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Production of melon (Cucumis melo) may be limited by excesses of boron and salinity, and it was hypothesized that melon grafted onto Cucurbita rootstock would be more tolerant to excessive boron concentrations than non-grafted plants. The objectives of this study were: (i) to determine the effects of salinity and excessive boron concentrations in irrigation water on growth and yields of grafted and non-grafted melon plants; and (ii) to study the interaction between the effects of salinity and boron on the uptake of macroelements and boron by grafted and non-grafted melon plants. The plants were grown in pots of Perlite in a greenhouse. The combined effects of boron and salinity on growth and yield were investigated for five boron concentrations, ranging from 0.2 to 10 mg L −1 , and two salinity levels, electrical conductivity (EC) 1.8 and 4.6 dS m −1 , in the irrigation water. With low salinity the boron concentrations in old leaves of non-grafted and grafted plants ranged from 249 to 2827 and from 171 to 1651 mg kg −1 dry weight, respectively; with high salinity the corresponding concentrations ranged from 192 to 2221 and from 200 to 1263 mg kg −1 dry weight, respectively. These results indicate that the grafted plants accumulated less boron than the non-grafted plants when they were exposed to similar boron concentrations, and that both plant types absorbed less boron when irrigated with the more saline irrigation water. It is suggested that: (i) the Cucurbita rootstock excluded some boron and that this, in turn, decreased the boron concentration in the grafted plants; and (ii) the low boron uptake under high-salinity irrigation was mainly a result of reduced transpiration of the plants. Significant negative linear regressions were found between fruit yield and leaf boron concentration for grafted plants, under both low and high salinity levels, and for non-grafted plants under low salinity. The fruit yield of the grafted plants was less affected by boron accumulation in the leaves than that of non-grafted plants. Increasing the water salinity decreased the sensitivity of both plant types to increases in leaf boron concentration, which indicates that the effects of boron and salinity on melon plants were not additive.

Previous studies about the effect of antecedent moisture content (AMC) on seal formation have shown contradictory results. We hypothesize that this controversy is related to differences in slaking during wetting. The objectives were to analyze the effects of: (i) clay content on aggregate stability and slaking; (ii) clay content and slaking on seal formation and interrill erosion under various wetting rates (WR) and AMC under simulated rain. Aggregate stability was determined on six smectitic soils from Israel with clay content from 80 to 630 g kg−1 In the rain simulator, soils with 230, 410 and 620 g kg−1 clay were prewetted with WR = 1 and 5 mm h−1 to AMC = 0.25 and 0.5 of field capacity (FC), prior to the application of 80 mm of rain. Aggregate stability and slaking by fast WR increased with increase in clay content. In soils with 230 and 410 g kg−1 clay, raindrop impact was enough to disintegrate the aggregates and sealing was not affected by WR and AMC. Conversely, in the soil with 620 g kg−1 clay, seal formation increased with slaking caused by fast wetting. Thus, final infiltration rate of the clay soil with AMC = 0.5 FC and WR = 1 mm h−1 was 11.1 mm h−1 compared with 6.0 mm h−1 in the air‐dry soil (fast wetting by rain). The effects of WR and AMC on soil loss were similar to their effect on runoff but more pronounced. The relation between wetting process and clay content should be considered when predicting soil erosion in smectitic soils.

The effects of grafting on Na and Cl– uptake and distribution in plant tissues were quantified in a greenhouse experiment using six combinations of melon (Cucumis melo L. cv. Arava) and pumpkin (Cucurbita maxima Duchesne×Cucurbita moschata Duchesne cv. TZ-148): non-grafted, self-grafted, melons grafted on pumpkins, and pumpkins grafted on melons. Total Na concentration in shoots of plants with pumpkin or melon rootstocks was <60 mmol kg−1 and >400 mmol kg−1, respectively, regardless of the scion. In contrast, shoot Cl– concentrations were quite similar among the different scion–rootstock combinations. Na concentrations in exudates from cut stems of plants with a pumpkin rootstock were very low (<0.18 mM), whereas those in the exudates of plants with melon rootstocks ranged from 4.7 mM to 6.2 mM, and were quite similar to the Na concentration in the irrigation water. Root Na concentrations averaged 11.7 times those in the shoots of plants with pumpkin rootstocks, while in plants with melon rootstocks, values were similar. Two mechanisms could explain the decrease in shoot Na concentrations in plants with pumpkin rootstocks: (i) Na exclusion by the pumpkin roots; and (ii) Na retention and accumulation within the pumpkin rootstock. Quantitative analysis indicated that the pumpkin roots excluded ∼74% of available Na, while there was nearly no Na exclusion by melon roots. Na retention by the pumpkin rootstocks decreased its amount in the shoot by an average 46.9% compared with uniform Na distribution throughout the plant. In contrast, no retention of Na could be found in plants grafted on melons.

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