首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Dynamic characteristics of soil properties in a Robinia pseudoacacia vegetation and coastal eco-restoration
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Dynamic characteristics of soil properties in a Robinia pseudoacacia vegetation and coastal eco-restoration

机译:刺槐植被土壤性质的动态特征与沿海生态恢复。

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Precipitation is one of the major determinants of soil moisture in plantations growing in the saline-alkali soil in the Yellow River Delta. The present study was conducted on a 28-yr old Robiniapseudoacacia plantation, a major vegetation type of the Yellow River Delta, and the results indicated strong seasonal patterns in soil moisture, salt, nutrient and enzyme activities at varying depths with respect to annual precipitation. Soil moisture during the growing season of March to October fluctuated drastically in response to precipitation events and was generally higher than that from November to February. Furthermore, soil water content in the 0-60 cm soil layer was positively correlated with precipitation during the same period but not for the value in the 60-80 cm soil layer. Salt content in different soil layers increased gradually from November to February, decreased from February to September and then increased in October. Precipitation was strongly and negatively correlated with soil salt content in different soil layers (except 20-40 cm). Soil enzymes became less active and soil nutrient contents decreased with soil depth, though different enzymes and nutrients showed seasonal variations. The activity of polyphenol oxidase increased in spring, reached the maximum values in June, and decreased in later months. The activity of alkaline phosphatase, proteinase and urease fluctuated throughout the growing season, with the maximum values in October. Available phosphorous increased in the early months and decreased after August, whereas available potassium, hydrolysable nitrogen and organic substances content in soil gradually increased throughout. Therefore, it is suggested that precipitation is the crucial limiting factor to tree growth through impacts on soil moisture, salt, nutrient and enzyme activities in saline-alkali soils in the Yellow River Delta. (C) 2016 Elsevier B.V. All rights reserved.
机译:降水是黄河三角洲盐碱土壤中人工林土壤水分的主要决定因素之一。本研究是在黄河三角洲的主要植被类型28年生的Robiniapseudoacacia人工林上进行的,结果表明,相对于年降水量,不同深度的土壤水分,盐分,养分和酶活性具有强烈的季节性特征。 3月至10月生长季节的土壤湿度因降水事件而剧烈波动,通常高于11月至2月。此外,在同一时期,0-60厘米土壤层中的土壤水分含量与降水呈正相关,但与60-80厘米土壤层中的值却没有正相关。从11月到2月,不同土壤层中的盐含量逐渐增加,从2月到9月减少,然后在10月增加。降水与不同土壤层(20-40 cm除外)中的土壤盐分含量呈显着负相关。土壤酶的活性降低,土壤养分含量随土壤深度而降低,尽管不同的酶和养分表现出季节性变化。春季多酚氧化酶的活性增加,6月达到最大值,随后数月下降。整个生长季节,碱性磷酸酶,蛋白酶和脲酶的活性波动,十月份达到最大值。有效磷在开始的几个月中增加,而在八月之后减少,而土壤中的有效钾,可水解氮和有机物质的含量在整个过程中逐渐增加。因此,建议通过影响黄河三角洲盐碱土壤中的水分,盐分,养分和酶活性,降雨是影响树木生长的关键限制因素。 (C)2016 Elsevier B.V.保留所有权利。

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