Long-term non-sustainable soil erosion rates and soil compaction in drip-irrigated citrus plantation in Eastern Iberian Peninsula
Creators
- 1. Soil Erosion and Degradation Research Group, Department of Geography, Valencia University, Blasco Ibàñez, 28, 46010 Valencia (Spain)
- 2. Department of Agricultural, Food and Forest Sciences, University of Palermo, Viale delle Scienze, 90128 Palermo (Italy)
- 3. Department of Reclamation of Arid and Mountainous Regions, University of Tehran, Karaj 31585-3314 (Iran, Islamic Republic of)
Description
Highlights: • Soil bulk density increased from 1.05 to 1.33 g cm−3 in 13 years. • Machinery passes increase soil compaction in the inter-row center till 1.43 g cm−3. • High soil losses were located in the center of the inter-row till 277 Mg ha−1 y−1. • New drip-irrigated plantations on slopes accelerate soil erosion. • Long-term soil erosion measurements assess agriculture sustainability. Agriculture is known to commonly cause soil degradation. In the Mediterranean, soil erosion is widespread due to the millennia-old farming, and new drip-irrigated plantations on slopes, such as the citrus ones, accelerate the process of soil degradation. Until now, the published data about soil erosion in citrus orchards is based on short-term measurements. Long-term soil erosion measurements are needed to assess the sustainability of drip-irrigated citrus production and to design new strategies to control high soil erosion rates. The objective of this study is to assess long-term soil erosion rates in citrus plantations and report the changes in soil bulk density as indicators of land degradation. We applied ISUM (Improved Stock-Unearthing Method) to 67 paired trees in an inter-row of 134 m (802 m2 plot) with 4080 measurements to determine the changes in soil topography from the plantation (2007) till 2020. Soil core samples (469) were collected (0–6 cm depth) to determine the soil bulk density at the time of plantation (2007) and in 2020. The results demonstrate an increase in soil bulk density from 1.05 g cm−3 to 1.33 g cm−3. Changes in soil bulk density were higher in the center of the row as a result of compaction due to passing machinery. Soil erosion was calculated to be 180 Mg ha−1 y−1 due to a mean soil lowering of 1.5 cm yearly. The highest soil losses were found in the center of the inter-row and the lowest underneath the trees. The extreme soil erosion rates measured in new drip-irrigated citrus plantations are due to soil lowering in the center of the inter-row and in the lower inter-row position where the incision reached 80 cm in 13 years. The whole field showed a lowering of the soil topography due to extreme soil erosion and no net sedimentation within the plantation. The results show the urgent need for soil erosion control strategies to avoid soil degradation, loss of crop production, and damages to off-site infrastructures.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2021.147549Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2021.147549;
- PII
- S0048969721026206;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 787
- Journal Page Range
- vp.
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 54061370
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- AGRICULTURE; BULK DENSITY; CROPS; EROSION; EROSION CONTROL; IRRIGATION; MACHINERY; SEDIMENTATION; SOILS; SUSTAINABILITY; TOPOGRAPHY
- Descriptors DEC
- CONTROL; DENSITY; EQUIPMENT; PHYSICAL PROPERTIES
Optional Information
- Copyright
- Copyright (c) 2021 The Authors. Published by Elsevier B.V.