Numerous studies have focused on modern hydroclimate and the modulated mechanisms in the Tianshan Mountains(TMs),arid central Asia.However,the detailed information of hydroclimatic processes beyond the instrumental pe...Numerous studies have focused on modern hydroclimate and the modulated mechanisms in the Tianshan Mountains(TMs),arid central Asia.However,the detailed information of hydroclimatic processes beyond the instrumental period is still scarce.This paper reconstructed a hydrology history from core sediments of the Dalongchi Lake in the Tianshan Mountains.The comparability between endmembers(EMs)of grain size and ICP-AES based geochemical elements in the lake sediments highlighted their availability for hydrological reconstructions.Hydrodynamic forces(EM1,EM4,Ti/Al and Li/Al),chemical weathering intensity[(Mg+Ca+K)/Al],salinity proxy(Mg/Ca)and redoxsensitive proxy(Fe/Mn)highly correlated with the first principal component(P<0.01),whereas paleoproductivity proxies(TN,TOC,Ba/Al,Zn/Al and Cu/Al)and C/N showed high loadings on the second principal component(P<0.05).The inferred hydrology progress was nonlinearly responded to temperature,precipitation and climate-dictated glaciers.Specifically,the water level didn’t always covary with the humidity because of glaciers.The maximum water level was the comprehensive result of glaciers melting and high humidity around 1830 CE.Thereafter,water level continually decreased with declining moisture at high temperature,implying a limited buffering capacity of glaciers in the Dalongchi Lake basin.EM3-indicated eolian activity intensity was caused by the behaviors of Siberian High because the latter intensified surface wind and the dust transportation.The hydrothermal patterns were characterized by warm/dry and cold/wet alternations in a long run although warm/wet pattern was identified from a short-term view.展开更多
采用盆栽试验,通过测定延胡索植株内铅含量、地上植株及地下块茎的生物量,研究了不同钾铅浓度组合对延胡索(Corydalis yanhusuo W. T. Wang)生长及其不同器官干物质积累过程的影响。结果表明:总体上低铅和高铅处理土壤延胡索地上部分和...采用盆栽试验,通过测定延胡索植株内铅含量、地上植株及地下块茎的生物量,研究了不同钾铅浓度组合对延胡索(Corydalis yanhusuo W. T. Wang)生长及其不同器官干物质积累过程的影响。结果表明:总体上低铅和高铅处理土壤延胡索地上部分和地下部分生物量与空白对照相比均有增加,其中低铅处理的地上部分增加了16.26%、地下部分增加了13.44%,高铅处理的地上部分增加了10.26%、地下部分增加了7.40%。钾肥的施加能够缓解铅的生物毒性,使延胡索生物量增加。延胡索地上和地下部分中钾处理的生物量对比未施加钾肥处理,在低铅和高铅处理中均有增加,分别增加了18.67%、35.97%、29.24%、46.78%。同时,延胡索不同部位铅的积累量地下部分与地上部分总体差异显著。即地下部分呈现随时间逐渐减小的趋势,而地上部分随时间先增加后降低的趋势。且中钾处理的地上和地下部分在低铅处理中分别比未施加钾肥处理的铅含量降低了44.08%、53.37%,在高铅处理中则分别降低了28.26%、14.07%。因此在延胡索规范化种植中应在保证其铅积累量不超标的情况下,尽量选择含低铅的土壤,试验条件下增施200 mg kg-1钾肥可缓解重金属对药用植物的毒害,提高产量。展开更多
基金financially supported by the National Natural Science Foundation of China(No.41902024U1203821L08)+3 种基金the Chongqing Science and Technology Commission(cstc2019jcyjmsxmX0656)the Talent Introduction Program of Chongqing Three Gorges University(17RC08)the Research Center for Sustainable Development of the Three Gorges Reservoir Area(18sxxyjd12)the Youth Innovation Promotion Association of Chinese Academy of Sciences(No.2022447)。
文摘Numerous studies have focused on modern hydroclimate and the modulated mechanisms in the Tianshan Mountains(TMs),arid central Asia.However,the detailed information of hydroclimatic processes beyond the instrumental period is still scarce.This paper reconstructed a hydrology history from core sediments of the Dalongchi Lake in the Tianshan Mountains.The comparability between endmembers(EMs)of grain size and ICP-AES based geochemical elements in the lake sediments highlighted their availability for hydrological reconstructions.Hydrodynamic forces(EM1,EM4,Ti/Al and Li/Al),chemical weathering intensity[(Mg+Ca+K)/Al],salinity proxy(Mg/Ca)and redoxsensitive proxy(Fe/Mn)highly correlated with the first principal component(P<0.01),whereas paleoproductivity proxies(TN,TOC,Ba/Al,Zn/Al and Cu/Al)and C/N showed high loadings on the second principal component(P<0.05).The inferred hydrology progress was nonlinearly responded to temperature,precipitation and climate-dictated glaciers.Specifically,the water level didn’t always covary with the humidity because of glaciers.The maximum water level was the comprehensive result of glaciers melting and high humidity around 1830 CE.Thereafter,water level continually decreased with declining moisture at high temperature,implying a limited buffering capacity of glaciers in the Dalongchi Lake basin.EM3-indicated eolian activity intensity was caused by the behaviors of Siberian High because the latter intensified surface wind and the dust transportation.The hydrothermal patterns were characterized by warm/dry and cold/wet alternations in a long run although warm/wet pattern was identified from a short-term view.
文摘采用盆栽试验,通过测定延胡索植株内铅含量、地上植株及地下块茎的生物量,研究了不同钾铅浓度组合对延胡索(Corydalis yanhusuo W. T. Wang)生长及其不同器官干物质积累过程的影响。结果表明:总体上低铅和高铅处理土壤延胡索地上部分和地下部分生物量与空白对照相比均有增加,其中低铅处理的地上部分增加了16.26%、地下部分增加了13.44%,高铅处理的地上部分增加了10.26%、地下部分增加了7.40%。钾肥的施加能够缓解铅的生物毒性,使延胡索生物量增加。延胡索地上和地下部分中钾处理的生物量对比未施加钾肥处理,在低铅和高铅处理中均有增加,分别增加了18.67%、35.97%、29.24%、46.78%。同时,延胡索不同部位铅的积累量地下部分与地上部分总体差异显著。即地下部分呈现随时间逐渐减小的趋势,而地上部分随时间先增加后降低的趋势。且中钾处理的地上和地下部分在低铅处理中分别比未施加钾肥处理的铅含量降低了44.08%、53.37%,在高铅处理中则分别降低了28.26%、14.07%。因此在延胡索规范化种植中应在保证其铅积累量不超标的情况下,尽量选择含低铅的土壤,试验条件下增施200 mg kg-1钾肥可缓解重金属对药用植物的毒害,提高产量。
