Field-saturated hydraulic conductivity (Ks) reflects porous system ability to transfer water in the soilplant system. The study aimed to measure Ks through two distinct techniques. One of them was carried out in the laboratory by applying the constant-head cylinder method (CHC) in undisturbed samples, herein referred to as a standard technique. The other consisted of a simplified falling-head technique to measure Ks in situ (SFH), as proposed by Bagarello et al. (2004). We also verified the correlations of the obtained Ks values with other soil physical properties. SFH method is simpler, faster and does not require sophisticated equipment, which can be executed directly in the field. The experiment was conducted in the city of Floresta (PR), Brazil, at Cocamar Technology Diffusion Unit. It consisted of four treatments: maize-crop interrow without recent machine traffic (MI), maize-crop interrow traveled by a harvester (MIT), maize-crop row (MR) and its relative position to brachiaria crop row sown in consortium, and in maize-crop interrow (BR). In each treatment, 10 sampling points were defined (repetitions), where Ks was determined by SFH and an undisturbed sample was taken to measure Ks in the laboratory. Ks values measured by methodological approaches were compared through the following statistical indices, with their respective results: Willmott's concordance index (0.944), maximum error (1.269) and mean absolute error (0.291), square root of normalized mean error (0.45), determination coefficient (0.88), residual mass coefficient (0.07), efficiency coefficient (0.72), performance index (0.80), and Pearson's correlation (0.85). A high agreement was found between the studied techniques, with measured values close to each other. Notably, we must give emphasis on SFH since it had a variation coefficient 1.4 times lower than the standard technique.
In Brazil, no-tillage is the most widely used soil conservation system (on more than 32 million hectares). However, intensification of the mechanisation of agricultural operations with larger and heavier machines increases the pressure on the soil, which, together with the reduced diversity of crops, results in compaction and physical degradation of soils under no-tillage systems. In this context, strategies to reduce soil compaction have been employed and the use of Braquiaria grass (Urochloa ruziziensis) (hereafter urochloa) as a cover plant is one promising strategy. The objectives of this study were to quantify, using physical indicators of capacity and intensity processes, the effects of cultivating urochloa sown in the interrow between corn (Zea mays L.) on storage and transmission of air and water in the surface layer of the soil and to evaluate the sensitivity of these indicators at detecting such effects. The results indicated that urochloa cultivation in the interrow produced an increase in storage capacity of air and water, and transmission of air and water, compared with the treatment in which the interrow was without urochloa. Cultivation of urochloa also alleviated compaction through an 18% reduction in soil bulk density and an increase of up to 490% in pore system continuity, in addition to improving the relationship between water and air storage, creating an environment that facilitates access to water and air. These results suggest that the use of urochloa as an interrow cover plant in corn improves the physical functions of the topsoil, producing a physical environment more favourable to development of crops. The use of intensity process indicators of physical properties was ~10 times more sensitive at detecting the effects of urochloa than the properties indicating capacity processes.
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