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Persistence of fertilization effects on soil organic carbon in degraded alpine wetlands in the Yellow River source region

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Journal of Mountain Science 2024年第4期21卷 1358-1371页

作者： DUAN Peng WEI Rongyi WANG Fangping LI Yongxiao SONG Ci HU Bixia YANG Ping ZHOU Huakun YAO Buqing zhao zhizhong Qinghai University Xining 810016China Qinghai Transportation Planning and Design Institute Co.Ltd Xining 810000China Key Laboratory of Adaptation and Evolution of Plateau Biota Chinese Academy of SciencesXining 810008China Key Laboratory of Restoration Ecology of Cold Area in Qinghai Province Northwest Institute of Plateau BiologyChinese Academy of SciencesXining 810008China Qinghai University of Science and Technology Xining 810016China

In the restoration of degraded wetlands,fertilization can improve the vegetation-soil-microorganisms complex,thereby affecting the organic carbon content.However,it is currently unclear whether these effects are sustainable.This study employed Biolog-Eco surveys to investigate the changes in vegetation characteristics,soil physicochemical properties,and soil microbial functional diversity in degraded alpine wetlands of the source region of the Yellow River at 3 and 15 months after the application of nitrogen,phosphorus,and organic mixed fertilizer.The following results were obtained:The addition of nitrogen fertilizer and organic compost significantly affects the soil organic carbon content in degraded wetlands.Three months after fertilization,nitrogen addition increases soil organic carbon in both lightly and severely degraded wetlands,whereas after 15 months,organic compost enhanced the soil organic carbon level in severely degraded wetlands.Structural equation modeling indicates that fertilization decreases the soil pH and directly or indirectly influences the soil organic carbon levels through variations in the soil water content and the aboveground biomass of vegetation.Three months after fertilization,nitrogen fertilizer showed a direct positive effect on soil organic carbon.However,organic mixed fertilizer indirectly reduced soil organic carbon by increasing biomass and decreasing soil moisture.After 15 months,none of the fertilizers significantly affected the soil organic carbon level.In summary,it can be inferred that the addition of nitrogen fertilizer lacks sustainability in positively influencing the organic carbon content.

关键词： Degraded alpine wetlands Fertilizer Soil organic carbon Temporal variation Vegetation aboveground biomass Yellow River source region

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Spatio-temporal Dynamic of Quality of Life of Residents, Northeast China

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Chinese Geographical Science 2016年第5期26卷 623-637页

作者： CHENG Yeqing WANG Ying WANG Zheye DU Na SUN Yu zhao zhizhong College of Geography and Environmental Sciences Hainan Normal University Department of Geography Kent State University Northeast Institute of Geography and Agroecology Chinese Academy of Sciences

Quality of life(QOL) is a hotspot issue that has attracted increasing attention from the Chinese Government and scholars, it is also a vital issue that should be addressed during the cause of ′establishing overall well-off society′. Northeast China is one of the most import old industrial bases in China, however, the industrial structure of heavy chemical industry and the development mode of ′production first, living last′ have leaded to series of social problems, which have also become a serious bottleneck to social stability and economic sustainable development. Through applying the methods of BP neural network, exploratory spatial data analysis(ESDA) and spatial regression model, this paper examines the space-time dynamics of QOL of the residents in Northeast China. We first investigate the indexes of QOL of the residents and then use ESDA methods to visualize its space-time relationship. We have found a spatial agglomeration of QOL of the residents in middle-southern Liaoning Province, central Jilin Province and Harbin-Qiqihar-Daqing area of Heilongjiang Province. Two third of the counties are low-low spatial correlation, and the correlative type of about 60% of the prefecture level areas keeps stable, indicating QOL of the residents in Northeast China shows a certain character of path dependence or spatial locked. We have also found that economic strength and development levels of service industry have positive and obvious effect on QOL of the residents, while the effect of such indexes as the social service level and the proportion of the tertiary industries are less.

关键词：生活质量中国政府东北地区时空动态居民 BP神经网络方法经济可持续发展空间数据分析

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Variations of geochemical compositions and the paleoclimatic significance of a loess-soil sequence from Garzê County of western Sichuan Province,China

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Chinese Science Bulletin 2009年第24期54卷 4697-4703页

作者： QIAO YanSong zhao zhizhong WANG Yan FU JianLi WANG ShuBing JIANG FuChu Institute of Geomechanics Chinese Academy of Geological Sciences Beijing 100081 China Key Laboratory of Neotectonic Movement & Geohazard Beijing 100081 China

The West Sichuan Plateau is located in the southeast margin of the Tibetan Plateau, where the climate is mainly influenced by the Indian southwest summer monsoon and the Tibetan Plateau monsoon. In this study, detailed geochemical analysis has been carried out on Ganzisi loess-paleosol sequence in Ganzê County of western Sichuan Province. The results indicate that Ganzê loess and paleosol have experienced the incipient stage of chemical weathering in dust source regions, characterized by the decomposition of plagioclase which caused the depletion of mobile elements Na and Ca. The post-depositional chemical weathering is characterized by carbonate dissolution and oxidation of Fe2+. The variations of some geochemical indexes (such as CIA values, Na/K and Fe2+/ Fe3+ ratios) in Ganzisi loess-paleosol sequence indicate a gradually decreased chemical weathering intensity in the dust source regions and deposition areas since 1.15 Ma BP consistent with the general increase of global ice volume, reflecting that the arid trend since 1.15 Ma BP in the southeast Tibetan Plateau is a regional response to the global climate change. The geochemical indexes in this section also reveal an obvious drying step occurred at about 250 ka BP in this region. We interpret this drying step as a result of decreased influence of the Indian southwest summer monsoon. This decrease in monsoon moisture is probably attributable to the uplift of the southeast margin of the Tibetan Plateau at about 250 ka BP.

关键词：古土壤序列地球化学分析甘孜黄土化学成分四川省古气候青藏高原东南部西部

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Magnetostratigraphic and paleoclimatic studies on the Red Earth Formation from the Chengdu Plain in Sichuan Province,China

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Science China Earth Sciences 2007年第6期50卷 927-935页

作者： zhao zhizhong QIAO YanSong WANG Yan FU JianLi WANG ShuBing LI ChaoZhu YAO HaiTao JIANG FuChu Institute of Geomechanics Chinese Academy of Geological Sciences Beijing 100081 China

Two red earth sections from the Chengdu Plain in Sichuan Province are dated using geomagnetic methods. The Brunhes/Matuyama (B/M) reversal boundary is recognized within the upper parts of the two sections,and the Jaramillo normal subzone occurs in the middle-lower parts of the vermiculated red soil (VRS),which indicate that the parent material for the VRS deposited in the middle Quaternary. Sedimentologic and geochemical studies suggest that the Chengdu Clay and part of the parent material for the VRS are of aeolian origin. Pollen analysis indicates that the Chengdu Plain was mainly covered by needle-leaved forest with a cool to cool temperate humid climate when the parent material for the VRS deposited. The relatively cool to cool temperate climatic condition in the Chengdu Plain in the middle Quaternary,which may be caused by the uplift of the Tibetan Plateau,was a response to the geo-environmental changes of global significance.

关键词： Institute of Geomechanics Chinese Academy of Geological Sciences Beijing 100081 China

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A New Method to Identify Quaternary Moraine:Acoustic Emission Stress Measurement

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Acta Geologica Sinica(English Edition) 2006年第5期80卷 754-758页

作者： zhao zhizhong QIAO Yansong TIAN Jiaorong WANG Min LI Mingze HE Peiyuan QIAN Fang Institute of Geomechanics Chinese Academy of Geological Sciences Beijing 100081 China University of Geosciences Beijing 100083 Lushan Administrative Bureau Jiujiang Jiangxi 332900

How to effectively identify glacial sediments, especially Quaternary moraine, has been in dispute for decades. The traditional methods, e.g., sedimentary and geomorphologic ones, are facing challenge in eastern China where controversial moraine deposits are dominatingly distributed. Here, for the first time, we introduce the acoustic emission （AE） stress measurement, a kind of historical stress measurement, to identify Quaternary moraine. The results demonstrate that it can be employed to reconstruct stress information of glaciation remaining in gravels, and may shed light on the identification of Quaternary moraine in eastern China. First, we measured the AE stress of gravels of glacial origin that are underlying the Xidatan Glacier, eastern Kunlun Mountains in western China. Second, we calculated the stress according to the actual thickness of the glacier. The almost identical stress values suggest that the glacial gravels can memorize and preserve the overlying glacier-derived aplomb stress. And then we introduce this new approach to the controversial moraine in Mount Lushan, eastern China. The results indicate that the stress is attributed to the Quaternary glacier, and the muddy gravels in the controversial moraine in Mount Lushan are moraine deposits but not others.

关键词： acoustic emission stress gravel moraine glaciation Quaternar

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基于混合密度和微簇聚合的密度峰值聚类算法

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淮北师范大学学报（自然科学版） 2024年第1期45卷 62-70页

作者：赵志忠陈素根安庆师范大学数理学院安徽安庆246133

密度峰值聚类算法是一种简单高效聚类新算法,但该算法在处理密度分布不均匀数据集时,很难找到正确的类簇中心,并且在样本分配过程中容易出现错误连带现象,导致聚类效果不佳。针对上述问题,提出一种基于混合密度和微簇聚合的密度峰值聚... 详细信息

密度峰值聚类算法是一种简单高效聚类新算法,但该算法在处理密度分布不均匀数据集时,很难找到正确的类簇中心,并且在样本分配过程中容易出现错误连带现象,导致聚类效果不佳。针对上述问题,提出一种基于混合密度和微簇聚合的密度峰值聚类算法(HMDPC)。HMDPC算法首先根据反向K近邻和样本间的归属关系定义样本的混合密度;其次,将数据划分为多个微簇,定义微簇之间的相似度,基于此相似度对多个微簇进行聚合,从而获得最终的聚类结果。在人工数据集和UCI数据集上进行实验,并将HMDPC算法与其它6种聚类算法比较,实验结果表明HMDPC算法聚类效果较好。

关键词：密度峰值聚类反向K近邻混合密度微簇聚合

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Geochemical Characteristics of Eolian Deposits in the Chengdu Plain of Sichuan Province and the Implications for Provenance

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Acta Geologica Sinica(English Edition) 2013年第6期87卷 1712-1723页

作者： TAN Yuanlong QIAO Yansong zhao zhizhong WANG Yan QI Lin FU Jianli LIU Zongxiu YAO Haitao WANG Shubing JIANG Fuchu Institute of Geomechanics Chinese Academy of Geological Sciences Key Laboratory of Neotectonic Movement and Geohazard

In this study Chengdu Red Earth （CRE） from the Chengdu Plain （CP）,Sichuan province,was analyzed for its elemental （major and trace elements） and isotopic （Sm-Nd） geochemistry and compared with Pleistocene loess and paleosol samples from the Chinese Loess Plateau （CLP） in Northern China.The geochemical composition of CRE is similar to north China loess,and also resembles the average UCC.This indicates that CRE,as loess deposits in Northern China,was derived from well-mixed sedimentary protoliths that have undergone numerous upper crustal recycling processes.However,obvious differences in the geochemical characteristics of CRE and the north China loess are also revealed in our results.For chemically stable elements,CRE has higher Ti,Zr,Hf and lower ΣREE,Ba contents in comparison with loess samples from the CLP.Further analysis shows that CRE has higher TiO2/Al2O3,SiO2/Al2O3,Ba/Rb and lower Ce/Yb,Eu/Yb,LaN/YbN and ΣLREE/ ΣHREE ratios.In Sm-Nd isotopic geochemistry,Sm and Nd content and the εNd（0） value in CRE are significantly higher than those in north China loess.The higher TiO2 content in CRE coincided with a high background concentration of Ti in the Sichuan Basin and the surrounding regions.The lower ΣREE and higher Sm,Nd,εNd（0） values are related to the wide distribution of basalt in the southwest Sichuan Basin.The elemental and isotopic geochemistry of CRE indicates that eolian materials in the CP predominantly come from the Sichuan Basin and the surrounding regions,which differs from loess deposits in the CLP.

关键词： The Chengdu Plain Chengdu red earth eolian deposits geochemical characteristics provenance

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Late Cenozoic Geology and Paleo-environment Change in the Eastern Edge of Qinghai-Xizang Plateau

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Acta Geologica Sinica(English Edition) 2008年第5期82卷 959-966页

作者： zhao zhizhong QIAO Yansong WANG Shubing YAO Haitao WANG Yan LI Chaozhu FU Jianli LIU Zongxiu LI Mingze MIAO Qi JIANG Fuchu Institute of Geomechanics Chinese Academy ofGeosciences Beijing 100081 China Open Laboratory of Lake Sediment and Environment Chinese Academy of Sciences Nanjing 210008 Jiangsu China

There are late Cenozoic lacustrine deposits and loess and red clay and moraines in eastern edge of the Qinghai-Xizang Plateau. Various genetic sediments recorded rich information on late Cenozoic paleo-environment changes. Xigeda lacustrine formed during 4.2 Ma B.P.-2.6 Ma B.P. There were 9 periodic warm-cold alternations. Eolian deposition in western Sichuan began at 1.15 Ma B.P. The loess-soil sequences recorded successively 14 paleo-monsoon climate cycles. Laterite in Chengdu plain recorded 5 stages of paleoclimatic stages since 1.13 Ma B.P. There was an old glacial period of 4.3 Ma B.P. in eastern Qinghai-Xizang Plateau. During Quaternary, there are 5 extreme paleoclimatic events corresponding with 5 glaciations.

关键词： Qinghai-Xizang Plateau Xigeda lacustrine Loess in western Sichuan Chengdu laterite Quaternary glaciations

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海南岛尖峰岭热带雨林土壤固碳微生物群落特征

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土壤 2024年第1期56卷 64-72页

作者：陈红利赵志忠吴丹余玉莹韩知序霍红义海南师范大学地理与环境科学学院海口571158

采集海南岛尖峰岭地区低地雨林次生林、山地雨林次生林和山地雨林原始林土壤,基于绝对定量PCR和高通量测序技术,探讨了热带雨林土壤中固碳微生物群落结构的多样性与组成及其影响因素。结果表明:固碳微生物的Alpha多样性与基因丰度均表... 详细信息

采集海南岛尖峰岭地区低地雨林次生林、山地雨林次生林和山地雨林原始林土壤,基于绝对定量PCR和高通量测序技术,探讨了热带雨林土壤中固碳微生物群落结构的多样性与组成及其影响因素。结果表明:固碳微生物的Alpha多样性与基因丰度均表现为低地雨林次生林高于山地雨林原始林;尖峰岭热带雨林土壤固碳微生物优势菌门为假单胞菌门(Pseudomonadota,44.28%~70.60%)和放线菌门(Actinomycetota,11.95%~33.73%),优势菌属为慢生根瘤菌属(Bradyrhizobium,11.53%~31.06%)、诺卡氏菌属(Nocardia,4.97%~17.07%)、中慢生根瘤菌属(Mesorhizobium, 4.44%~12.97%)、分枝杆菌属(Mycobacterium, 2.62%~9.20%)、芽绿菌属(Blastochloris,4.34%~10.12%)、固氮弧菌属(Aromatoleum,1.97%~5.39%)、分枝菌酸杆形菌属(Mycolicibacterium,1.71%~3.78%)、固氮螺菌属(Azospirillum,1.97%~2.65%)、Methylibium (1.22%~3.77%),且以兼性自养菌为主。PCoA与LEfSe分析表明,热带雨林3个林型土壤固碳微生物群落存在差异,其标志物种分属放线菌纲、γ-变形菌纲、α-变形菌纲和β-变形菌纲。RDA分析表明,全氮、全磷、有机碳、易氧化有机碳是驱动尖峰岭热带雨林固碳微生物群落差异的重要影响因素。

关键词：热带雨林固碳微生物高通量测序 cbbL基因

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早/晚抽薹性大白菜自交系中光敏色素B及光周期关键基因的动态研究

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华北农学报 2024年第2期39卷 11-18页

作者：刘栓桃王树彬王荣花王立华李巧云张志刚赵智中山东省农业科学院蔬菜研究所国家蔬菜改良中心山东分中心山东省设施蔬菜生物学重点实验室山东济南250100

光周期是影响植物抽薹开花最重要的环境因子之一,光周期信号通过植物的光敏色素蛋白调控植物的抽薹开花,其中PHYB介导的信号网络对植物抽薹开花有重要的抑制作用。前期研究发现,大白菜耐抽薹材料06-247与易抽薹材料He102的PHYB基因启动... 详细信息

光周期是影响植物抽薹开花最重要的环境因子之一,光周期信号通过植物的光敏色素蛋白调控植物的抽薹开花,其中PHYB介导的信号网络对植物抽薹开花有重要的抑制作用。前期研究发现,大白菜耐抽薹材料06-247与易抽薹材料He102的PHYB基因启动子存在大片段插入/缺失差异,为了进一步研究启动子突变对PHYB及其下游途径关键基因的影响,以耐抽臺材料06-247与极易抽臺材料He102为试验材料,采用生物信息法分析了大白菜基因组中光敏色素基因的冗余特点,发现大白菜基因组包含6个光敏色素基因,其中PHYA有2个拷贝,PHYB、PHYC、PHYD和PHYE都仅有1个拷贝。进一步通过氨基酸序列比对筛选出了PHYB的特异序列、设计了抗原决定簇并制备了抗大白菜PHYB的特异抗体,采用荧光定量RT-PCR技术和Western Blot技术研究了06-247与He102中PHYB的相对含量,同时比较了PHYB下游光周期通路关键调控基因CCA1、FLC、CO和FT的动态变化。结果表明:启动子突变造成PHYB在06-247中表达水平显著升高并进而造成PHYB蛋白水平显著升高,同时下游调控基因CCA1、FLC、CO和FT均在06-247中高水平表达,这对06-247的耐抽薹特性有重要影响。

关键词：大白菜 PHYB 光周期抽薹蛋白质印迹

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