祁连山黑河上游不同退化草地有机碳和酶活性分布特征

为揭示草地退化过程中土壤有机碳和酶活性的分布特征及相关性,在祁连山黑河上游俄博岭区域的高山灌丛草甸土上,根据草地退化程度,划分了未退化草地、轻度退化草地、中度退化草地、重度退化草地,采用野外采样室内分析方法,研究了不同退化草地土壤有机碳和酶活性的分布特征。结果表明：4种退化草地0～60 cm土层有机碳的含量、密度、储量,以及土壤酶活性变化顺序为：未退化草地>轻度退化草地>中度退化草地>重度退化草地;4种退化草地（从轻到重）0～10 cm土层有机碳密度是50～60 cm土层有机碳密度的1.78倍、1.98倍、1.87倍和2.00倍,说明土壤有机碳密度在表层具有很强的表聚性;4种退化草地不同土层有机碳的含量、密度和储量,以及土壤酶活性均随着土壤剖面垂直深度的增加而递减;4种退化草地土壤有机碳含量与有机碳密度、土壤酶活性成显著正相关关系。     

苜蓿草地土壤呼吸及其对环境响应的研究

采用LI-8100对河北沽源牧场地区3年生苜蓿(Medicago sativa L.)草地生长季土壤呼吸速率日动态以及季动态进行测定,分析了土壤呼吸速率与土壤温度、土壤湿度和大气辐射的相关性。结果表明:苜蓿草地的土壤呼吸日动态呈单峰曲线,各观测日的最小值分别为3.102,2.071,4.655,4.52,3.355μmol·m^-2·s^-1,出现在每天8:00-9:00和18:00-19:00之间,相对应的最大值分别是4.934,3.034,6.948,5.682,4.823μmol·m^-2·s^-1,出现在13:00-16:00之间。土壤呼吸速率日动态与5 cm土壤温度的相关性最大,R2的值为0.2722~0.8214(P<0.05),与10 cm土壤温度有一定的相关性,与20 cm土壤温度相关性不大。土壤呼吸季动态呈不规则单峰曲线,最小值是2.48μmol·m^-2·s^-1,出现在6月26日,最大值是5.79μmol·m^-2·s^-1,出现在7月24日。土壤呼吸季动态与5,10,20 cm深度的土壤温度均无相关性,与5,10,20 cm深度土壤湿度均有极相关关系(P<0.01),与太阳辐射无相关性。     

连作障碍发生机制研究进展

目的研究不同前作对土壤生物化学性质的影响。方法利用化学和酶学分析及16S多样性测序技术,分析种植7年的不同前作[荞麦(FB)、油菜(FR)、小麦(FW)和绿肥(FG)]烟田土壤的养分、酶活性及细菌群落结构组成。结果(1) FR烟田土壤的有机质、全氮、碱解氮和有效磷含量最高,分别为30.04 g/kg、1.62 g/kg、143.50 mg/kg和88.09 mg/kg,FG烟田次之,但FG烟田速效钾的含量最高(240.10 mg/kg);FG烟田土壤蛋白酶和磷酸酶的活性最高,分别为709.02 μg/(g·d)(酪氨酸)和306.60 μg/(g·h)(对硝基酚),而其脲酶和蔗糖酶的活性仅低于FW烟田,且无显著性差异(P>0.05)。(2)在细菌群落组成上,FB、FG、FW和FR烟田分别检测出770、670、654和597属,归属于Actinobacteria、Proteobacteria、Chloroflexi和Acidobacteria等36门,其中Actionbacteria和Proteobacteria相对丰度最高,分别为26.87%~45.21%和25.82%~30.69%,Treptomyces、Bradyrhizobium、Bacillus和Mycobacterium等拮抗菌和Bradyrhizobium、Rhizobium和Paenibacillus等固氮菌在FB烟田土壤细菌群落的相对丰度最高。结论不同前作对烟田土壤理化性质、酶活性和细菌群落结构的影响不同,绿肥提高了土壤有机质和养分含量以及酶活性;而荞麦改善和提高了烟田土壤细菌种群结构和多样性。     

玉米根系分泌物对烟草黑胫病菌的抑制活性及其抑菌物质分析

目的明确玉米、辣椒单作和间作种植后根围土壤细菌群落的变化与病害发生的关系,解析土壤微生物在玉米和辣椒多样性种植中控制病害的作用。方法比较玉米/辣椒间作和分别单作后根围土壤微生物对玉米小斑病和辣椒疫病发生的影响,并应用Illumina Miseq高通量测序技术比较不同处理根围细菌群落的差异。结果单作玉米的根围土壤微生物能显著抑制辣椒疫病的发生(P<0.05),辣椒单作、玉米/辣椒间作后玉米根围土壤微生物降低玉米小斑病的趋势明显。根围土壤细菌群落分析结果表明：单作玉米根围气单胞菌属、堆囊菌属和固氮螺菌属等的相对丰度显著高于间作玉米和单作辣椒根围(P<0.05);单作辣椒和间作玉米根围土壤中拟杆菌门相对丰度上调,并且其中的拟杆菌属、农研丝杆菌属、鞘氨醇杆菌属和Muribaculum的相对丰度也显著上调(P<0.05)。结论玉米/辣椒间作和间作后有利于帮助彼此降低病害的发生。单作或间作后导致土壤细菌群落的变化是其缓解病害发生的重要机制。     

土壤处理对西洋参根际线虫数量动态的影响及对防治茎线虫根腐病的效果

 Root rot of American ginseng (Panax quinquefolium) caused by Ditylenchus destructor is a novel disease found recently in Beijing area. The effects of three soil treatments (fumigating with chloropicrin, chloropicrin + lvfeng organic manure and nematicide fosthiazate) on the number of rhizospheric nematodes, survived plants, root yield and root rot of 3-year ginseng plant were compared. The effects were also investigated at the second year after treatment. The results indicated that the number of parasitic nematodes in rhizosphere of treated soil reached the peak value in late June to early July as the soil temperature raised in the growing season. Compared with the regular treatment, the number of plant parasitic nematodes was reduced while non-plant parasitic nematodes increased. The number of non-plant parasitic nematodes in the soil treated with chloropicrin + lvfeng organic manure was 2 times than that treated with chloropicrin only. The ratio of non-parasitic to parasitic nematodes of three treatments was higher than the control. Percent of survived plants was 94.8%-96.4% and diseased root was decreased obviously. The control efficacy was more than 89% at the first year after treatment. The survived plants and plot yield of ginseng increased significantly and the control efficacy was around 40% at the second year. The best of the three treatments was by chloropicrin + organic manure.     

施肥对热带雨林下种植砂仁土壤氮矿化和硝化作用的影响

采用封顶埋管法(Close-TopIncubation)研究了施肥后西双版纳热带雨林下种植砂仁土壤的氮素净氨化、净硝化和净矿化速率。结果表明,种植砂仁的热带雨林土壤有机氮的净氨化、硝化和矿化速率明显受外来无机氮的影响,施入铵态氮肥后,土壤中的氨化速率明显提高(P<0.01),由对照土壤的-0.66(mg·kg-1·30d-1)增加至施肥处理土壤的1.65(mg·kg-1·30d-1),但硝化速率和矿化速率却显著降低(P<0.01),分别由对照土壤的6.79(mg·kg-1·30d-1)和6.13(mg·kg-1·30d-1)减少至施肥处理土壤的2.60(mg·kg-1·30d-1)和4.25(mg·kg-1·30d-1),导致了土壤中NH4+-N的积累。     

覆盖对烟田土壤酶活性及烤烟叶片荧光特性的影响

通过对烤烟大田3种不同覆盖方式的覆盖效应比较表明:覆盖明显增强了土壤过氧化氢酶和蔗糖酶活性,对脲酶活性有一定抑制作用;在烤烟生长前期,液膜覆盖处理土壤过氧化氢酶活性较对照和地膜覆盖处理分别平均提高5.72%、23.19%,且覆盖处理间差异达0.05显著水平;覆盖处理的蔗糖酶较对照平均提高0.8%,但3个处理间差异均不显...     

优化施肥对春小麦产量、氮素利用及氮平衡的影响

2009 ～ 2010年,在宁夏引黄灌区分别以宁春11号和宁春16号小麦为供试作物,利用田间试验研究了优化施肥(OPT)和习惯施肥(CON)对春小麦产量、氮素吸收利用和土壤硝态氮累积的影响,表观评估了土壤—小麦体系氮素平衡.结果表明,相对于CK处理,OPT和CON都显著提高春小麦籽粒产量地上部生物量,并促进籽粒N和地上...     

Integrating multiple electromagnetic data to map spatiotemporal variability of soil salinity in Kairouan region,Central Tunisia

Soil salinization is a major problem affecting soils and threatening agricultural sustainability in arid and semi-arid regions,which makes it necessary to establish an efficient strategy to manage soil salinity and confront economic challenges that arise from it.Saline soil recovery involving drainage of shallow saline groundwater and the removal of soil salts by natural rainfall or by irrigation are good strategies for the reclamation of salty soil.To develop suitable management strategies for salty soil reclamation,it is essential to improve soil salinity assessment pro cess/mechanism and to adopt new approaches and techniques.T his study mapped a recovered area of 7200 m2 to assess and verify variations in soil salinity in space and time in K airouan region in Central Tunisia,taking into account the thickness of soil materials.Two electromagnetic conductivity meters(EM38 and EM31)were used to measure the electrical conductivity of saturated soil-paste extract(ECe)and apparent electrical conductivity(E Ca).Multiple linear regression was established between ECe and ECa,and it was revealed that ECa-EM38 is optimal for E Ce prediction in the surface soils.Salinity maps demonstrated that the spatial structure of soil salinity in the region of interest was relatively unchanged but varied temporally.Variation in salinity at the soil surface was greater than that at a depth.These findings can not only be used to track soil salinity variations and their significance in the field but also help to identify the spatial and temporal features of soil salinity,thus improving the efficiency of soil management.     

干旱区农田土壤水分地温变化规律及其相互关系

以干旱区农田灌溉后土壤水分、地温实测数据为基础,研究了其土壤水分、地温各自的变化规律及两者的相互关系.结果表明,各层含水量之间具有高相关性,基本达到了极显著的水平.这与土壤水分灌溉时由上而下的逐渐下渗,以及蒸发时由下而上的逐层上升有密切的关系.各层地温间的相关性大,除地面温度外,其余各层地温间的相关水平为显著或极显著水平,且相邻土层地温间均呈极显著相关.土壤水分及地温剖面垂直变化特征明显,并具有动态性.土壤水分含量大时,两者的垂直变异系数小,反之变异系数大.0～20 cm、地面(0 cm)分别为剖面含水量及地温变异强度的最大层,属中等变异强度.土壤水分及温度之间的负相关性明显.地面温度是预测表层、底层土壤水分的良好指标,利用回归分析法建立的土壤水分与地温间的函数关系可为推测土壤水分提供依据.