Testing the Feasibility of Usumacinta River Sediments as a Renewable Resource for Landscaping and Agronomy

Author:

Hussain Mazhar12,Levacher Daniel1ORCID,Leblanc Nathalie2ORCID,Zmamou Hafida2,Djeran-Maigre Irini3ORCID,Razakamanantsoa Andry4ORCID

Affiliation:

1. UMR 6143 CNRS—M2C, Normandie Université, Unicaen, 24 Rue des Tilleuls, 14000 Caen, France

2. UniLaSalle, Université d’Artois, EA7519—Transformations & Agro-Ressources, Normandie Université, 76130 Mont Saint Aignan, France

3. INSA Lyon, Laboratoire GEOMAS, Université Lyon, 69621 Villeurbanne, France

4. Département GERS, Université Gustave Eiffel, 44344 Bouguenais, France

Abstract

Fluvial sediment recycling in agronomy is a relatively recent development, as sediment fertilizing potential for crops is unexplored. Freshwater sediments can act as fertilizer and improve the aeration of soils to increase the yield of crops, support vegetation for landscaping, and provide protective cover against erosion. This study focuses on the investigation of the agronomic potential of Usumacinta River sediments. The pH of the sediments is around 8.5, which is slightly alkaline. The organic matter content is low (5.7%). The sodium absorption ratio is 1.2 and the electrical conductivity is low (0.02 mS/cm). These values indicate that sediments are nonsaline, which is essential for the growth of crops and vegetation. The environmental characteristics of sediments show that the heavy metals, polycyclic aromatic hydrocarbon (PAH), and polychlorinated biphenyl (PCB) pollutants in sediments are below the recommended thresholds. In addition, sediments from the Usumacinta River contain minerals such as potassium and iron oxides that are helpful in improving the biological and nutritional characteristics of the soil. Furthermore, the pH, granulometry, mineralogy, organic matter, and carbonate contents of the Usumacinta River sediments are similar to agronomic soils. The Usumacinta River sediment’s potential for agronomy was practically investigated by sowing ryegrass (Lolium perenne) in a greenhouse by using the local climatic conditions and mixing sediments with potting soil. Three soil compositions were used to evaluate the germination and growth of ryegrass. The soil compositions were 100% potting soil (C1), 50% sediments + 50% potting soil (C2), and 100% sediments (C3). The growth rate of ryegrass was evaluated by monitoring the increase in grass height and production of fresh biomass. The germination of ryegrass was similar in all three compositions. The growth of ryegrass and production of fresh biomass were the most significant with 100% potting soil (0.25 kg/m2), somewhat less with sediment mix (0.18 kg·m2), and were the least significant with 100% sediments (0.05 kg/m2). The mixture of potting soil and sediments shows similar growth to 100% potting soil. The ryegrass seed germination, growth, and production of fresh biomass with the mixture of sediments gave encouraging results, and underlined the potential of sediments for soil amendments for agronomy and protective developments, such as limiting riverbank erosion, gardening, and landscaping.

Funder

“From traditional uses to an integrated valorization of sediments in the Usumacinta River basin (VAL-USES)” from the Agence Nationale de la Recherche of France

Consejo Nacional de Ciencia y Tecnología of Mexico

Publisher

MDPI AG

Subject

Management, Monitoring, Policy and Law,Renewable Energy, Sustainability and the Environment,Geography, Planning and Development,Building and Construction

Reference43 articles.

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2. (2016). Qualité du Sol—Détermination du pH (Standard No. AFNOR NF ISO 10390).

3. (2016). Qualité du Sol—Détermination de la Conductivité Électrique Spécifique (Standard No. AFNOR NF ISO 11265).

4. (2016). Sols: Reconnaissance et Essais. Détermination de la Teneur en Carbonate. Méthode du Calcimètre (Standard No. AFNOR NF P 94-048).

5. (2016). Sols Reconnaissance Et Essais—Mesure de la Capacité D’adsorption de Bleu de Méthylène d’un sol ou d’un Matériau Rocheux—Détermination de la Valeur de Bleu de Méthylène d’un sol ou d’un Matériau Rocheux par L’essai à la tâche (Standard No. AFNOR NF P 94-068).

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