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Seasonal Performance and Spatial Heterogeneity of Soil Salt Ions in a Semiarid Orchard of Northwest China

文献类型： 外文期刊

作者： Guo, Quanen 1 ; Guo, Tianwen 1 ; Ma, Zhongming 1 ; Che, Zongxian 1 ; Nan, Lili 2 ; Wang, Yiquan 3 ; Palta, Jairo A. 4 ; X 1 ;

作者机构： 1.Gansu Acad Agr Sci, Soil Fertilizer & Water Saving Inst, Lanzhou 730070, Peoples R China

2.Gansu Agr Univ, Gansu Prov Key Lab Aridland Crop Sci, Lanzhou 730070, Peoples R China

3.Northwest Sci Tech Univ Agr & Forestry, Coll Resources & Environm, Yang Ling 712100, Peoples R China

4.CSIRO Plant Ind, Wembley, WA 6913, Australia

5.Lanzhou Univ, Sch Life Sci, Inst Arid Agroecol, State Key Lab Grassland Agroecosyst, Lanzhou 730000, Peoples R China

期刊名称：HORTSCIENCE （ 影响因子：1.455； 五年影响因子：1.617 ）

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收录情况： SCI

摘要： The relationship between spatial and temporal dynamics of major salt ions and their toxicology is still unclear, particularly in perennial orchard fields. A seasonal soil sampling was conducted from Apr. to Oct. 2011 in a salinized orchard soil in semiarid northwest China. Soil moisture content and concentrations of total soluble salt and eight salt ions were measured every 2 weeks in the soil at 0 to 2,2 to 5,5 to 10, 10 to 15, 15 to 20,20 to 25, 25 to 40,40 to 60, 60 to 80, and 80 to 120 cm during the growing period of apple trees. Soil moisture content decreased early in the growth season (Period 1) but with increasing rainfall in the middle of growing season (Period 2 and Period 3) and reached a maximum at late season (Period 4) at all depths. Soil salt concentration increased along with soil profile, particularly in the 60- to 120-cm soil layer at all periods. The highest soil salt level was observed in Period 4. The contents of HCO3-, Ca2+, and Mg2+ were almost uniform in all soil layers, but the contents of Cl-, SO42-, and Na+ increased with soil layer. The content of K+ decreased from the upper to the deeper layers of soil profile. The distribution of CO32- had a high temporal and spatial heterogeneity with soil depths and season. Analysis of the charge balance on positive and negative salt ions indicated that the horizontal movement of ions and the transfer of soil water were likely the driving factors affecting soil salinization. The movement of Na+ and Mg2+ ions in the top soil may be responsible for rhizospheric ions composition and toxin effect to restrain apple tree growth in the early growth period.

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