Abstract

Environmental stresses (soil compaction, drought, waterlogging) cause changes in plants’ root system structure, also affecting the growth of above-ground parts. The aim of this study was to estimate phenotypic variation among maize and triticale genotypes in root penetration ability through petrolatum-wax-layer (RPA). Also, the effect of shortage or excess of soil water on dry matter of shoots and roots and morphological changes in root system structure in sensitive and resistant maize and triticale genotypes grown in low or high soil compaction level was evaluated. To estimate RPA index, the petrolatum-wax-layer method (PWL) was used. The strength of three petrolatum-wax concentrations 60, 50 and 40 % was 0.52, 1.07 and 1.58 MPa, respectively. High coefficients of variation (CV) were observed in 0.52 and 1.07 MPa and for maize were 19.2 and 21.7 %, and for triticale, 12.5 and 18.3 %, respectively. The data indicate that the use of PWL technique is an effective screening method, and makes it possible to divide the genotypes into resistant and sensitive groups. The second part of this study investigated a multistress effect of soil compaction combined with drought or waterlogging on root and shoot growth and morphological changes in root system structure of maize and triticale genotypes differing in susceptibility to environmental stresses. Seedlings were grown for 4 weeks in root-boxes under conditions of low (LSC 1.1 g cm−3) or severe (SSC 1.6 g cm−3) soil compaction. Drought or waterlogging stresses were applied for 2 weeks from 14th to 28th day. In comparison to LSC treatment, in SSC treatment the decrease in dry matter of shoots and roots was greater for sensitive genotypes of maize and triticale (Ancora, CHD-147). Soil drought or waterlogging caused greater decrease of dry matter of shoots and roots in seedlings grown in SSC in comparison to LSC. The root penetration index (RPI) was estimated as a ratio of root dry matter in 15–40 cm root-box layer to total root dry matter. On the basis of RPI it was possible to group the genotypes according to their ability to distribute roots in soil profile. In comparison to LSC, SSC exerted a strong influence on the length of seminal and seminal adventitious roots, as well as the number and length of L- and S-type lateral roots developed on seminal and nodal roots. In both species the restriction effect of soil compaction on number and length of roots was more severe in sensitive (Ankora, CHD-147) than in resistant (Tina, CHD-247) genotypes. The restriction in roots propagation was greater in triticale than in maize. Exposure to drought or waterlogging in the case of genotypes grown in LSC and SSC treatments caused a decrease in number and length of particular components of root system structure. In both species the decrease of root number and length in plants grown under waterlogging was greater than under drought. The observed changes in root system were greater in sensitive (Ankora, CHD147) than in resistant (Tina, CHD-247) genotypes. Statistically significant correlations were found between RPA and RPI and also between these indexes and soil compaction, drought and waterlogging susceptibility indexes. This indicates that genotypes resistant to soil compaction were resistant to drought or waterlogging and also that genotypes resistant to drought were resistant to waterlogging.

Highlights

  • Abiotic stresses, e.g., soil compaction, drought and waterlogging are environmental factors that affect plants growth, development and yield

  • The second part of this study investigated a multistress effect of soil compaction combined with drought or Communicated by W

  • We deal in circumstances when the amount of rainfall do not compensate the water loss through a transpiration and evaporation, and with waterlogging, when the soil is inundated as a result of heavy rainfalls or river floods what causes drastic decrease in roots capability to water uptake as a result of decrease in oxygen content in water (Masle 2002; Fageria et al 2006)

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Summary

Introduction

E.g., soil compaction, drought and waterlogging are environmental factors that affect plants growth, development and yield. Different levels of soil compaction are caused mainly by natural processes and by the use of heavy machinery in soil cultivation. We deal in circumstances when the amount of rainfall do not compensate the water loss through a transpiration and evaporation, and with waterlogging, when the soil is inundated as a result of heavy rainfalls or river floods what causes drastic decrease in roots capability to water uptake as a result of decrease in oxygen content in water (Masle 2002; Fageria et al 2006). The degree of plant restriction by environmental stresses mainly depends on the species, variety and the age of the plants. The interand intraspecific variations between species and within genotypes in responses to those stresses are significant, problems related to a combined influence of different soil moisture with physical soil parameters have not been studied thoroughly (Kono et al 1987b; Masle 2002; Ashraf 2010)

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