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1.
刘宁  赵国  刘刚 《农业工程学报》2021,37(18):232-243
溶出伏安法具有分析速度快、成本低、灵敏度高等优点被广泛应用于检测土壤重金属含量,但在检测土壤重金属时,溶出伏安检测精度会受到多方面因素的影响。该文在介绍溶出伏安法工作原理的基础上,从伏安参数、试验条件和土壤物质成分三方面阐述溶出伏安法检测土壤Pb2+和Cd2+为的影响因素,解析各因素的影响机理,归纳影响削弱方法的研究进展。研究结论为:方波脉冲阳极溶出伏安法最常用于检测土壤Pb2+和Cd2+,伏安参数包括脉冲幅值、电压增量和脉冲频率,试验条件包括沉积时间、沉积电压和支持电解质种类及其pH值,土壤成分主要干扰因素包括非目标重金属和有机质。针对伏安参数和试验条件的影响可以设计优化试验有效削弱。针对非目标重金属和有机质的干扰影响,目前研究还没有提出有效的削弱方法。最后,展望了溶出伏安法检测土壤重金属的未来发展方向。  相似文献   
2.
金属硫蛋白是一类富含巯基的低分子量蛋白,在植物的重金属解毒及细胞氧化还原调控等方面起重要的作用。本研究以甘蔗热带种Badila组培苗为材料,分别测定了其在CdCl2、ZnSO4和CuCl2水溶液培养条件下地上部和地下部的重金属含量,结果显示其对上述3种重金属有较强的耐受与富集能力。继而克隆了ScMT1(登录号为KJ504373)、ScMT2-1-5(登录号为MH191346)和ScMT3(登录号为KJ5043704)3个金属硫蛋白家族基因,它们分别属于植物MT亚家族中的MT1、MT2和MT3型基因。ScMT1含有1个内含子和2个外显子,开放阅读框(Open Reading Frame,ORF)长228 bp,编码75个氨基酸;ScMT2-1-5含有2个内含子和3个外显子,ORF长246 bp,编码81个氨基酸;ScMT3含有1个内含子和2个外显子,ORF长198 bp,编码65个氨基酸。RT-qPCR显示,Cd2+胁迫下,在甘蔗地上部和地下部,ScMT2-1-5均连续显著上调表达,而ScMT1的上调应答出现延迟。ScMT3在地上部的上调应答出现延迟,在地下部呈“扬-抑”趋势,提示甘蔗响应Cd^2+胁迫过程中ScMT2-1-5起更积极的作用,ScMT1参与胁迫后期的分子响应,而ScMT3不起主导作用。Cu^2+胁迫下,地上部ScMT1连续显著上调表达,ScMT2-1-5和ScMT3呈总体上调的表达趋势;地下部,ScMT1和ScMT2-1-5的上调表答均出现延迟,仅在胁迫后期显著上调表达,而ScMT3仅在胁迫前期显著上调表达。该结果提示了ScMT1、ScMT2-1-5和ScMT3在Cu2+胁迫响应过程中的协作关系,三者共同参与了地上部的胁迫响应,其中ScMT1起更积极的作用;此外三者还先后参与了地下部对Cu^2+胁迫的分子响应。Zn^2+胁迫下,ScMT1和ScMT3分别仅在地上部和地下部显著上调表达;ScMT2-1-5在地上部和地下部均呈“扬-抑”的应答趋势;提示了在甘蔗响应Cd^2+胁迫应答过程中ScMT1和ScMT3分别在地上部和地下部起主要作用,ScMT2-1-5参与了胁迫前期的分子响应。ScMT1、ScMT2-1-5和ScMT3在甘蔗不同组织中及在重金属(Cd^2+、Zn^2+或Cu^2+)不同累积水平下呈现出相似或互补的应答特性,提示上述甘蔗MT家族不同成员在重金属解毒及细胞氧化还原调控等方面产生了功能分化,且三者在应对过量Cd^2+、Zn^2+或Cu^2+对甘蔗组织造成伤害的过程中存在时空上的协同作用。该研究为深入理解多倍体植物甘蔗中MT家族各成员基因在重金属耐受过程中的协同作用机制奠定了基础。  相似文献   
3.
为了给内蒙古高原紫花苜蓿(Medicago sativa L.)测土施氮奠定科学基础,本研究采用“零散实验数据整合法”和“养分平衡-地力差减法”新应用公式,开展了该自然区域紫花苜蓿土壤氮素丰缺指标和推荐施氮量研究。结果表明:内蒙古高原生长第1年紫花苜蓿土壤碱解氮第1~6级丰缺指标为≥48,20~48,8~20,4~8,2~4和<2 mg·kg-1,土壤全氮第1~5级丰缺指标为≥1.4,0.8~1.4,0.4~0.8,0.2~0.4和<0.2 g·kg-1,土壤有机质第1~6级丰缺指标为≥17,10~17,6~10,3~6,2~3和<2 g·kg-1。当紫花苜蓿目标产量9~18 t·hm-2、氮肥利用率40%时,内蒙古高原紫花苜蓿第1~6级土壤推荐施氮量分别为0,68~135,135~270,203~405,270~540和338~675 kg·hm-2。  相似文献   
4.
5.
李美琪  贾小卫  郭蕊  吴丹  刘浩 《绿色科技》2020,(6):34-37,42
利用FNL再分析资料、卫星资料和自动站资料对2019年7月22~23日京津冀一次区域性暴雨过程进行了环流形势、卫星云图、动热力结构的分析。结果表明:此次暴雨发生在500hPa两槽一脊、副热带高压北抬、低空急流的大尺度环流背景下。西南方向的水汽输送和黄渤海的补充水汽为暴雨提供了良好的水汽条件,在河北中部的水汽辐合抬升则为暴雨提供了抬升条件。此次暴雨的产生受中尺度对流云团的连续生成合并影响,降水效率高。在暴雨中心整层表现为低层辐合、高层辐散,上升速度中心明显,使得高层的抽吸作用更强,更有利于上升运动的维持与发展,为降水强度增大提供了有力的动力条件,高空弱冷空气的入侵对能量锋区不稳定能量的释放起到了触发作用。  相似文献   
6.
The increased recognition of the importance of soil is reflected in the UN Post‐2015 Development Agenda with sustainable development goals that directly and indirectly relate to soil quality and protection. Despite a lack of legally binding legislation for soil protection, the European Commission remains committed to the objective of soil protection. However, the achievement of a legally binding framework for soil protection relies on the implementation of a soil monitoring network (SMN) that can detect changes to soil quality over time. As beneficiaries do not pay for the provision of soil information, the options for soil monitoring are limited. The use of existing data sets should be considered first. Using Ireland as an example, this research explored the opportunities for a SMN for Ireland considering three existing national data sets. The options for a SMN are considered in terms of their spatial and stratified distribution, the parameters to be measured and an economic analysis of the options proposed. This research finds that for Ireland, either a 10 or a 16 km2 grid interval stratified by land use and drainage class offers the best potential in relation to the spatial distribution of existing data sets to reflect local data at a national level. With existing data, the stratified SIS data using the 16 km2 grid offers the best value for money, with baseline costs for analysis, excluding field costs, of between €706 481 and €2.8 million. Acknowledging the impossibility of measuring all parameters with ideal frequency, this study proposes a two‐tier system for optimized monitoring frequency. Parameters must anticipate future policy requirements. Finally, the implementation of a SMN must be accompanied by standardized methods, defined thresholds and action mandates to maintain soil quality within allowable limits.  相似文献   
7.
SUMMARY: Aoshio is hypoxic milky blue-green seawater observed in some eutrophic bays. Previous studies have shown that colloidal sulfur causes the coloration and that the source of aoshio water is attributed to coastal anoxic bottom water. Occurrences of aoshio have been reported in limited areas of coastal seawater, although hypoxic transparent water seems rather universal. Promotion in auto-oxidation of sulfide by metal ions in seawater was investigated to explain the occurrences of aoshio. Artificial seawater containing 10 μM metal ion was assayed for the sulfide oxidation rate. The velocity constant which represents the oxidation rate within the initial 30 min and the amount of reacted sulfide in 2 h were determined by oxygen monitoring and sulfide quantification, respectively. Fe2+ and Cu2+ enhanced the initial 30 min reaction. Fe2+, Fe3+ and Ni2+ increased the amount of reacted sulfide in 2 h, forming whitish turbid water. Seawater from a suspected source of aoshio water was also assayed for the auto-oxidation rate of sulfide. The oxidation rate in water from 12 m depth was 13–19 times higher than the artificial seawater without an addition of heavy metal ions. More than 15% of the oxidation rate in 12 m deep seawater was explained by dissolved iron in the seawater.  相似文献   
8.
In this research, five Nitraria sibirica provenances such as Dayilu were selected to do experiment of salt-resistance, combining fixed plots test with typical plot investigation, measuring survival rate and growth as main indicators. The experiments of main cultural technology were done on Nitraria sibirica in 4 types of site preparation, 3 types of planting, 3 designs for planting density. The Nitraria sibirica experiments for the effects of curbing salt and improving soil were done by testing soil nutrients, salt content, soil physical properties as focal points in typical site of 3-4 years woods. The experiment results showed that the Nitraria sibirica could survive well with soil salt content of 0.6%, and that survival rate declined distinctively as soil salt content exceeded 0.8%. However, high soil salt content did not influence growth in the year of planting. There were obvious differences in salt-tolerance among Nitraria sibirica provenances; Dayilu was the best on salt-tolerance, the other 4 pro  相似文献   
9.
Soil pH declined from 5.9 to 5.0 in 8 years beneath plantations of Eucalyptus saligna (Sm.) in Hawaii. In stands of Albizia falcataria, (L.) Fosberg, the soil pH change was more dramatic, declining from 5.9 to 4.6. We measured several components of soil acidity beneath four mixtures of the two tree species to gain insight on the processes responsible for the decline in soil pH. These components were studied using an empirical method of comparing acid quantity, degree of neutralization (depletion of base cations), and acid strength. The decline in soil pH differed between species as a result of differences in the degree of neutralization of the soil exchange complex; the larger decrease in soil pH under Albizia was produced by greater acidification of the exchange complex. Empirical titration curves suggested that differences in acid strength moderated the divergence in soil pH beneath the species. Had the acids accumulating in the soil under Albizia been as strong as those in the Eucalyptus soil, the difference in soil pH would have been greater. Though the two species had contrasting effects on soil pH, the differences in degree of neutralization, responsible for the pH decline, were small compared with differences in the amount of cations stored in tree biomass. Continued supply of nutrient cations (from weathering or fertilization) will ultimately control both the extent of soil pH decline and the level of productivity sustained by the forest.  相似文献   
10.
Abstract. In field and laboratory experiments the conditioner‘Agri-SC’has shown improvements in the structure of loamy sand soils in east Shropshire, UK. It resulted in statistically significant decreases in soil bulk density values and increases in soil porosity and aggregate stability. Further experiments are in progress on both loamy sand and silt loam soils.  相似文献   
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