137Cs dating of lacustrine sediments and human impacts on Dalian Lake,Qinghai Province,China

¹³⁷Cs and grain-size analyses indicate the total amounts of ¹³⁷Cs deposited by wind and water in the Dalian Lake of Gonghe Basin, Qinghai Province. The vertical profile of ¹³⁷Cs in the lacustrine sediments shows three ¹³⁷Cs activity peaks and one trough: the main peak corresponds to the global ¹³⁷Cs fallout in 1963; the two secondary peaks correspond to the leakage of the Chernobyl reactor in 1986 and complete desiccation of the lake in 1994. The trough corresponds to aeolian deposition caused by extensive reclamation of farmland in late 1980s and early 1990s. The ¹³⁷Cs dating was used to evaluate sedimentation rates in Dalian Lake since 1963. They are divided into three periods: two with slow deposition (1963–1986 and 1994–1998), and one with rapid deposition (1986–1994). ¹³⁷Cs seems to have the same potential for indicating environmental changes and human interference in the arid and semiarid regions as in humid regions.     

农膜残留对大豆光生理特征及生物量累积的影响

农膜覆盖技术的应用及推广极大地提高了干旱半干旱地区的农业产量,促进了当地农业发展及社会经济效益。然而,由于农膜碎片化程度高、回收难度大、降解周期长,使得残留在土壤中的农膜日益增多,严重威胁着作物生长、土壤健康以及农业可持续发展。尽管农膜残留对土壤质量影响的研究较多,但对于其种类(可降解或不可降解)及残留累积量对作物光生理特征的研究还相对较少。本试验以大豆为研究对象,对比普通聚乙烯(PE)和生物降解(BP)两种农膜(残片大小为0.5～2 cm),研究不同农膜残留累积量(土壤重量的0、0.1%、0.5%、1.0%)下大豆花期及初荚期叶片光合作用光、CO_2响应曲线特征及花期、收获期的植株生物量,探讨塑料类型及残留量对大豆光生理特征及生物量累积的影响。结果表明:PE残留导致大豆叶片光补偿点在花期降低23.96%,而初荚期升高51.38%,说明PE残留导致大豆叶片弱光利用能力在花期提升,但在初荚期被抑制。在初荚期,BP残留使光补偿点降低54.82%,且光饱合点升高58.12%,从而提高了叶片强光适应能力,增大了叶片光能利用范围。同时, PE和BP添加使暗呼吸速率分别增长30.56%和22.28%,从而导致干物质消耗增加。土壤中PE、BP残留量的增加,最大光合力分别降低36.49%和23.56%,表明大豆叶片CO_2利用能力减弱; CO_2补偿点分别降低67.96%和38.91%,从而提高了叶片低浓度CO_2的利用能力,并降低光呼吸速率,从而减少了干物质的消耗。此外,不同农膜及残留量处理下,仅在花期0.1%与0.5%残留量的BP处理中,地下生物量随农膜残留量的增加显著降低,其他各处理间地上及地下生物量无明显变化。光响应及CO_2响应曲线各拟合参数与生物量的Pearson相关性分析结果表明,收获期PE处理下,地上生物量与光补偿点呈显著负相关,而光呼吸速率、CO_2补偿点、初始羧化效率与生物量(地上+地下)的积累有较强相关性。因此,PE农膜残留量增加提高了大豆花期叶片对于弱光的利用能力而减弱初荚期对弱光的利用能力,BP农膜残留量增加则会增强初荚期叶片对弱光的利用,也对大豆叶片适应强光的能力有所提升。     

Quantifying key model parameters for wheat leaf gas exchange under different environmental conditions

The maximum carboxylation rate of Rubisco(V_(cmax)) and maximum rate of electron transport(J_(max)) for the biochemical photosynthetic model, and the slope(m) of the Ball-Berry stomatal conductance model influence gas exchange estimates between plants and the atmosphere. However, there is limited data on the variation of these three parameters for annual crops under different environmental conditions. Gas exchange measurements of light and CO_2 response curves on leaves of winter wheat and spring wheat were conducted during the wheat growing season under different environmental conditions. There were no significant differences for V_(cmax), J_(max) or m between the two wheat types. The seasonal variation of V_(cmax), J_(max) and m for spring wheat was not pronounced, except a rapid decrease for V_(cmax) and J_(max) at the end of growing season. V_(cmax) and J_(max) show no significant changes during soil drying until light saturated stomatal conductance(gssat) was smaller than 0.15 mol m~(–2) s~(–1). Meanwhile, there was a significant difference in m during two different water supply conditions separated by gssat at 0.15 mol m~(–2) s~(–1). Furthermore, the misestimation of V_(cmax) and J_(max) had great impacts on the net photosynthesis rate simulation, whereas, the underestimation of m resulted in underestimated stomatal conductance and transpiration rate and an overestimation of water use efficiency. Our work demonstrates that the impact of severe environmental conditions and specific growing stages on the variation of key model parameters should be taken into account for simulating gas exchange between plants and the atmosphere. Meanwhile, modification of m and V_(cmax)(and J_(max)) successively based on water stress severity might be adopted to simulate gas exchange between plants and the atmosphere under drought.     

氧化石墨烯和五价砷在改性多孔介质中的共迁移特征

砷是农田土壤重金属污染的主要元素之一,在砷污染农田土壤的修复过程中往往忽视纳米颗粒能够使结合态的砷重新释放,导致有效态砷浓度升高,探究土壤中黏土矿物对氧化石墨烯(Graphene Oxide,GO)和五价砷(As(V))在多孔介质中迁移行为的影响,对进一步完善农田土壤砷修复理论以及提高农作物产量、保护人体健康具有重要意义。该研究利用蒙脱石和高岭石改性石英砂,通过砂柱迁移试验系统地研究了GO、As(V)和GO-As(V)在填加0%、10%、30%和50%的蒙脱石和高岭石改性石英砂柱中的迁移行为。研究结果表明,随着高岭石和蒙脱石改性石英砂填加比例的增加,GO和As(V)的迁移能力均呈降低趋势,且GO和As(V)在不同条件下的迁移曲线均存在显著差异(P0.05);GO在50%高岭石和蒙脱石改性石英砂柱中的回收率相对于石英砂柱分别下降了14%和17%,As(V)分别下降了15%和12%;在共迁移试验中,GO和As(V)在石英砂柱中回收率分别上升至99%和100%。分析表明,As(V)在蒙脱石改性石英砂柱中的迁移能力大于高岭石改性石英砂,而GO与之相反;当GO和与As(V)共迁移时,二者在介质中的迁移能力均大于其单独迁移。本研究表明GO、As(V)释放到土壤后,能够加速As(V)的迁移,造成土壤砷污染的扩大化。     

Effects of agriculture,climate, and policy on NDVI change in a semi-arid river basin of the Chinese Loess Plateau

In 1999, the Grain for Green Project was implemented by the Chinese government. Since then, the vegetation of Zuli River Basin, a semi-arid river basin of the Chinese Loess Plateau, has been greatly changed. Clearly understanding the impact of natural and artificial factors on vegetation change is important for policy making and ecosystem management. In this study, spatio-temporal variations in vegetation cover in Chinese Zuli River Basin during 1999–2016 were investigated using Landsat normalized difference vegetation index (NDVI) data. Analyses of several indicators, including changes in NDVI in different slopes and land use changes and the relationships between climatic factors and NDVI change, were presented to quantitatively evaluate the effects of agriculture, climate, and policy on NDVI change. The NDVI in the Zuli River Basin increased during the study period, and the main contributors to this change were forest in 1999–2011, cropland, abandoned farmland, and grassland in 2009–2016, and land with slopes ≤ 15°. Land with slope > 15°, where the “Project” was implemented, slightly contributed to the increase in regional NDVI. In 1999–2011, the project (?98.16%) combined with climate change (?68.18%) showed negative effects on the increase in NDVI in the Zuli River Basin, but agriculture (22.28%) played a positive role in increasing this index. In 2009–2016 and 1999–2016, the project (38.45% and 35.25%, respectively), the project combined with climate change (49.83% and 46.30%, respectively), agriculture (18.61% and 23.30%, respectively), promoted increases in NDVI in the basin.     

中国河湖沼系统时空变化特征及驱动力影响分析

河湖沼系统具有重要的水资源涵养及调节功能,对我国的经济发展、生态保护等具有十分重要的意义。本研究以中国河湖沼系统为研究对象,以土地利用类型数据为基础,采用ArcGIS空间分析法、转移矩阵及相关系数计算等方法,核算探究1990至2015年中国河湖沼系统水面率的时空变化特征及迁移转换趋势,在此基础上,定量及定性对我国河湖沼系统的变化驱动力影响开展分析及讨论。结果表明：（1）河湖沼系统主要分布在我国的东部地区,其中东北地区分布最为广泛,其次是长江区域中下游和西南地区;（2）我国河湖沼系统水面率在1990-2010年总体变化幅度较小,而2010-2015年有所增加,且河湖沼系统中水面率沼泽>湖泊>河流;（3）1990-2015年河湖沼主要与耕地、草地和林地之间发生地类的迁移转换,其中沼泽与草地间的迁移转化趋势更明显;（4）相关系数结果表明,人为因素与河湖沼系统变换相关性更显著,是河湖沼系统短期内时空变化的主要原因;自然因素对河湖沼系统时空变化的影响持久且稳定。本研究结果可为国家合理规划和配置水资源提供基础,对保障我国经济健康可持续发展具有重要意义。     

耕地空间保护格局影响因素及整治规划对策——以甘肃省平凉市崆峒区为例

[目的]通过对耕地保护现状空间格局成因及其空间相关性分析,划分科学的耕地整治规划分区,为进一步优化崆峒区耕地布局,提升耕地质量,科学利用、保护耕地提供参考。[方法]以甘肃省平凉市崆峒区为例,采用景观格局指数法、多目标决策法、Spreaman秩相关法、聚类分析法,选取耕地坡度、耕地保护政策、城镇化影响来分析耕地景观格局现状与其在空间上的存在的协同或权衡关系,构建耕地保护格局相关性分析评价指标体系。[结果](1)研究区整体上耕地景观格局指数2010—2022年上升3.55%,耕地集聚程度大部分区域呈现下降趋势,但在整个过程中呈现波动。区域土地利用程度整体上呈上升趋势,各乡镇耕地布局特征及土地利用程度差异明显。(2)耕地保护指数2022年较2010年上升315.30%,2°～6°耕地增加120.96%,15°～25°耕地减少32.64%,>25°耕地减少100%,耕地质量提升明显,与耕地景观格局在空间上高度协同;城镇化影响指数呈上升趋势。2010—2022年城镇化影响指数上升25.17%,城镇化对耕地布局影响加大,与耕地景观格局在空间上存在权衡关系。(3)划分耕地质量提升重点区、耕地质...     

矿区生态修复过程中不同立地类型土壤水动力学特性

[目的]揭示矿区不同立地土壤水动力学特性及其影响因素,为矿区生态环境恢复治理提供科学依据。[方法]基于矿区不同立地类型土壤水分特征曲线、非饱和导水率、孔隙度与紧实度等监测试验,揭示不同立地类型土壤持水性、有效水含量和导水特性等变化规律。[结果]土壤持水性和供水性在受损区<修复3a区<修复5a区<修复10a区<修复15a区<未干扰区,但修复区20—40cm土壤持水性、供水性较0—20cm土壤低,修复效果不明显;土壤结构改善效果遵循受损区<修复区<未干扰区的变化规律,且修复区亚表层土壤结构改善效果不明显。采用指数函数拟合吸力和非饱和导水率效果较好(r2>0.95),相同吸力下,容重大而非饱和导水率较小;非饱和导水率和容重呈负相关,和孔隙度呈正相关且相关性随吸力增加降低。矿区0—20cm易有效含水量呈现受损区<修复3a区<修复5a区<修复10a区<未干扰区<修复15a区,但修复区20—40cm土层易有效水含量较0—20cm小。[结论]土壤易有效水含量和容重、紧实度呈负相关关系,与总孔隙度、黏粒含量呈正相关关系。修复后土壤结构有所改善,持蓄调节水分能力有所提高。     

白膜、黑膜全年覆盖下的土壤水、热、盐变化

地膜覆盖因能有效地增温保墒增产而在黄土丘陵区旱作农林生产中广泛应用。为明确不同薄膜覆盖的差异以及连续覆膜条件下的土壤水热盐变化特征,于2015年7月1日—2017年6月30日在陕北米脂进行野外连续覆膜定位观测,试验设裸地(CK)、白色薄膜(WF)与黑色薄膜(BF)3种处理,利用GS3仪器监测0～150cm深度的土壤水分、温度和电导率。结果表明:1)连续覆盖两年后,两种覆膜处理平均土壤含水量为16.9%, CK为13.6%,土壤储水量分别达314.56mm、204.44mm,具体表现为土壤含水量BF在0～15cm高于WF(P0.05),15～30cm低于WF(P0.05); 0～150 cm, WF和BF总储水量差异不显著,与CK差异显著(P0.05);在作物生育期覆膜平均较CK提高储水量60.8 mm。2)膜覆盖下近地面日温差WF大于BF, 0～150 cm,两种覆膜周年土壤平均温度无显著差异,较CK高1.3℃(P0.05);气温较高条件下WF比BF、CK缩短冻融时间分别达8d和24d,WF更有利于土壤解冻和早春土壤增温。3)周年土壤表层盐分高,其中0～30 cm土层电导率为BFWFCK, 30～50 cm土层为WFBFCK,但土壤总体盐分较低,无土壤盐渍化趋势, 50 cm以下3种处理盐分没有差异。综合而言, WF较BF更能提高表层土壤温度, BF较WF更能提高表层土壤水分,覆膜保墒增温,延长作物生长时间。研究成果可为黄土丘陵区旱作农业覆膜应用提供土壤水热盐调控依据,也为果园和林地常年连续覆膜提供参考。     

转基因小麦抗旱性鉴定及相关指标灰色关联度分析

以9份转ABP9基因春小麦株系UC4-1~UC4-9及其受体亲本宁春4号为材料,在雨养和灌溉条件下,对这些材料的主要农艺性状和部分生化指标进行了测定,采用隶属函数值法和抗旱性度量(D)值法对其抗旱性进行了综合评价,并利用灰色关联度法对相关抗旱性状与抗旱指数之间的关联度进行了分析评价。结果表明:6份转基因小麦的抗旱性较受体亲本宁春4号增强,3份材料的抗旱性较非转基因春小麦品种定西35增强;各农艺性状和生化指标与抗旱指数的关联度从高到低依次分别为株高、单穗粒重、穗长、SOD活性、穗粒数、结实小穗数、有效分蘖数、POD活性、千粒重、脯氨酸含量、MDA含量。