<?xml version="1.0" encoding="UTF-8"?>
<rss xmlns:dc="http://purl.org/dc/elements/1.1/" version="2.0">
  <channel>
    <title>DSpace Communidade: Embrapa Solos (CNPS)</title>
    <link>https://www.alice.cnptia.embrapa.br/alice/handle/item/36</link>
    <description>Embrapa Solos (CNPS)</description>
    <pubDate>Fri, 17 Jul 2026 16:47:08 GMT</pubDate>
    <dc:date>2026-07-17T16:47:08Z</dc:date>
    <item>
      <title>Avaliação da condutividade hidráulica saturada do solo num Argissolo Amarelo, sob sistema de integração pecuária-floresta no Médio Vale do Paraíba do Sul - Rio de Janeiro.</title>
      <link>https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188324</link>
      <description>Título: Avaliação da condutividade hidráulica saturada do solo num Argissolo Amarelo, sob sistema de integração pecuária-floresta no Médio Vale do Paraíba do Sul - Rio de Janeiro.
Autoria: TEIXEIRA, W. G.; BALIEIRO, F. de C.; VASQUES, G. M.; DONAGEMMA, G. K.; GONÇALVES, A. O.; MULLER, M. D.; MARTINS, C. E.; CARVALHO FILHO, A. de
Conteúdo: Este estudo avaliou a condutividade hidráulica saturada avaliada no campo (Kfs) em um sistema de integração pecuária-floresta (IPF) no município de Valença, RJ que está implantado num Argissolo Amarelo Distrófico sob eucalipto e braquiária. O componente arbóreo atingiu maturidade aos 73 meses, com área basal de 9,22 m2 ha-1. Utilizou-se permeâmetro de poço automatizado, com poço escavado com 20 cm de profundidade. As medições abrangeram o renque (linha das árvores), a borda (na projeção da copa das árvores) e o pasto. A Kfs foi classificada como baixa em todas as posições (&lt; 3,1 mm h⁻¹). A borda (3,05mm h⁻¹) apresentou valores significativamente superiores ao renque (0,97 mm h⁻¹) e ao pasto (1,09 mm h⁻¹). A restrição hídrica decorre do adensamento no horizonte BA e da transição para o Bt, que é consequência de processos pedogenéticos e do pisoteio animal. Tais condições situam o solo no limite inferior de condutividade para Argissolos no Brasil. Conclui-se que o solo possui restrição severa ao fluxo de água. A maior densidade de raízes das espécies, na borda, favorece a conectividade de poros. Chuvas intensas geram alto risco de enxurradas pela baixa permeabilidade.</description>
      <pubDate>Thu, 01 Jan 2026 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188324</guid>
      <dc:date>2026-01-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Performance of the SWAP–WOFOST model for simulating cotton growth and yield under tropical cerrado conditions.</title>
      <link>https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188317</link>
      <description>Título: Performance of the SWAP–WOFOST model for simulating cotton growth and yield under tropical cerrado conditions.
Autoria: BENDER, E. P.; RODRÍGUEZ, L. D.; JANTALIA, C. P.; GONÇALVES, A. O.; TEIXEIRA, P. C.; LYRA, G. B.
Conteúdo: Process-based agro-hydrological models are essential tools for assessing crop growth and yield under contrasting management and environmental conditions. This study assessed the performance of the coupled Soil-Water-Atmosphere-Plant and World Food Studies Simulation Model (SWAP–WOFOST) to simulate cotton (Gossypium hirsutum L., cv. FiberMax 975 Wild Strike®) growth and yield under tropical Cerrado conditions in western Bahia, Brazil. Field experiments were carried out during the 2014/2015 growing season under three nitrogen management treatments: ammonium sulfate®, prilled urea®, and a control without nitrogen fertilization. The SWAP component was calibrated to simulate soil water dynamics, whereas WOFOST was used to represent crop growth and yield. Model performance was evaluated using the coefficient of determination (R²), Willmott’s agreement index (d-index), Root Mean Square Error (RMSE), Nash–Sutcliffe efficiency (NSE), and the performance index (c-index). The SWAP model showed limited performance in simulating soil volumetric water content, with low precision (R²), agreement (d-index) and efficiency (NSE), indicating limitations in representing near-surface soil water dynamics, particularly after rainfall events. In contrast, the WOFOST component showed excellent performance in simulating leaf area index, reproductive structure biomass, and total aboveground biomass across all treatments. These results indicate that, despite limitations in soil water content representation, the coupled SWAP–WOFOST framework was robust for simulating cotton growth and yield responses under contrasting nitrogen management strategies. The model may support assessments of crop performance and nitrogen fertilization strategies under tropical Cerrado conditions.</description>
      <pubDate>Thu, 01 Jan 2026 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188317</guid>
      <dc:date>2026-01-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Effects of the public policies on the natural rubber production in São Paulo and Mato Grosso states.</title>
      <link>https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188100</link>
      <description>Título: Effects of the public policies on the natural rubber production in São Paulo and Mato Grosso states.
Autoria: ROSADO, P. L.; TOSTO, S. G.; GOMES, M. F. M.; CARMO, C. A. F. de S. do
Conteúdo: The objective of this study was to evaluate the effects of the government intervention on the expansion of the natural rubber production in São Paulo and Mato Grosso states. The method used was the policy analysis matrix, developed by MONKE and PEARSON (1989). The results showed that the production of natural rubber in those states has conditions to face the liberalization changes that have been taking place in the international market. The government’s role in that process is relevant in order to promote the development of that activity and to reduce the distortions, since these impede that the market signals guide the producer decisions in an integrated economy into the world market. Some policy measures can be carried out to improve the competitiveness of the natural rubber in São Paulo and Mato Grosso states, which are related with reductions of the tax aliquots on the production; with interest rate in the financings; and with labor legal requirements that increase the pro-duction costs. It is, also, important to underline the positive effects of technological changes. It is necessary to the government to be conscious with the effects of its policies. For that, it is important that the adoption of those policies provides to the production of rubber natural larger competitiveness. In that perspective, the government intervention could generate larger social benefits, if the divergences between the social and the private valuations were reduced. In the medium term, the policy reorientation benefits both the producers and the consumers, taking to a larger incentive to the local production of this product. Keywords: Competitiveness, liberalization of markets, natural rubber, public policies.</description>
      <pubDate>Sat, 01 Jan 2005 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188100</guid>
      <dc:date>2005-01-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Anthropic soils in SiBCS and WRB: review of criteria and conceptualization of the Anthropic horizon.</title>
      <link>https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188104</link>
      <description>Título: Anthropic soils in SiBCS and WRB: review of criteria and conceptualization of the Anthropic horizon.
Autoria: CORDEIRO, F. R.; FONTANA, A.; ANJOS, L. H. C. dos; TEIXEIRA, W. G.
Conteúdo: The diagnostic anthropic A horizon in the Brazilian Soil Classification System (SiBCS) and the Pretic horizon in the World Reference Base for Soil Resources (WRB) comprise the surface mineral genetic horizons of soils formed under strong influence of original indigenous communities for a long time, notably in Brazil those known as Terras Pretas de Índio (TPI) or Amazonian Dark Earths (ADE). The surface horizons of these soils in Brazil are characterized by ceramic artifacts, charcoal, dark colors, and higher levels of carbon, calcium, magnesium, and phosphorus than the adjacent soils. This study aimed to propose additional quantitative criteria for the anthropic A horizon in the SiBCS and contribute to the Pretic horizon and Pretic Anthrosols in the WRB. A database of many studies on these soils was compiled, including morphological, physical, and chemical diagnostic characteristics of horizons classified as anthropic (Au) in anthropized soils. The following data was used to identify and differentiate these horizons: thickness, color (value and chroma), pH(H2O), calcium (Ca2+), magnesium (Mg2+), sum of bases (SB), cation exchange capacity (CEC), base saturation (V), available phosphorus (P – Mehlich-1 extractant), and organic carbon (Corg). For SiBCS, it is suggested to define the diagnostic anthropic A horizon based on a limit of organic carbon content (Corg) greater than or equal to 6.0 g kg-1 and a color with value ≤4 and chroma ≤3; to create the “anthropic character” for surface mineral diagnostic horizons with expressive anthropic modifications that do not meet the quantitative criteria of thickness, color, P, and Corg for the diagnostic anthropic A horizon; and to define a criteria of “anthric properties”, to be used in soils in which the surface mineral diagnostic horizons show recent and significant modifications due to agricultural and/or other activities, meeting a P content (Mehlich-1 extractant) ≥30 mg kg-1 and V ≥50 %, abrupt transition from the surface horizon to the subsequent one, and/or absence of transitional horizons AB and/or BA. In the WRB system, it is proposed that the Pretic horizon should maintain the P content (Mehlich-1 extractant) ≥30 mg kg-1, and in the Pretic Anthrosols class, to reduce the combined thickness of Pretic sub horizons to ≥0.30 m (0.30 m) within 1.00 m (1.00 m) of the mineral soil surface.</description>
      <pubDate>Thu, 01 Jan 2026 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://www.alice.cnptia.embrapa.br/alice/handle/doc/1188104</guid>
      <dc:date>2026-01-01T00:00:00Z</dc:date>
    </item>
  </channel>
</rss>

