Abstract
Salt accumulation in topsoil is a widespread restricting factor that limits agricultural production and threatens food security in arid and semi-arid regions. However, whether this upward enrichment was suppressed by macropores was less documented. Therefore, artificial macropores with sandy fillings (AMSF) method was proposed in this study. Soil column experiments showed a significant improvement of saturated hydraulic conductivity (Ks) by more than 260% under artificial macropore treatment. Freshwater irrigation was conducted to monitor the short-term water and salt movement. This research aimed at evaluating the potential benefit of AMSF method on soil desalinization in coastal farmland of northern China. The results demonstrated that downward movement of soil water was stimulated in AMSF method, accordingly, washing more salt ions out of top rooting zone. Particularly, 10 cm or more macropore depth treatments of AMSF method enhanced total desalinization by 52.1% to 176.6% in 0–30 cm soil layer, in comparison to the control group without macropore. Subsequent observations for alfalfa showed higher biomass by 20.8% under 15 cm macropore depth. The results here provided an exploration demonstration to pursue these studies with the ultimate goal of optimizing application strategies for amendment in coastal salt-affected lands of northern China.
Highlights
Soil salinization is a global widespread problem, which would limit agricultural production and threaten food security dramatically in arid and semi-arid regions [1,2]
The results indicated an improvement for artificial macropores with sandy fillings (AMSF) method on drainage capacity in soils
This could be explained by the replacement of cohesive particle, so that continuous macropores were generated between sand particles
Summary
Soil salinization is a global widespread problem, which would limit agricultural production and threaten food security dramatically in arid and semi-arid regions [1,2]. Salt accumulation has detrimental influence on soil physicochemical properties and crop growth as well. This upward movement of salt is caused by the combined influence of groundwater transport, soil evapotranspiration and other water input. The groundwater which contains soluble salt tends to transport via capillary rise to upper soil layer due to continuous evapotranspiration [4]. Liquid water moves up to compensate for the water loss, and thereby, salt accumulates and precipitates in topsoil. The vast majority of crops’ roots concentrate in the top 0 to 30 cm soil layer [5], so it is of great importance to ensure an acceptable salt conditions in the topsoil for realizing regional agro-ecological value
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