Sariyildiz Temel
Kars Kafkas Universitesi, Artvin Orman Fakültesi, 08000 Artvin, Turkey.
J Environ Biol. 2004 Jul;25(3):343-50.
The effects of sea-salt on drainage water and soil chemistry was studied using two different soil types and setting up five soil-leaching experiments under controlled laboratory conditions. The objectives of the soil-leaching experiments were to provide information of the variability of soils and their drainage water chemistry following the input of different sea-salt solutions with different times which was similar to the precipitation input experienced during the storms in fields. Analyses were presented of major ions (Na+, Ca2+, Mg2+, Cl-, NO3-, SO4(2-) and NH4+) and pH for drainage water. At the end of the experiment, CEC (cation exchange capacity), %BS (percent base saturation), exchangeable capacity of Na, Ca and Mg and pH were also analysed for soil horizon chemistry. The results showed an increase in concentration of most of the major ions in the drainage water, though some adsorption of Na, Ca and Mg had taken place; so the result being a significant decrease in soil water pH. The chemical characteristics of each soil horizons also showed significant changes with the sea-salt applications compared to initial chemical characteristics. However, comparison of data from the four different sea-salt applications under different soil type or land-use didn't indicate the additional role that different land management could play in drainage water or soil chemistry.
在实验室控制条件下,使用两种不同土壤类型并设置五个土壤淋溶实验,研究了海盐对排水和土壤化学的影响。土壤淋溶实验的目的是提供不同海盐溶液在不同时间输入后土壤及其排水水化学变异性的信息,这类似于田间暴雨期间的降水输入。对排水中的主要离子(Na +、Ca2 +、Mg2 +、Cl -、NO3 -、SO4(2 -)和NH4 +)和pH进行了分析。实验结束时,还对土壤层化学的阳离子交换容量(CEC)、碱饱和度百分比(%BS)、Na、Ca和Mg的交换容量以及pH进行了分析。结果表明,排水中大多数主要离子的浓度有所增加,尽管发生了一些Na、Ca和Mg的吸附;结果是土壤水pH显著降低。与初始化学特性相比,每种土壤层的化学特性在施用海盐后也有显著变化。然而,在不同土壤类型或土地利用下对四种不同海盐施用数据的比较并未表明不同土地管理在排水或土壤化学中可能发挥的额外作用。