水分优化对温室葡萄产量及土壤生物学特性的影响

为揭示滴灌不同水分调控下设施栽培葡萄产量与土壤学特性等相关指标的响应关系,在甘肃省永登县设施葡萄试验基地开展葡萄滴灌不同生育期水分调控田间灌溉试验,分析水分调控对设施栽培葡萄土壤积温、蔗糖酶和淀粉酶活性、有机碳(TOC)、微生物量碳(MBC)和微生物熵(qMB)等土壤学特性的影响,基于隶属函数综合分析明确影响葡萄产量及各项土壤生物学特性指标的最佳水分优化处理。结果表明:新梢期水分胁迫的土壤积温、土壤酶、TOC、MBC、qMB均显著(P <0. 05)高于对照;新梢期水分胁迫较对照可增产44. 6%;果实膨大期作为葡萄生长的关键阶段,此时水分胁迫对土壤淀粉酶影响不显著,但对其他土壤学特性指标具有一定的抑制作用,并且可减产9.7%;隶属函数综合分析表明,土壤生物学特性指标及产量综合隶属排名为:PS﹥FS﹥CS﹥CK﹥ES。     

Responses of plant community to the linkages in plant-soil C:N:P stoichiometry during secondary succession of abandoned farmlands,China

Succession is one of the central themes of ecology;however,the relationship between aboveground plant communities and underground soils during secondary succession remains unclear.In this study,we investigated the composition of plant community,plant-soil C:N:P stoichiometry and their relationships during secondary succession after the abandonment of farmlands for 0,10,20,30,40 and 50 a in China,2016.Results showed that the composition of plant communities was most diverse in the farmlands after secondary succession for 20 and 50 a.Soil organic carbon and total nitrogen contents slightly decreased after secondary succession for 30 a,but both were significantly higher than those of control farmland(31.21%-139.10%and 24.24%-121.21%,respectively).Moreover,C:N ratios of soil and microbe greatly contributed to the changes in plant community composition during secondary succession of abandoned farmlands,explaining 35.70%of the total variation.Particularly,soil C:N ratio was significantly and positively related with the Shannon-Wiener index.This study provides the evidence of synchronous evolution between plant community and soil during secondary succession and C:N ratio is an important linkage between them.     

Effect of organic amendment amount on soil nematode community structure and metabolic footprints in soybean phase of a soybean-maize rotation on Mollisols

It has been well documented that organic amendment affects soil nematode community structure. However, little is known about the effect of organic amendment amount on soil nematodes. To assess the effect of the amount of organic amendments on soil nematode community structure and metabolic activity, the community composition, abundance, and metabolic footprints of soil nematodes were determined in a long-term field experiment with various amounts of organic amendment in Northeast China. Fertilization treatments included an unfertilized control (CK), chemical fertilizer without manure amendment (OM₀), manure applied at 7.5 Mg ha^-1 plus chemical fertilizer (OM₁), and manure applied at 22.5 Mg ha^-1 plus chemical fertilizer (OM₂). A total of 46 nematode genera were found. Treatments with the largest amount of organic amendment had the smallest number of plant parasite genera (5), but a largest number of dominant genera (7). Soil nematodes, bacterivores, and fungivores were the most abundant in OM₂, followed by OM₁, and the lowest in OM₀ and CK. Organic amendment increased the enrichment index (EI), and the large amount of organic amendment increased the metabolic footprints of bacterivore (Baf) and fungivore (Fuf) and enrichment footprint (Ef). The relationships between Baf (or Fuf) and the increases in soil organic carbon (ΔSOC) and total nitrogen (ΔTN) were stronger than those of bacterivore (or fungivore) abundance with ΔSOC and ΔTN, except for the relationship between bacterivore abundance and ΔSOC. The EI and Ef were positively correlated with ΔSOC and ΔTN. These findings suggest that the amount of organic amendment affects soil nematode activity and function at entry levels in soil food web, and that metabolic footprints of soil nematodes may be better indicators than their abundances in assessing their relationships with soil nutrients.     

陕北黄土区退耕还林(草)地土壤质量特征及其对降水的响应

为了解陕北黄土区退耕还林（草）地土壤质量差异特征及其对降水的响应，该文沿370～470 mm的降水梯度，选取了陕西省吴起县境内的王洼子（370～395 mm）、大吉沟（440～445 mm）和白豹（460～470 mm）3个降水梯度区作为研究区，并结合土壤质量指数法，定量评价降水梯度区广泛栽植的刺槐林（Robinia pseudoacacia）、沙棘林（Hippophae rhamnoides）和草地的土壤物理结构、持水性、盐碱度、碳汇指标以及速效养分指标方面的综合得分，明确植被恢复后土壤质量随降水梯度的变化特征。结果表明：1）降水量、植被类型以及二者的交互作用对土壤指标影响显著（P<0.05）。2）在460～470 mm降水量区，刺槐林（0.829）对土壤质量改良效果最好，其次为沙棘林（0.808），二者土壤质量均达到肥沃水平，且差异不显著，草地（0.679）土壤质量指数最低，土壤为较肥沃水平；在440～445 mm降水量区，沙棘林（0.74）对土壤改良效果最好，其次为刺槐林（0.601），二者均达到较肥沃水平，草地（0.479）土壤质量指数最低为中等水平；在370～395 mm降水量区，3种植被类型土壤质量指数由大到小表现为沙棘林（0.744）>刺槐林（0.387）>草地（0.251），沙棘林土壤质量等级为较肥沃、刺槐林和草地为贫瘠水平。3）在370～470 mm降水梯度内，3种植被类型土壤质量综合指数均随着降水量的减少而降低，其中沙棘林土壤质量指数变异性较低（4.1%），刺槐林（30.1%）和草地（37.2%）土壤质量变异性较高。该研究结果可为陕北黄土区370～470 mm降水梯度下的植被恢复与重建等林业生态工程实施提供数据支撑与理论支持。     

培肥措施对复垦土壤微生物碳氮代谢功能多样性的影响

土壤复垦是矿区生态环境恢复和耕地总量平衡及质量提升的根本要求。本研究依托山西襄垣采煤塌陷区复垦定位试验基地，采用Biolog-ECO方法和荧光定量PCR技术，研究了不施肥（CK）、单施化肥（CF）、单施有机肥（M）和有机无机培肥（MCF）4种培肥措施下复垦4年和8年土壤微生物碳代谢功能多样性及氮代谢功能基因丰度的变化特征。结果表明，随复垦年限增加，单施有机肥较其他处理可显著提高复垦土壤微生物的总碳源利用能力；不同处理复垦土壤微生物碳源相对利用率总体表现为氨基酸类>糖类>聚合物类>羧酸类>双亲化合物类>胺类，其中单施有机肥更大程度上提高了羧酸类、氨基酸类和胺类碳源的利用率；复垦年限和培肥措施没有改变复垦土壤微生物优势度指数，但有机无机配施较其他处理可显著提高香浓指数（H′）和Pielou均匀度指数；不同处理复垦土壤氮转化功能基因丰度总体表现为amoA（AOA）> amoA（AOB）>nisS、nirK> nifH，5种功能基因丰度均为以有机无机培肥处理最高，且随复垦时间增加而增加；复垦土壤有机质含量与nirS、nirK、nifH基因丰度以及AWCD值存在显著相关性，相关系数在0.707～0.807，同时5种氮转化功能基因丰度均与玉米产量存在显著或极显著的相关性，相关系数在0.824～0.949。综上所述，单施有机肥可提高土壤有机质含量，进而增强了复垦土壤碳代谢强度，有机无机培肥则更有利于复垦土壤碳氮代谢功能多样性的提升，并促进作物产量形成。     

链霉菌和壳聚糖对淮山土壤微生物活性与群落的影响

为探究链霉菌30702和壳聚糖对淮山土壤微生物活性与群落的影响,采用比色法和滴定法观测土壤酶活性的变化,采用高通量测序技术和Trimmomatic等软件,分析土壤微生物群落中细菌和真菌的发展变化。结果表明,链霉菌、壳聚糖、土壤原始微生物和培养时间等4个因素对淮山土壤的脲酶和过氧化氢酶活性均有显著影响,壳聚糖浓度在0~10.0 g/kg内,土壤酶活性随壳聚糖浓度的增大而提高;随时间的延长,先升再降;壳聚糖与链霉菌之间存在交互效应。链霉菌和壳聚糖能增加淮山土壤细菌的物种丰度,减少细菌的多样性,增加艾德昂菌属（Ideonella）和纤维弧菌（Cellvibrio）等有益菌属的相对丰度,而对真菌的物种丰度和多样性的影响较小,与对照之间的差异不显著,土壤优势菌属为腐质霉属（Humicola）、枝孢属（Cladosporium）、鞘氨醇单胞菌属（Sphingomonas）和uncultured_bacterium_ c_Subgroup_6。其中,链霉菌与2.5 g/kg壳聚糖复合处理的细菌物种丰度最大,细菌多样性最少。     

生物炭对酸化茶园土壤性状和真菌群落结构的影响

为探讨生物炭长期施用对酸化茶园土壤改良和真菌群落结构的影响,分析了按生物炭用量0、2.5、5、10、20、40 t·hm^-2施用5年后的茶园土壤性状和真菌群落结构变化。结果表明,施用生物炭5年后的茶园土壤pH提高了0.16~1.11,可溶性有机碳含量提高了52.6%~92.3%,而铵态氮和硝态氮含量以10 t·hm^-2处理最高。施用生物炭5年后的土壤性质变化,进一步影响了真菌群落结构,表现为Chao指数、ACE指数和Shannon指数随生物炭用量增加呈先增加后降低的趋势;提高生物炭施用量对茶园土壤次要作用的真菌（LDA值<3.50）丰度的增加效果高于优势真菌（LDA值>3.50）的效果,其中被孢霉属、木霉属、毛壳菌属的相对丰度增加,黑盘孢属的相对丰度降低。     

土壤团聚体有机碳研究进展

土壤有机碳是衡量土壤肥力的重要指标,对于促进土壤养分循环、增加养分有效性有重要作用。土壤团聚体是土壤的重要组成部分,是组成土壤结构的最小单元,受到自然因素和人为因素的影响,其形成转化过程与土壤固碳过程息息相关,因而研究团聚体和有机碳的关系及团聚体有机碳影响因素对于土壤结构的改善和土壤质量的提升具有重要意义。本文通过对文献的总结,明晰了土壤团聚体和有机碳的关系,阐述了土壤类型、施肥方式、土地利用和矿区复垦对土壤团聚体有机碳的影响,并从生物质炭的长期定位研究和复垦矿区的土壤修复两方面对土壤团聚体有机碳的研究进行展望,研究结果可为合理的农业生产提供科学依据。