The effect of rare earths (RE) on fractionation and transformation of available nitrogen in a yellow cinnamon soil was studied with soil cultivation. The results show that under the dry condition, when the extraneous...The effect of rare earths (RE) on fractionation and transformation of available nitrogen in a yellow cinnamon soil was studied with soil cultivation. The results show that under the dry condition, when the extraneous RE are added to the soil, both concentrations of soil ammonium N and hydrolysable N increase, and the concentrations of soil nitric N decrease. The concentrations of soil available N increase with the increase of RE concentrations in soils when the RE concentrations are low, but it decreases with the increase of high RE concentrations in soils. The NOEC (no observed effect concentration) of the extraneous RE to available N in the soils is 443.8 mg·kg -1 . Under the inundated condition, low RE concentrations in soil has no significant effect on soil ammonium N and hydrolysable N. However, when the soil RE concentrations are high, both of them decrease with the increase of RE concentrations. The NOEC of the extraneous RE to soil ammonium N and hydrolysable N are 171.2 and 256.9 mg·kg -1 , respectively.展开更多
北黄海泥质区具有地理位置独特、陆源物质供应丰富、沉积环境复杂等特点,为了更好地理解全球变化背景下对北黄海“源-汇”过程的影响,对北黄海泥质区边缘BS24岩芯沉积物进行了AMS14C测年、粒度、黏土粒级稀土元素和重矿物组成特征分析,...北黄海泥质区具有地理位置独特、陆源物质供应丰富、沉积环境复杂等特点,为了更好地理解全球变化背景下对北黄海“源-汇”过程的影响,对北黄海泥质区边缘BS24岩芯沉积物进行了AMS14C测年、粒度、黏土粒级稀土元素和重矿物组成特征分析,以判识沉积物的来源、沉积环境特征,并进一步探讨北黄海的沉积演化过程。研究表明,BS24岩芯轻重稀土元素具有明显分异,稀土元素的球粒陨石标准化配分曲线右倾,轻稀土元素富集,重稀土元素亏损,上陆壳标准化的δEu和δCe无明显异常。稀土元素的变化趋势较为一致,以170 cm为界,上段波动幅度较大,下段含量相对稳定。岩芯中共鉴定出30种重矿物,以黑云母(37.46%)和自生黄铁矿(22.39%)最为常见,辉石和氧化铁矿物及不稳定矿物含量低。黏土粒级及极细砂组分特征指示,BS24岩芯晚全新世以来主要接受黄河物质的沉积。BS24岩芯自生黄铁矿含量的变化可能指示了北黄海冷水团强度的变化。650 cal. a BP以来,北黄海冷水团强度增强,自生黄铁矿含量降低;650~1 560 cal. a BP期间,研究区处于还原环境,北黄海冷水团强度减弱,营造的缺乏对流性环境为自生黄铁矿的富集提供了有利条件。展开更多
文摘The effect of rare earths (RE) on fractionation and transformation of available nitrogen in a yellow cinnamon soil was studied with soil cultivation. The results show that under the dry condition, when the extraneous RE are added to the soil, both concentrations of soil ammonium N and hydrolysable N increase, and the concentrations of soil nitric N decrease. The concentrations of soil available N increase with the increase of RE concentrations in soils when the RE concentrations are low, but it decreases with the increase of high RE concentrations in soils. The NOEC (no observed effect concentration) of the extraneous RE to available N in the soils is 443.8 mg·kg -1 . Under the inundated condition, low RE concentrations in soil has no significant effect on soil ammonium N and hydrolysable N. However, when the soil RE concentrations are high, both of them decrease with the increase of RE concentrations. The NOEC of the extraneous RE to soil ammonium N and hydrolysable N are 171.2 and 256.9 mg·kg -1 , respectively.
文摘北黄海泥质区具有地理位置独特、陆源物质供应丰富、沉积环境复杂等特点,为了更好地理解全球变化背景下对北黄海“源-汇”过程的影响,对北黄海泥质区边缘BS24岩芯沉积物进行了AMS14C测年、粒度、黏土粒级稀土元素和重矿物组成特征分析,以判识沉积物的来源、沉积环境特征,并进一步探讨北黄海的沉积演化过程。研究表明,BS24岩芯轻重稀土元素具有明显分异,稀土元素的球粒陨石标准化配分曲线右倾,轻稀土元素富集,重稀土元素亏损,上陆壳标准化的δEu和δCe无明显异常。稀土元素的变化趋势较为一致,以170 cm为界,上段波动幅度较大,下段含量相对稳定。岩芯中共鉴定出30种重矿物,以黑云母(37.46%)和自生黄铁矿(22.39%)最为常见,辉石和氧化铁矿物及不稳定矿物含量低。黏土粒级及极细砂组分特征指示,BS24岩芯晚全新世以来主要接受黄河物质的沉积。BS24岩芯自生黄铁矿含量的变化可能指示了北黄海冷水团强度的变化。650 cal. a BP以来,北黄海冷水团强度增强,自生黄铁矿含量降低;650~1 560 cal. a BP期间,研究区处于还原环境,北黄海冷水团强度减弱,营造的缺乏对流性环境为自生黄铁矿的富集提供了有利条件。
