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首页> 外文期刊>Italian Journal of Agronomy >Irrigation with saline-sodic water: effects on two clay soils
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Irrigation with saline-sodic water: effects on two clay soils

机译:盐水冲洗:对两种黏土的影响

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The results of a4-year experiment aimed at evaluating the effect of irrigation with saline-sodic water on the soil are reported. The research was carried out at the Campus of the Agricultural Faculty of Bari University (Italy) on 2 clay soils (Bologna- Ti and Locorotondo - T2). The soils were cropped to boriotto bean (Phaseolus vulgaris L), capsicum (Capsicum annuum L), sunflower (Helianthus annuus L), wheat (Ttiticum durum Desf) grown in succession; the crops were irrigated with 9 saline-sodic types of water and subjected to two different leaching fractions (10% and 20% of the watering volume). The 9 solutions were obtained dissolving in de-ionised water weighted amounts of sodium chloride (NaCl) and calcium chloride (CaCfe), deriving from the combination of 3 saline concentrations and 3 sodicity levels. The crops were irrigated whenever the water lost by evapotranspiration from the soil contained in the pots was equal to 30% of the soil maximum available water. The results showed that, though the soils were leached during the watering period, they showed a high salt accumulation. Consequently, the saturated soil extract electrical conductivity increased from initial values of 0.65 and 0.68 dS nr1 to 1124 and 13.61 dS nr1 at the end of the experiment, for the soils Ti and T2, respectively. The saline concentration increase in irrigation water caused in both soils a progressive increase in exchangeable sodium, and a decrease in exchangeable calcium and non-significant variations in exchangeablepotassium (K) and magnesium (Mg).
机译:报道了一项为期四年的实验结果,该实验旨在评估盐水对土壤的灌溉效果。该研究是在意大利巴里大学农业学院的校园内的2种粘土上进行的(Bologna-Ti和Locorotondo-T2)。土壤依次种植了bo豆(菜豆),辣椒(辣椒),向日葵(向日葵),小麦(Ttiticum durum Desf)。将农作物用9种盐碱水灌溉,并进行两种不同的浸提(浇水量的10%和20%)。从3种盐水浓度和3种碱度的组合中获得9种溶液,将它们溶解在去离子水中,称量后称量的氯化钠(NaCl)和氯化钙(CaCfe)。每当蒸腾作用从盆中所含土壤中流失的水分等于土壤最大可用水分的30%时,便对作物进行灌溉。结果表明,尽管在浇水期间土壤被淋洗,但它们却显示出较高的盐分积累。因此,对于土壤Ti和T2,在实验结束时,饱和土壤提取物的电导率分别从初始值0.65和0.68 dS nr1增加到1124和13.61 dS nr1。两种土壤中灌溉用水中的盐浓度增加导致可交换钠的逐步增加,可交换钙的减少以及可交换钾(K)和镁(Mg)的无明显变化。

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