Effect of Native Vegetative Barriers to Prevent Wind Erosion: A Sustainable Alternative for Quinoa (Chenopodium quinoa Willd.) Production

Author:

Barrientos-Pérez Ermindo12,Carevic-Vergara Felipe S.23ORCID,Rodriguez Juan Pablo4ORCID,Arenas-Charlín Jorge2,Delatorre-Herrera José2

Affiliation:

1. Engineering Agriculture Department, Natural Sciences and Agriculture Faculty, Universidad Técnica de Oruro, Oruro 00591, Bolivia

2. Doctoral Program in Agriculture for Arid-Desert Environments, Faculty of Renewable Natural Resources, Desert Agriculture Area, Universidad Arturo Prat, Iquique 1100000, Chile

3. Plant Ecology Laboratory, Faculty of Renewable Natural Resources, Universidad Arturo Prat, Iquique 1100000, Chile

4. Julius Kühn Institute (JKI)—Institute for Plant Protection in Horticulture and Urban Green, Messeweg 11/12, 38104 Braunschweig, Germany

Abstract

The abandonment of ancestral techniques and the incorporation of new technologies in the production systems for the cultivation of quinoa has resulted in overexploitation of soils, a loss of fertility, water imbalance, a loss of native vegetation cover in plain land areas, and other negative effects on the southern Altiplano agricultural sustainable system. One of the methods to reduce wind erosion and improve soil environmental conditions is establishing a native vegetative barrier. The effect of t’ola [Parastrephia lepidophylla (Wedd.) Cabrera] as a vegetative barrier to prevent wind erosion was evaluated using the rod method, gravimetric humidity fluctuations, and soil quality measurements in traditional quinoa Real production plots. We found significant differences (p < 0.05) for mean erosion, sedimentation, net erosion, and mobilized soil variables. The highest loss of soil was reported for December and November. Vegetative barriers comprising three meters of t’ola better protected bare soils up to 7 m from the barrier, while in bare soils, the loss values were over 5 t ha−1 month−1. Soil humidity fluctuations in plots with t’ola vegetative barriers were highly significant for the distance factors and depth levels. There was a higher accumulation of gravimetric humidity (%) in bare soils from 1.5 m to the barrier (6.95%), while the insides of the vegetative barriers retained an average soil humidity of 6.37%. After two agricultural seasons in the quinoa plots, 62 t ha−1 per year of soils were lost due to a lack of vegetative barriers. Due to the large, cultivated area with quinoa (104,000 ha in 2014) in the Intersalar zone, wind erosion causes 6.48 million tons of soil loss yearly. T’ola vegetative barriers in the southern Altiplano of Bolivia favour the retention of sediments against wind erosion and soil protection for quinoa cultivation. Furthermore, incorporating native lupine increased soil fertility by 80% and protected the soil surface cover.

Publisher

MDPI AG

Subject

Plant Science,Agronomy and Crop Science,Food Science

Reference52 articles.

1. Navarro, G., and Maldonado, M. (2004). Geografía Ecológica de Bolivia. Vegetación y Ambientes Acuáticos, Centro de Ecología Simón I. Patiño-Departamento de Difusión.

2. Identification, distribution and characteristics of erosion sensitive areas in three different central Andean geo-ecosystems;Coppus;Catena,2003

3. Consequences of quinoa production (Chenopodium quinoa Willd.) increased in the southern altiplano of Bolivia;Medrano;J. Cienc. Tecnol. Agrar.,2009

4. The Situation for Quinoa and Its Production in Southern Bolivia: From Economic Success to Environmental Disaster;Jacobsen;J. Agron. Crop Sci.,2011

5. Gandarillas, A., Rojas, W., Bonifacio, A., and Ojeda, N. (2014). Estado del Arte de la Quinua en el Mundo en 2013, Organización de las Naciones Unidas para la Alimentación y la Agricultura. Available online: https://www.fao.org/3/a-i4042e.pdf.

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