E Ambiental, 2024 Objective: This study aimed to obtain the Bd of organic constitution horizons through PTFs and evaluate the C and N stocks of different soil classes found in the upper part of the INP. Theoretical framework: The evaluation of bulk density (Bd) depends on the method used to obtain the sample and presents great spatial variability, especially in mountainous regions such as the upper part of Itatiaia National Park (INP), Brazil. Techniques can be used for this purpose, including those of pedotransfer functions (PTFs) allowing the quantification of nutrients such as C and N in soils. Methodology: The research was conducted within the Itatiaia National Park (INP), situated in the Mantiqueira Mountains of southeastern Brazil. Soil samples were collected from the upper portion of the INP, specifically targeting soil profiles containing hystic horizons (O or H). The study employed pedotransfer functions (PTFs) established by Beutler et al. (2017) to estimate the soil bulk density (Bd) of organic horizons. Based on these assessments, stocks of carbon (C) and nitrogen (N) were calculated. The standard depth for these calculations was 30 cm. In total, 47 profiles were selected, 26 of which belonged to the order Histosols, 15 to Cambisols, and 6 Leptosols & Regosols. Results and conclusion: In general, a high C content, between 5 and 15 g kg-1, and N contents greater than 1.0 g kg-1 were observed. For Bd an increase in depth occurred, with values close to 0.50 Mg m-3 in the superficial horizons and > 0.75 Mg m-3 in depths greater than 30 cm. The area occupied by soil profiles presenting hystic horizons corresponds to 16403.69 ha (hectares) with 315645.7 Mg of C and 20043.0 Mg of N. Of this total, 10254.44 ha were Cambisols that store approximately 205282.1 Mg of C and 13121.8 Mg of N. Histosols occupied an area of 4148.38 ha and stored 90698.4 Mg of C and 5576.0 Mg of N. The area occupied by Leptosols & Regosols was 1347.74 ha and they stored 19665.1 Mg of C and 1345.1 Mg of N. For the Cambisols, the average values of C and N stocks were lower than those quantified in the Histosols, but considering the area occupied, the total C stock was more than twice the amount quantified in the Histosols. Research implications: Soils with organic horizons complicate Bd determination due to costly and unrepresentative collection methods. Additionally, converting soil masses to volume for nutrient stock measurements (e.g., C and N) is problematic. Due to limited accessibility in certain areas, obtaining undisturbed soil samples for evaluation can be challenging. In such cases, pedotransfer functions (PTFs) play a crucial role in assessing and modeling soil phenomena. Indirect quantification of Bd using PTFs has become essential for addressing these issues. Originality/value: This study utilizes pedotransfer functions (PTFs) to estimate soil bulk density (Bd) and, consequently, nutrient stocks in fragile mountainous soils, enabling monitoring of these environments.
Mapping soil properties in a poorly-accessible area Elias Mendes Costa, Helena Saraiva Koenow Pinheiro, Lúcia Helena Cunha dos Anjos, Robson Altiellys Tosta Marcondes, Yuri Andrei Gelsleichter Revista Brasileira De Ciencia do Solo, 2020
Alluvial soil formation in the plains of northeastern Brazil Rafael Cipriano-Silva, Gustavo Souza Valladares, Antônio Carlos de Azevedo, Lúcia Helena Cunha dos Anjos, Marcos Gervasio Pereira, et al. Revista Brasileira De Ciencia do Solo, 2020
Soil fauna changes across Atlantic Forest succession Maria Elizabeth Fernandes Correia, Rodrigo Camara, Claudia Reis Ferreira, Alexander Silva Resende, Lúcia Helena Cunha dos Anjos, et al. Comunicata Scientiae, 2018
Humic substances and phosphorus fractions in areas with crop-livestock integration, pasture and natural cerrado vegetation in Goiás, Brazil Tropical and Subtropical Agroecosystems, 2015
Oxidizable organic carbon fractions and soil aggregation in areas under different organic production systems in Rio de Janeiro, Brazil Tropical and Subtropical Agroecosystems, 2011
Carbon, light organic matter and oxidizable organic carbon fractions in different organic production systems Comunicata Scientiae, 2010
Pasture edaphic attributes in northwest region of Rio de Janeiro State, Brazil Comunicata Scientiae, 2010
Litter contribution and decomposition and root biomass production in forests at different sucessional stages in pinheiral, RJ Ciencia Florestal, 2010
Soil fertility of cultivated pastures under different managements in the northwest Rio de Janeiro Revista Brasileira De Engenharia Agricola E Ambiental, 2010
Anthropic soils in SiBCS and WRB: Review of criteria and conceptualization of the Anthropic horizon FR Cordeiro, A Fontana, LHC Anjos, WG Teixeira Revista Brasileira de Ciência do Solo 50 (spe1), e0250048 , 2026 2026
Exchangeable cations determined by different methods: Implications for soil classification and evaluation A Fontana, LHC Anjos, VP Almeida, DLK Kempner, TZ Horst, ... Rev. Bras. Ciênc. Solo 50, - , 2026 2026
Anthropogenic soils of Sambaqui middens in Maranhão, Brazil: P forms, genesis and classification AS Alves, MG Pereira, MS Farias Filho, MS Carvalho, AMG Ribeiro, ... Revista Brasileira de Ciência do Solo 50 (spe1), e0250036 , 2026 2026
USE OF THE NORMALIZED DIFFERENCE VEGETATION INDEX (NDVI) IN MAPPING LAND COVER CHANGES IN MINING AREAS IN THE SERTÃO OF PARAÍBA. JC de Amorim, DD de Araújo Ferreira, AC de Souza Ferreira, ... Environmental & Social Management Journal/Revista de Gestão Social e … , 2025 2025
Espodossolos of Brazil: A review of structure and composition of classes AR Menezes, A Fontana, LHC Anjos Revista Brasileira de Ciência do Solo 49, e0240117 , 2025 2025
Espodossolos in Brazil: A review of the criteria and conceptualization of the spodic B horizons AR Menezes, A Fontana, LHC Anjos Revista Brasileira de Ciência do Solo 49, e0240116 , 2025 2025 Citations: 2
Classes de solos do estado do Maranhão. MG PEREIRA, LHC dos ANJOS, MB SILVA, ML MENDONÇA-SANTOS, ... 2025
Distribuição das substâncias húmicas e a relação com as propriedades químicas em horizontes diagnósticos superficiais de solos brasileiros. EP FERREIRA, A FONTANA, MG PEREIRA, VM BENITES, ... 2025
Espodossolos in Brazil: a review of the criteria and conceptualization of the spodic B horizons. AR de Menezes, A Fontana, LHC dos Anjos 2025
Saturated hydraulic conductivity and steady-state infiltration rate database for Brazilian soils MV Ottoni, WG Teixeira, AMH Reis, LG Pimentel, LR Souza, ... Revista Brasileira de Ciência do Solo 49, e0240003 , 2025 2025 Citations: 13
Importância e aplicações do nível de subgrupo do Sistema Brasileiro de Classificação de Solos-SiBCS. HG dos SANTOS, LHC dos ANJOS, VA de OLIVEIRA, PKT JACOMINE, ... 2025
Humic fractions as support for the classification of high-mountain Organossolos in the southeast of Brazil MM Ziviani, LH Silva, JPC Scott, AS Alves, LASR Pinto, MS Motta, ... Revista Brasileira de Ciência do Solo 48, e0240005 , 2024 2024
Análise espacial da estrutura da paisagem no entorno da Área de Relevante Interesse Ecológico (ARIE) Floresta da Cicuta, sul do Estado do Rio de Janeiro, Brasil MFV Junior, ERP Junior, WK de Freitas, LHC dos Anjos REVISTA DELOS 17 (62), e3014-e3014 , 2024 2024
Drivers of carbon stabilization and sequestration in Brazil’s black soils CRP Junior, LP Canisares, MC Abreu, GB Lyra, AP de Oliveira, ... Catena 246, 108451 , 2024 2024 Citations: 6
Status of the World's Soils P Smith, RM Poch, DA Lobb, R Bhattacharyya, G Alloush, GD Eudoxie, ... Annual review of environment and resources 49 (1), 73-104 , 2024 2024 Citations: 143
Aerogeophysical Data to Modeling Soil Properties: A Study Case in Bom Jardim—RJ BP Bastos, HSK Pinheiro, W de Carvalho Junior, LHC dos Anjos Pedometrics in Brazil, 159-170 , 2024 2024
MultiSoils: A Digital Platform for Information Search and Project Management in Soil Science MB Ceddia, EFM Pinheiro, JP Larangeira, J de Abreu Soares, RC Mauro, ... Pedometrics in Brazil, 1-14 , 2024 2024
Aerogeophysical Data to Modeling Soil Properties: A Study Case in Bom W de Carvalho Junior, LHC dos Anjos Pedometrics in Brazil, 159 , 2024 2024
Proximal sensor characterization of Haitian agricultural soils: A case study in the Central Plateau R Cean, M Mancini, SHG Silva, N Bakr, S Chakraborty, B Li, A Acree, ... Journal of South American Earth Sciences 143, 105007 , 2024 2024 Citations: 3
MOST CITED SCHOLAR PUBLICATIONS
Sistema Brasileiro de Classificação de Solos HG SANTOS, PKT JACOMINE, LHC ANJOS, VÁ OLIVEIRA, ... 2018.0 Citations: 9605
World reference base for soil resources FAO ISRIC World soil resources reports 84 , 1998 1998.0 Citations: 1838
Aggregate distribution and soil organic matter under different tillage systems for vegetable crops in a Red Latosol from Brazil EFM Pinheiro, MG Pereira, LHC Anjos Soil and Tillage research 77 (1), 79-84 , 2004 2004.0 Citations: 347
Agregação, carbono e nitrogênio em agregados do solo sob plantio direto com integração lavoura-pecuária A Loss, MG Pereira, SG Giácomo, A Perin, LHC Anjos Pesquisa agropecuária brasileira 46 (10), 1269-1276 , 2011 2011.0 Citations: 187
The Brazilian soil spectral library (BSSL): A general view, application and challenges JAM Demattê, AC Dotto, AFS Paiva, MV Sato, RSD Dalmolin, ... Geoderma 354, 113793 , 2019 2019.0 Citations: 174
Do more detailed environmental covariates deliver more accurate soil maps? A Samuel-Rosa, GBM Heuvelink, GM Vasques, LHC Anjos Geoderma 243, 214-227 , 2015 2015.0 Citations: 160
Brazilian system of soil classification HG Santos, PKT Jacomine, LHC Anjos, VA Oliveira, JF Lumbreras, ... Rio de Janeiro: Empresa Brasileira de Pesquisa Agropecuária , 2018 2018.0 Citations: 153
Topography and spatial variability of soil physical properties MB Ceddia, SR Vieira, ALO Villela, LS Mota, LHC Anjos, DF Carvalho Scientia Agricola 66 (3), 338-352 , 2009 2009.0 Citations: 147
Status of the World's Soils P Smith, RM Poch, DA Lobb, R Bhattacharyya, G Alloush, GD Eudoxie, ... Annual review of environment and resources 49 (1), 73-104 , 2024 2024.0 Citations: 143
Dynamics of soil aggregation and organic carbon fractions over 23 years of no-till management C dos Reis Ferreira, EC da Silva Neto, MG Pereira, ... Soil and Tillage Research 198, 104533 , 2020 2020.0 Citations: 136
Proposição de valores de referência para a concentração natural de metais pesados em solos brasileiros FS Fadigas, N Sobrinho, A MB, N Mazur, LHC dos Anjos, AA Freixo Revista Brasileira de Engenharia Agrícola e Ambiental 10, 699-705 , 2006 2006.0 Citations: 114
Propriedades químicas e biológicas de solo de tabuleiro cultivado com cana-de-açúcar com e sem queima da palhada HNS Mendonza, E Lima, LHC Anjos, LA Silva, MB Ceddia, MVM Antunes Revista Brasileira de Ciência do Solo 24 (1), 201-207 , 2000 2000.0 Citations: 112
JF (2018) HG Santos, PKT Jacomine, LHC Anjos, VA Oliveira, JF Lumbreras, ... Sistema brasileiro de classificação de solos 5 , 0 Citations: 108
Relação entre acidez e outros atributos químicos em solos com teores elevados de matéria orgânica AG Ebeling, LHC Anjos, DV Perez, MG Pereira, GS Valladares Bragantia 67 (2), 429-439 , 2008 2008.0 Citations: 100
Adsorção de fósforo em solos de argila de atividade baixa GS Valladares, MG Pereira, LHC Anjos Bragantia 62 (1), 111-118 , 2003 2003.0 Citations: 94
Concentrações naturais de metais pesados em algumas classes de solos brasileiros FS Fadigas, NMB Amaral-Sobrinho, N Mazur, LHC Anjos, AA Freixo Bragantia 61 (2), 151-159 , 2002 2002.0 Citations: 92
Sistemas de colheita da cana-de-açúcar e alterações nas propriedades físicas de um solo Podzólico Amarelo no Estado do Espírito Santo MB Ceddia, LHC Anjos, E Lima, A Ravelli Neto, LA Silva Pesquisa Agropecuária Brasileira 34, 1467-1473 , 1999 1999.0 Citations: 92
Análise dos componentes principais e métodos multicritério ordinais no estudo de Organossolos e solos afins GS Valladares, EG Gomes, JCCB Soares de Mello, MG Pereira, ... Revista Brasileira de Ciência do Solo 32, 285-296 , 2008 2008.0 Citations: 88
Macrofauna edáfica em estádios sucessionais de Floresta Estacional Semidecidual e pastagem mista em Pinheiral (RJ): Rio de Janeiro State CEG Menezes, MEF Correia, MG Pereira, I Batista, KM Rodrigues, ... Revista Brasileira de Ciência do Solo 33, 1647-1656 , 2009 2009.0 Citations: 86
