Examining the land leveling impacts on the physical quality of lowland soils in Southern Brazil
Introduction
Land leveling has been used worldwide as an agricultural practice on lowland soils mainly cultivated with rice fields under anaerobic conditions (Parfitt et al., 2014, Brye et al., 2006, Linh et al., 2017, Marzolff and Pani, 2018). In recent times, the use of sprinkler irrigation in aerobic systems that cultivate rice, soybean, sorghum, and maize in lowland soils has been increased in the south of Rio Grande do Sul state/Brazil and in other countries such as Pakistan (Kahlown et al., 2007), Italy (Spanu et al., 2009), USA (Vories et al., 2017), and India (Mandal et al., 2019). Under aerobic conditions, water can be saved when soil management (e.g., land leveling), conservation practices (e.g., no-tillage), and crop rotation are adopted. Despite these findings, there is a lack of knowledge about the effects of land leveling on SPQ and production systems cultivated in lowland soils under aerobic conditions, as these topics have not been thoroughly explored.
Due to the intense traffic of machines during the cutting, filling, smoothing, and shaping operations on the soil surface, land leveling strongly affects the physical-hydraulic and chemical properties of the topsoil surface layer (Aschonitis et al., 2012, Öztekin, 2013). Leveling operations may cause an increase in bulk density and a decrease in organic carbon content in lowland soils (Brye et al., 2004, Martínez-Casasnovas and Ramos, 2009, Öztekin, 2013; Timm et al., 2020). Furthermore, the effective arable layer for crop development can be decreased exposing subsoil layers mainly in cutting operations in shallow lowland soils.
The soil water retention curve (SWRC) is a key soil hydraulic function that can also be used as a soil quality indicator (Rickson et al., 2012). In addition, several soil quality indices (SQIs) are derived from SWRC and allow the assessment of soil physical quality (SPQ). The pore size distribution (PSD) function (Reynolds et al., 2009), hydraulic-energy indices, and functions of aeration and water retention (Armindo and Wendroth, 2019) are examples of derived SQIs to be applied in the SPQ analysis under agricultural practices, such as land leveling. In this regard, this study aimed to examine the effect of land leveling operations on the water retention and aeration behavior of a lowland soil in Southern Brazil. We hypothesize that the water retention and aeration behavior of lowland soils in aerobic environments are affected by land leveling operations which impact their hydraulic-energy-indices.
Section snippets
Experimental area
The study was carried out on an experimental field of 1.0-ha area located in the lowland experimental station of “Embrapa Clima Temperado”, near to the municipality of Capão do Leão, state of Rio Grande do Sul, Brazil (31°49'12,75" S, 52°27'59" W). This area was used to analyze the changes in the SPQ before and after land leveling (Fig. 1).
The regional climate characteristic is the Cfa type, according to the Köppen’s classification, representative of subtropical environment, with sea
Soil properties and hydraulic-energy SPQ indices
The fitted parameters of Eq. 1, which describe the 100 SWRCs measured before and 100 SWRCs measured after soil land leveling, are presented in Table 1.
The mean values of parameter θs after the land leveling procedure suggest an occurrence of soil compaction since its value was significantly smaller (P-value= 0.000086) than before soil land leveling (paired t-test). A relation between θr and the physical indices was not found because θr is more related to the dry range of the SWRC and has more
Conclusions
In this study, the effect of land leveling operations on the soil physical quality (SPQ) of a lowland soil under flood-irrigated rice and conventional rotation was analyzed. Land leveling negatively impacted the majority of the evaluated soil physical properties and hydraulic-energy indices derived from the integral of the SWRCs. A significant linear correlation between the soil hydraulic-energy indices and other physical properties (bulk density, macroporosity, microporosity, and total
Declaration of Competing Interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgments
The authors wish to thank the Brazilian National Council for Scientific and Technological Development (CNPq) for the financial support and scholarships provided, and the Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES), Finance Code 001, for scholarships.
Conflict of Interest
I would like to declare on behalf of all authors that the work described is original research that has not been published previously.
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