供水及间甲酚对小麦间作蚕豆土壤微生物多样性和酶活性的影响

通过盆栽试验,探讨供水(田间持水量的45%、60%和75%)和化感物质间甲酚对小麦、蚕豆不同种植模式生长盛期土壤微生物多样性和酶活性的影响.结果表明,随灌水水平的降低,不同处理的土壤细菌、真菌和放线菌数量随之减少,间甲酚可加剧灌水减少引起的微生物数量的减少;间甲酚对不同处理土壤微生物多样性指数均具有降低作用,提高灌水水平可缓解间甲酚对间作群体土壤微生物多样性的负效应,但间甲酚在75%灌水水平下对单作微生物多样性的负效应最大,45%的供水水平和间甲酚作用下间作可维持更高的土壤微生物多样性.间甲酚对土壤过氧化氢酶的化感作用不显著,对脲酶和酸性磷酸酶活性的化感作用显著;3种土壤酶活性随供水水平的降低均显著下降,但供水与间甲酚、种植模式的互作效应对酶活性的影响不显著;间作对土壤过氧化氢酶和酸性磷酸酶活性具有极显著影响.     

间作减轻蚕豆枯萎病的微生物和生理机制

通过田间小区试验,研究了小麦与蚕豆间作对蚕豆枯萎病发病率、病情指数、根际镰刀菌数量、蚕豆根系抗氧化酶活性和膜质过氧化的影响.采用Biolog ECO板分析了根际土壤微生物的代谢功能多样性,通过高效液相色谱(HPLC)测定了蚕豆根际土壤中酚酸含量.结果表明: 与单作蚕豆相比,小麦与蚕豆间作有降低蚕豆枯萎病发病率的趋势;发病盛期和发病末期,间作使蚕豆枯萎病的病情指数比单作显著降低15.8%和22.8%,明显提高了蚕豆根际微生物活性(AWCD值),根际微生物的Shannon多样性指数显著提高4.4%和5.3%,丰富度指数显著提高19.4%和37.1%.主成分分析表明,发病盛期和发病末期,间作明显改变了蚕豆根际微生物的群落结构,蚕豆根际镰刀菌数量分别降低53.8%和33.1%;并显著降低了蚕豆根际土壤中对羟基苯甲酸、香草酸、丁香酸、阿魏酸、苯甲酸和肉桂酸的含量.发病盛期和发病末期,间作蚕豆根系的过氧化物酶(POD)和过氧化氢酶(CAT)活性分别显著提高了20.0%、31.3%和38.5%、66.7%,丙二醛(MDA)含量显著降低36.3%和46.3%;发病初期间作对蚕豆根系的POD、CAT酶活性和MDA含量无显著影响.小麦与蚕豆间作显著提高了蚕豆根际微生物的活性、多样性和根系抗氧化酶活性,降低了蚕豆根际土壤中酚酸含量和膜质过氧化程度,减少了土壤镰刀菌的数量,从而提高了蚕豆对枯萎病的抗性,降低了枯萎病的危害程度.     

间作缓解蚕豆连作障碍的根际微生态效应

通过田间小区试验,研究了3个品种蚕豆(92-24、云豆324、凤豆6号)与小麦间作对蚕豆产量、枯萎病病情指数、根际镰刀菌数量、根际真菌代谢功能多样性和土壤酶活性的影响。结果表明:与单作蚕豆相比,云豆324与小麦间作(YD324/W)和凤豆6号与小麦间作(FD6/W)处理均显著提高了蚕豆地上部干重、籽粒产量和百粒重。YD324/W和FD6/W处理使蚕豆枯萎病发病初期病情指数分别降低57.14%和41.67%,镰刀菌数量分别降低32.06%和29.88%,而92-24与小麦间作(92-24/W)处理蚕豆产量、枯萎病病情指数和镰刀菌数量与单作蚕豆均无显著差异。YD324/W和FD6/W处理显著提高了蚕豆根际真菌的多样性指数和丰富度指数,并使蚕豆根际真菌的AWCD值分别比单作蚕豆提高了61.75%和46.49%;YD324/W和FD6/W处理明显改变了蚕豆根际真菌的群落结构。而92-24/W处理对蚕豆根际真菌的多样性指数、丰富度指数和AWCD值均无显著影响,也未明显改变真菌的群落结构。不同发病时期,YD324/W和FD6/W处理均显著提高了蚕豆根际土壤的蔗糖酶、脲酶和过氧化氢酶活性;而92-24/W处理蚕豆根际蔗糖酶、脲酶和过氧化氢酶活性与单作蚕豆均无显著差异。总之,小麦与不同品种蚕豆间作改变了蚕豆根际的真菌群落结构,提高了蚕豆根际真菌的活性、多样性和丰富度,提高土壤酶活性并改善蚕豆生长,增加了蚕豆产量。表明小麦与蚕豆间作改善了根际土壤的微生态环境,降低了镰刀菌的数量,缓解了蚕豆连作障碍,但蚕豆品种的差异影响间作控病效果。     

木薯/花生间作对根际土壤微生态的影响

为了探明木薯/花生间作在增产增收的同时对土壤微生态的影响,研究木薯和花生以不同行距(30 cm,40 cm,50 cm)间作的根际土壤养分、微生物及相关酶活性的变化。结果表明:木薯/花生间作可增加根际土壤细菌、真菌、放线菌及总微生物数量和微生物多样性,30 cm间作行距的木薯、花生根际土壤微生物总数量分别比单作木薯、花生增加了129.6%和101.1%;间作根际土壤碱解氮、有效磷、有效钾和有机质含量相比单作增加,50 cm间作花生的根际土壤碱解氮、有效磷、有效钾量比单作花生增加了145.9%~195.9%,30 cm间作木薯的根际土壤有效钾、有效磷含量分别比单作木薯增加了161.8%和187.9%;木薯/花生间作的根际土壤过氧化氢酶、酸性磷酸酶活性活性相比单作升高,间作土壤脲酶和蛋白酶活性相比单作降低,30 cm间作木薯的根际土壤过氧化氢酶活性比单作木薯增加了59.2%,50 cm间作花生的根际土壤蔗糖酶活性比单作花生增加了97.4%。可见,木薯/花生间作可改善根际土壤微生态坏境,且适宜的间作行距更利于土壤养分含量和微生物数量的增加。     

小麦-蚕豆间作条件下氮肥施用量对根际微生物区系的影响

通过田间小区试验,研究了小麦/蚕豆间作条件下4种施氮水平(0、90、180和270 kg·hm^-2)对根际微生物区系和多样性的影响.结果表明：在整个生育期,微生物数量有一定的波动,但均以开花期数量最高.与单作相比,间作显著增加了小麦和蚕豆根际的细菌、真菌、放线菌数量和微生物总量,而显著降低了开花期和成熟期蚕豆根际的微生物多样性.在不施氮（N₀）和低氮（N₉₀）水平下,间作与单作在微生物数量上的差异较大.间作对土壤微生物数量的促进效应在分蘖期和开花期最大,成熟期显著降低.小麦根际的微生物数量随施氮量的增加先增加后降低,以常规施氮处理（N₁₈₀）的微生物数量最多,氮肥用量对单作小麦的影响大于间作小麦. 施氮量对蚕豆根际细菌、真菌、放线菌数量和微生物多样性无显著影响,但降低了间作蚕豆根际微生物总量.适量施用氮肥能有效调节根际微生物区系,间作系统地上部植物多样性与地下部微生物区系间存在紧密联系.     

栽植生姜对不同种植模式下紫色土微生物生物量及水解酶活性的影响

研究了岷江下游紫色丘陵区玉米+红薯间作、大豆单作、生姜连作、水稻-紫云英轮作等4个典型种植模式下栽植生姜后土壤微生物生物量碳、氮、磷含量和水解酶活性的变化特征.结果表明： 栽植生姜显著降低了4个种植模式下土壤微生物生物量碳、氮和磷含量,但各种植模式之间存在较大差异.其中,玉米+红薯间作和水稻-紫云英轮作模式下土壤微生物生物量碳、氮的下降幅度明显低于大豆单作与生姜连作模式,但土壤微生物生物量磷下降幅度明显较高.栽植生姜显著降低了土壤酸性磷酸酶活性,其下降幅度以玉米+红薯间作模式最大,水稻-紫云英轮作模式最小;土壤转化酶活性在生姜连作模式下显著降低;土壤脲酶活性在大豆单作、生姜连作和水稻-紫云英轮作模式下均显著降低.相对于其他模式,栽植生姜使玉米+红薯间作模式下的土壤维持了较高的转化酶和脲酶活性.     

小麦与蚕豆间作体系根系形态与磷吸收的定量解析

豆科与禾本科作物间作能够改变作物根系生长,但不同施磷水平下间作-根系形态-磷吸收之间的关系尚未明确。本研究通过田间定位试验和根箱模拟试验,研究不同种植模式(小麦单作、蚕豆单作和小麦-蚕豆间作)和不同磷水平下小麦和蚕豆的产量、生物量、磷吸收及根系形态特征,分析探讨不同施磷条件下小麦-蚕豆间作对根系形态和磷吸收的影响。结果表明: 根箱试验中,与单作相比,间作小麦的根干重、根冠比分别增加21.2%、61.5%,地上部干重降低14.6%,根系磷含量和总吸磷量分别提高23.8%和12.1%;间作蚕豆的地上部干重、根干重、根冠比、总根长和根体积分别增加16.5%、47.3%、24.0%、3.5%和8.4%,间作蚕豆地上部磷含量、根系磷含量和总吸磷量分别提高14.7%、26.2%和21.5%。田间试验中,与单作相比,分蘖期间作小麦地上部磷吸收量降低8.7%,而在拔节期、抽穗期、灌浆期和成熟期分别提高40.6%、19.7%、7.8%和12.4%;但种间互作导致开花期、结荚期和成熟期间作蚕豆的地上部磷吸收量分别降低9.8%、9.0%和5.2%。偏最小二乘法(PLS)回归分析表明,小麦的根表面积和根体积、蚕豆的根表面积对作物磷吸收的贡献最大,在低磷胁迫条件下,间作同时提高了小麦和蚕豆的根体积和根表面积,促进了磷的吸收。总之,在缺磷或低磷条件下,种间互作扩大了小麦和蚕豆根土接触面积,促进了苗期磷的吸收,为后期间作优势的形成奠定了基础。     

栽植生姜对不同种植模式下紫色土微生物生物量及水解酶活性的影响

研究了岷江下游紫色丘陵区玉米+红薯间作、大豆单作、生姜连作、水稻-紫云英轮作等4个典型种植模式下栽植生姜后土壤微生物生物量碳、氮、磷含量和水解酶活性的变化特征.结果表明： 栽植生姜显著降低了4个种植模式下土壤微生物生物量碳、氮和磷含量,但各种植模式之间存在较大差异.其中,玉米+红薯间作和水稻-紫云英轮作模式下土壤微生物生物量碳、氮的下降幅度明显低于大豆单作与生姜连作模式,但土壤微生物生物量磷下降幅度明显较高.栽植生姜显著降低了土壤酸性磷酸酶活性,其下降幅度以玉米+红薯间作模式最大,水稻-紫云英轮作模式最小;土壤转化酶活性在生姜连作模式下显著降低;土壤脲酶活性在大豆单作、生姜连作和水稻-紫云英轮作模式下均显著降低.相对于其他模式,栽植生姜使玉米+红薯间作模式下的土壤维持了较高的转化酶和脲酶活性.     

施氮对间作蚕豆根际微生物区系和枯萎病发生的影响

通过田间小区试验,研究了小麦、蚕豆间作条件下4个施氮水平(0,56.25,112.5kg.hm-2和168.75kg.hm-2)对蚕豆根际微生物区系和蚕豆枯萎病发生的影响。结果表明,单作和间作条件下,施氮显著增加了蚕豆根际的微生物数量,在N2(112.5kg.hm-2)水平下达到最高值;施氮对土壤微生物多样性无显著影响,但减轻了单、间作蚕豆枯萎病的发生,且在N2水平下发病最轻。与单作相比,间作显著增加了蚕豆根际的细菌、真菌、放线菌数量、微生物总数和微生物多样性,尤其在N0、N1(56.25kg.hm-2)和N2(112.5kg.hm-2)水平下间作对蚕豆根际微生物的促进效应明显,且以真菌和放线菌的增幅较大.N0、N1和N2水平下间作显著降低了蚕豆枯萎病的发病率和病情指数。小麦蚕豆间作下适量施氮能有效调节蚕豆根际微生物区系,是抑制蚕豆枯萎病发生的有效措施。     

小麦蚕豆间作对蚕豆根际微生物群落功能多样性的影响及其与蚕豆枯萎病发生的关系

通过田间小区试验,研究了小麦与蚕豆间作对蚕豆枯萎病发生和根际微生物代谢功能多样性的影响。结果表明,小麦与蚕豆间作使蚕豆枯萎病的发病率和病情指数分别比单作显著降低20%和30.4%。与单作处理相比,间作显著增加了蚕豆和小麦根际微生物对31种碳源的平均利用率（AWCD）,其中间作蚕豆的AWCD值最高,比单作增加82.7%,单作蚕豆最低。间作蚕豆和间作小麦根际微生物的Shannon多样性指数与丰富度指数均显著高于单作,间作使蚕豆和小麦的丰富度指数分别增加29.2%和30.3%。根际微生物对六类碳源的利用强度百分比以糖类、羧酸类和氨基酸最高,分别为41.96%,19.80%和18.13%。主成分分析表明,小麦与蚕豆间作改变了根际微生物的群落组成;相关分析表明,糖类、羧酸类和氨基酸类碳源是区分单间作处理差异的主要碳源,其中氨基酸类碳源是最敏感的碳源。小麦与蚕豆间作增加了根际微生物活性,提高了Shannon多样性指数和丰富度指数,改变了微生物群落功能多样性,是抑制蚕豆枯萎病的有效措施。该研究为阐明根际微生物功能多样性变化在间作体系病害控制中的作用与机制奠定了理论基础。     

Trajectories of change: riparian vegetation and soil conditions following livestock removal and replanting

Riparian zones provide critically important ecological functions, including the interception of nutrients and sediments before they enter waterways. Consequently, riparian zones, and the vegetation they support, are often considered as an important ‘final buffer’ between waterways and adjacent land. In agricultural ecosystems, riparian zones are therefore increasingly recognized as an important component of strategies aimed at minimizing the flow of nutrients and sediments into waterways. Accordingly, riparian zones are increasingly afforded protection and are targeted for restoration. Here we present results of a study in which we aimed to identify patterns of change in soil and vegetation properties in riparian zones, under different management regimes, adjacent to tributary streams in one of south‐eastern Australia's main agricultural regions. We compared riparia that were heavily impacted by agricultural activities, were in remnant condition or had undergone some restoration activities and were thus in a transitional state. There was an increase in plant cover and soil C concentration between impacted through to remnant sites, with transitional sites intermediate, suggesting that improvements in soil conditions were becoming evident following restoration activities. In our assessment of soil physicochemical properties we investigated the relationships between riparian condition and soil properties, taking into account the influence of adjacent land use on these relationships. Importantly, the concentrations of NO₃^‐ and plant available P in riparian surface soils were more or less influenced by concentrations in the adjacent land depending upon riparian condition. This will, in turn, have consequences for nutrient inputs into streams. This study emphasizes that riparian zones need to be managed within their wider landscape context. Furthermore, the results of this study will inform efforts seeking to minimize impacts of agricultural activities on waterways, through the conservation and/or restoration of riparian ecosystems.     

土壤微生物资源管理、应用技术与学科展望

土壤中蕴藏着高度的微生物多样性,在陆地生态系统中发挥着非常重要的功能,加强对土壤微生物资源的综合管理与开发应用是提升生态系统稳定性与生产力及农产品质量的重要途径。首先,土壤微生物多样性具有全球性的重大意义,有待完善对土壤微生物的检测与监测技术研究,进而实现土壤微生物多样性与土壤功能的耦合以及对土壤质量的评定;其次,土壤微生物作为一种宝贵的生产资料和可持续资源,要加强其在土壤肥力强化与保育、土壤障碍消减与调节、土壤污染控制与修复等3个领域的应用研究。最后,未来土壤微生物学发展将会形成土壤微生物系统学、土壤微生物过程学与土壤微生物功能学3个子学科,要建立土壤微生物种质资源库与遗传信息库,推进土壤微生物生理代谢过程、生物化学过程及生态行为过程的研究,联结土壤微生物与土壤功能的关系,并从土壤中的功能微生物出发对环境变化作出积极响应和主动调控。此外,原创性方法的建立与应用是限制土壤微生物学发展的技术瓶颈,联合生物地理学与生物信息学破译重要基因的特定生态功能,并将其应用到生态模型以及生态系统未知领域的研究中去,是土壤微生物学面临的挑战。     

不同地表覆盖方式对苹果园土壤性状及果树生长和产量的影响

以黄土高原9年生红富士果园生态系统为对象,研究不同地表覆盖模式（清耕、生草覆盖、地膜覆盖、秸秆覆盖和砂石覆盖）对果园土壤性状及果树生长和产量的影响.结果表明：生草覆盖土壤水分剖面分异最低,砂石覆盖土壤水分剖面分异最高;砂石覆盖提高了根层水分含量,有利于果树对水分的利用.不同地表覆盖模式土壤热量状况变化显著,处理间差异明显,极端最高温度下降,但地膜覆盖处理夏季地温超过果树根系生长的上限温度,对果树根系生长和生理功能发挥不利.除地膜覆盖外,其他地表覆盖模式均能提高土壤CO₂释放速率,其中生草覆盖的效果最为显著.不同地表覆盖模式对果树枝条类型比例及产量影响较大,砂石覆盖处理的中短枝比例和果实产量最高;生草覆盖处理的果实产量最低.因子分析结果表明,对于黄土高原沟壑区盛果期果园,砂石覆盖处理是较为适宜的地表覆盖模式.     

辣椒茎、叶对酸化土壤交换性能及土壤酶活性的影响

采用辣椒秸秆废弃物与酸化土壤共培养的方法, 设计了不同添加量的辣椒茎、叶与酸化土壤充分混合、共培养, 测定了土壤交换性离子及土壤酶活性的变化, 探讨辣椒茎、叶对酸化土壤交换性能及土壤酶活性的影响。结果表明, 辣椒茎、叶可以改善酸化土壤pH, 降低酸化土壤交换性酸含量; 添加辣椒茎、叶可提高土壤NH4+-N含量, 影响土壤NO3--N转化; 添加辣椒茎、叶可提高土壤交换性盐基含量、CEC及盐基饱和度, 尤其以添加辣椒叶5%的效果最好; 辣椒茎、叶可以提高土壤脲酶活性, 但培养60 d后各处理土壤过氧化氢酶、蔗糖酶、酸性磷酸酶活性无显著性差异; 添加辣椒茎、叶能提高土壤酶的几何平均数, 改善酸化土壤质量, 其对酸化土壤质量的改变与辣椒茎、叶的添加量有关。研究结论可为开拓辣椒秸秆利用途径、改善土壤酸度, 提高土壤肥力等方面提供理论依据。     

Soil and total ecosystem respiration in agricultural fields: effect of soil and crop type

A study was made of the effect of soil and crop type on the soil and total ecosystem respiration rates in agricultural soils in southern Finland. The main interest was to compare the soil respiration rates in peat and two different mineral soils growing barley, grass and potato. Respiration measurements were conducted during the growing season with (1) a closed-dynamic ecosystem respiration chamber, in which combined plant and soil respiration was measured and (2) a closed-dynamic soil respiration chamber which measured only the soil and root-derived respiration. A semi-empirical model including separate functions for the soil and plant respiration components was used for the total ecosystem respiration (TER), and the resulting soil respiration parameters for different soil and crop types were compared. Both methods showed that the soil respiration in the peat soil was 2–3 times as high as that in the mineral soils, varying from 0.11 to 0.36 mg (CO₂) m^–2 s^–1 in the peat soil and from 0.02 to 0.17 mg (CO₂) m^–2 s^–1 in the mineral soils. The difference between the soil types was mainly attributed to the soil organic C content, which in the uppermost 20 cm of the peat soil was 24 kg m^–2, being about 4 times as high as that in the mineral soils. Depending on the measurement method, the soil respiration in the sandy soil was slightly higher than or similar to that in the clay soil. In each soil type, the soil respiration was highest on the grass plots. Higher soil respiration parameter values (R_s0, describing the soil respiration at a soil temperature of 10°C, and obtained by modelling) were found on the barley than on the potato plots. The difference was explained by the different cultivation history of the plots, as the potato plots had lain fallow during the preceding summer. The total ecosystem respiration followed the seasonal evolution in the leaf area and measured photosynthetic flux rates. The 2–3-fold peat soil respiration term as compared to mineral soil indicates that the cultivated peat soil ecosystem is a strong net CO₂ source.     

Concept,Components, and Strategies of Soil Health in Agroecosystems

The terms ''''soil health'''' or ''''soil quality'''' as applied to agroecosystems refer to the ability of soil to support and sustain crop growth while maintaining environmental quality. High-quality soils have the following characteristics: (i) a sufficient, but not excess, supply of nutrients; (ii) good structure (tilth); (iii) sufficient depth for rooting and drainage; (iv) good internal drainage; (v) low populations of plant disease and parasitic organisms; (vi) high populations of organisms that promote plant growth; (vii) low weed pressure; (viii) no chemicals that might harm the plant; (ix) resistance to being degraded; and (x) resilience following an episode of degradation. Management intended to improve soil health involves creatively combining a number of practices that enhance the soil''s biological, chemical, and physical suitability for crop production. The most important general strategy is to add plentiful quantities of organic matter—including crop and cover crop residues, manures, and composts. Other important strategies include better crop rotations, reducing tillage and keeping the soil surface covered with living and dead residue, reducing compaction by decreasing heavy equipment traffic, and using best nutrient management practices. Practices that enhance soil quality frequently reduce plant pest pressures.     

Soil Erosion Impact on Agronomic Productivity and Environment Quality

Soil erosion is a global issue because of its severe adverse economic and environmental impacts. Economic impacts on productivity may be due to direct effects on crops/plants on-site and off-site, and environmental consequences are primarily off-site due either to pollution of natural waters or adverse effects on air quality due to dust and emissions of radiatively active gases. Off-site economic effects of erosion are related to the damage to civil structure, siltation of water ways and reservoirs, and additional costs involved in water treatment. There are numerous reports regarding the on-site effects of erosion on productivity. However, a vast majority of these are from the U.S., Canada, Australia, and Europe, and only a few from soils of the tropics and subtropics. On-site effects of erosion on agronomic productivity are assessed with a wide range of methods, which can be broadly grouped into three categories: agronomic/soil quality evaluation, economic assessment, and knowledge surveys. Agronomic methods involve greenhouse and field experiments to assess erosion-induced changes in soil quality in relation to productivity. A widely used technique is to establish field plots on the same soil series but with different severity of past erosion. Different erosional phases must be located on the same landscape position. Impact of past erosion on productivity can also be assessed by relating plant growth to the depth of a root-restrictive horizon. Impact of current erosion rate on productivity can be assessed using field runoff plots or paired watersheds, and that of future erosion using topsoil removal and addition technique. Economic evaluation of the on-site impact involves assessment of the losses of plant available water and nutrients and other additional inputs needed due to erosion. Knowledge surveys are conducted as a qualitative substitute for locations where quantitative data are not available. Results obtained from these different techniques are not comparable, and there is a need to standardize the methods and develop scaling procedures to extrapolate the data from plot or soil level to regional and global scale. There is also a need to assess on-site impact of erosion in relation to soil loss tolerance, soil life, soil resilience or ease of restoration, and soil management options for sustainable use of soil and water resources. Restoration of degraded soils is a high global priority. If about 1.5×10⁹?ha of soils in the world prone to erosion can be managed to effectively control soil erosion, it would improve air and water quality, sequester C in the pedosphere at the rate of about 1.5?Pg/year, and increase food production. The risks of global annual loss of food production due to accelerated erosion may be as high as 190×10⁶?Mg of cereals, 6×10⁶?Mg of soybeans, 3×10⁶?Mg of pulses, and 73×10⁶?Mg of roots and tubers. The actual loss may depend on weather conditions during the growing season, farming systems, soil management, and soil ameliorative input used. Erosion-caused losses of food production are most severe in Asia, Sub-Saharan Africa, and elsewhere in the tropics rather than in other regions.     

晋西北不同土地管理方式对土壤碳氮、酶活性及微生物的影响

晋西北丘陵区受干旱大风气候以及人为活动的影响,土壤肥力较低,土壤质量退化严重,不同的土地利用和管理方式,因植被覆被、人为活动等不同,对土壤质量产生影响不同。为了更好地了解晋西北地区不同土地管理方式对土壤质量的影响,于山西省北部忻州市五寨县,研究不同管理方式对土壤肥力、土壤酶活性、微生物群落结构及多样性的影响,以及微生物与土壤环境因子的关系,为晋西北地区土地管理和生态建设提供参考。研究中设置4种土地管理方式:苜蓿样地(MX)、免耕样地(MG)、翻耕样地(FG)和荒地(HD),采用野外采集土壤样品、室内测定和分析的研究方法,其中土壤pH值利用电位法测定,土壤有机碳(OC)采用重铬酸钾氧化-分光光度法测定;土壤硝态氮、铵态氮利用全自动间断化学分析仪测定,其原理为紫外分光光度和靛酚蓝比色法。土壤过氧化氢酶、蔗糖酶、脲酶和磷酸酶活性分别采用KMnO_4滴定法、3,5-二硝基水杨酸法、苯酚钠-次氯酸钠比色法、磷酸苯二钠比色法测定,采用高通量测序测定土壤细菌和真菌的群落组成,利用统计分析软件SPSS和Canoco以及QIIME、USEARCH和Uclust生物信息软件分析不同土地管理方式对土壤质量的影响。结果表明,不同土地管理方式对土壤化学性质、土壤酶活性、细菌和真菌的群落结构及多样性均有影响。苜蓿和免耕2种土地管理方式可显著提高表层土壤养分并增加土壤酶活性;4种土地管理方式共有9个细菌门和11个真菌门,细菌相对丰度较大的为变形菌门、放线菌门和酸杆菌门,真菌的子囊菌门相对丰度最大;苜蓿和免耕样地土壤细菌和真菌群落丰富度和多样性都较高,荒地土壤细菌和真菌群落丰富度较低,但多样性较高;RDA分析结果表明,土壤pH、NH~+_4-N和NO~-_3-N含量和过氧化氢酶活性对细菌群落影响较大,pH、有机碳含量、蔗糖酶、脲酶和过氧化氢酶活性对真菌群落影响最大。苜蓿和免耕2种土地管理方式能够提高土壤质量,是晋西北地区较为适宜的管理措施。     

渭北旱塬苹果园土壤紧实化现状及成因

本研究通过分析渭北旱塬苹果园土壤的紧实化现状及其诱导因素,找出影响当地苹果园健康发展的土壤退化隐性因素,为果园科学管理提供理论依据。分别选取种植年限＜10年(4～6年)、10～20年(14～16年)和＞20年(24～26年)的苹果园各4个,分析0～60 cm土层土壤容重和紧实度随土层深度的变化规律,探明果园土壤内部紧实化发生的部位和退化程度,同时,通过分析土壤团聚体数量及其稳定性、土壤黏粒和有机质含量,揭示引起渭北果园土壤内部紧实化的原因。结果表明: 渭北果园0～60 cm土层土壤容重和紧实度均随植果年限和土层深度的增加而显著增大。以20 cm土层为界,渭北各园龄段苹果园土壤具有明显的“上松下实”变异特征,20 cm以上土层上述各指标基本满足苹果树的正常生长需求,20 cm以下土层土壤则已超出了苹果树健康生长的阈值。造成渭北苹果园亚表层以下土壤紧实化的原因主要是土壤团聚作用差、有机质含量低,加之植果期间人为扰动少,土壤中分散的黏粒会向下层移动。此外,随着植果年限的增加,土壤紧实化过程更加明显。     

落叶松林土壤溶液吸光度与土壤碳、氮含量的相关性

通过4个土壤深度100个样品14个波长(250、254、260、265、272、280、285、300、340、350、365、400、436和465 nm)土壤溶液吸光度值和土壤碳(可溶性碳DOC、全碳SOC)、土壤氮(可溶性氮DON、全氮SON)的测定,旨在探讨土壤溶液吸光度指示土壤碳氮指标的可行性及土壤深度对其可能影响。结论如下:(1)表层土壤和深层土壤吸光度值均随波长增加而指数下降,但表层土壤吸光度值较高,下降速度较快,较低波长更有利于区分表层和深层土壤溶液吸光度差异;和深层土壤相比,表层0～20 cm土壤SOC、DON和SON与不同波长吸光度有更好的相关性,但DOC与不同波长吸光度的相关性表层和深层差异较小;(2)250～300 nm的8个吸光度值具有高度相关性,它们在分析土壤溶液吸光度变化时具有等效性;基于所有数据的拟合分析发现,低波长(如254 nm)吸光度与土壤SOC、DON和SON相关性最高(R2=0.53～0.59),而更高波长(340 nm及以上)相关性明显降低。但DOC与254、340、365和400 nm吸光度相关性相差不大(R2=0.25～0.33)。这些发现说明,土壤溶液吸光度值,特别是低波长(250～300 nm)可以表征落叶松林土壤碳、氮相关指标的变化,但是需要考虑不同碳氮指标以及不同土层之间的差异。