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Water and salt distribution characteristics of shallow soil at different diving water levels |
LI Xiaoqian1,2, XIA Jiangbao2, ZHAO Ximei1,2, YANG Jihua1 |
1. Shandong Provincial Key Laboratory of Soil Erosion and Ecological Restoration, College of Forestry, Shandong Agricultural University, 271018, Tai'an, Shandong, China; 2. Shandong Provincial Key Laboratory of Eco-environmental Science for Yellow River Delta, Binzhou University, 256603, Binzhou, Shandong, China |
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Abstract [Background] Water and salt distribution of shallow soil are the main affecting factors of seedling growth. Taking soil columns planted with Tamarix chinensis Lour.(3-year-old), a constructive species in the Yellow River Delta as the research object, we aimed at studying how the diving water level (DWL) affects the water and salt distribution. [Methods] The experiment was carried out as such, first, planting the T. chinensis Lour. to soil column in the greenhouse, configuring the salt water in which mineralization degree was 6 grams per liter with sea salt, then setting up 6 diving water levels of 0.3 m, 0.6 m, 0.9 m, 1.2 m, 1.5 m, and 1.8 m, and each level set 3 repeats. In the use of drying method and residue drying method, the relative water content (RWC), salt content and absolute concentration at soil depths of 0-10 cm and 10-20 cm in a simulated device with DWL of 0.3 m, 0.6 m, 0.9 m, 1.2 m, 1.5 m and 1.8 m were measured. [Results] The RWC in 10-20 cm was higher than that in 0-10 cm and decreased significantly with the DWL increased (0-20 cm), but the decreasing degree in 0-10 cm was much higher than that in 10-20 cm, the highest reduction of the RWC was at both 1.2 m and 1.5 m. The salt content (0-10 cm) increased at first and then decreased with the DWL increasing, reached peak at 1.2 m (1.38%) and increased by106.35% compared with that at 0.3 m. The salt content (10-20 cm) was complex with the DWL changing, it changed smoothly at 0.3-0.9 m and increased at 1.2 m then decreased at 1.5-1.8 m, reached maximum at 1.2 m (1.33%) and increased by 304.04% compared with 0.3 m. The absolute concentration (0-10 cm) exponentially increased with the DWL increasing and maximum at 1.2 m (17.12%).The absolute concentration (10-20 cm) increased at first and then decreased with the DWL increasing and was maximal at 1.2 m (10.10%). [Conclusions] The RWC was significantly negative with the DWL (P < 0.01) while significantly positive for the salt level (P < 0.05); the absolute concentration (0-10 cm) was significantly positive with the DWL (P < 0.01) but significantly negative with the DWL (P < 0.01), the absolute concentration (10-20 cm) was significantly positive with the salt level (P < 0.01). This study provides theoretical basis and technical reference for the prevention of soil salinization in the Yellow River Delta and the planting management of T. chinensis Lour.
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Received: 14 July 2016
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