Limestone Dissolution Under Varying Rates and Soil Textures-Reference-Cited by-同舟云学术

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Limestone Dissolution Under Varying Rates and Soil Textures

Published:2023-10-25 Issue: Volume: Page:1-10
ISSN:0010-3624
Container-title:Communications in Soil Science and Plant Analysis
language:en
Short-container-title:Communications in Soil Science and Plant Analysis

Author:

Garcez Tiago Barreto¹,Pogorzelski Denison²,Santos Wedisson Oliveira³,Matias Patrícia Cardoso²,Ballotin Fabiane²^ORCID,Cantarutti Reinaldo Bertola²

Affiliation:

1. Soil Department, Universidade Federal de Sergipe, Vicosa, Brazil

2. Departamento de Solos, Universidade Federal de Viçosa, Viçosa, Brazil

3. Laboratory of Soil and Plant Analysis, Institute of Agricultural Sciences, Universidade Federal de Uberlândia, Vicosa, Brazil

Publisher

Informa UK Limited

Subject

Soil Science,Agronomy and Crop Science

Link

https://www.tandfonline.com/doi/pdf/10.1080/00103624.2023.2274030

Reference17 articles.

1. Determinação e uso do fósforo remanescente;Alvarez V. H.;B Inf SBCS,2000

2. Soil structure and greenhouse gas emissions: a synthesis of 20 years of experimentation

3. The effects of pH on phosphate uptake from the soil

4. Bloom, P. R. 2000. Soil pH and pH buffering. In Handbook of soil science, ed. M. E. Sumner, 333–52. Baco Raton, Florida: CRC Press.

5. Estimating specific surface area and cation exchange capacity in soils using fractal dimension of particle-size distribution

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