崔鹏, 秦宇, 刘霄, 秦永建, 曹帮华. 滨海盐碱地刺槐林降水与土壤水盐运动规律相关性研究[J]. 西南林业大学学报, 2013, 33(4): 1-4. DOI: 10.3969/j.issn.2095-1914.2013.04.001
引用本文: 崔鹏, 秦宇, 刘霄, 秦永建, 曹帮华. 滨海盐碱地刺槐林降水与土壤水盐运动规律相关性研究[J]. 西南林业大学学报, 2013, 33(4): 1-4. DOI: 10.3969/j.issn.2095-1914.2013.04.001
CUI Peng1, QIN Yu2, LIU Xiao3, QIN Yongjian4, CAO Banghua2. Studies on Correlations Among the Precipitation and Variation of Soil Water and Salt Under Robinia pseudoacacia Plantation in Coastal Saline-Alkali Area[J]. Journal of Southwest Forestry University, 2013, 33(4): 1-4. DOI: 10.3969/j.issn.2095-1914.2013.04.001
Citation: CUI Peng1, QIN Yu2, LIU Xiao3, QIN Yongjian4, CAO Banghua2. Studies on Correlations Among the Precipitation and Variation of Soil Water and Salt Under Robinia pseudoacacia Plantation in Coastal Saline-Alkali Area[J]. Journal of Southwest Forestry University, 2013, 33(4): 1-4. DOI: 10.3969/j.issn.2095-1914.2013.04.001

滨海盐碱地刺槐林降水与土壤水盐运动规律相关性研究

Studies on Correlations Among the Precipitation and Variation of Soil Water and Salt Under Robinia pseudoacacia Plantation in Coastal Saline-Alkali Area

  • 摘要: 以滨海盐碱地33年生刺槐纯林为对象,研究不同土层土壤水盐年份变化,分析年际降水与土壤水盐运动规律的相关性。结果表明:表层土壤同期含盐量低,土壤含盐量随土层深度的增加逐渐升高;雨季表层土壤同期含水量高,土壤含水量随土层深度增加逐渐降低,随蒸发量的增大,表层土壤含水量逐渐低于深层土;年份降水主要集中在夏季,占全年降水量的66%;土壤含水量与降水量呈显著正相关,土壤含盐量与降水量呈显著负相关,不同土层之间含水量与含盐量呈负相关;不同土层之间含水量相关性显著,在3月份0~20cm表层土与60~80cm土层土壤含水量差异显著(P=00341<005);不同土层之间含盐量相关性显著,差异不显著(P=01252>005)。

     

    Abstract: The annual variations of soil water and salt content at different soil layers in a 33a old Robinia pseudoacacia pure plantation in the coastal salinealkali area were measured, and meanwhile the correlation between the annual precipitation and the annual variations of soil water and salt content was analyzed. The results showed that the synchronized salt content in the surface soil was the lowest, the salt content increased with the increment of soil depth. The synchronized water content at the top soil layer in the rainy season was the highest, it was reduced with the increment of soil depth. The water content at the top soil layer was reduced along with the increase of evaporation and finally lower than that of the deeper layer soil. The annual precipitation in the studied area was concentrated in the summer, which accounted for 66% of the total. The soil water content was significantly positively correlated to rainfall. The salt content in the soil was significantly negatively correlated to the rainfall. Whereas there was a negative correlation between water content and salt content at different layers of the soil. There were significant correlations among the water and salt contents at different soil layers. There was significant difference in water content between the 0-20cm and 60-80cm soil layers in March (P=00341<005), but there was no significant difference in salt content between different soil layers (P=01252>005).

     

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