不同有机物料对苏打碱化土有机碳库和化学性质的影响

以内蒙古河套灌区苏打碱化土为研究对象开展田间试验,设置常规施肥(CK)、生物炭+常规施肥(BC)、牛粪+常规施肥(CD)、玉米秸秆+常规施肥(SW)和羊粪+常规施肥(GM)5个处理,研究不同有机物料添加对碱化土壤有机碳(SOC)库和化学性质的影响。分别于2019年和2020年收获季采集0—30 cm耕层土壤,分析不同有机物料添加下SOC及其活性碳组分和主要盐碱指标的变化特征及其相关关系。结果表明:与CK相比,2019年和2020年各有机物料添加处理下SOC平均增幅分别为22.7%和17.2%,土壤有机碳储量(SOCs)平均增幅分别为22.9%和18.2%;4种有机物料均提高了碱化土壤活性有机碳组分含量,其中,CD和GM处理下各活性碳组分含量增幅较其他处理更高;2019年各有机物料添加处理下碳库管理指数(CPMI)较CK提高53.8%~108.3%,2020年提高71.3%~144.1%(P＜0.05),CD和GM对CPMI的提升作用更明显。土壤化学性质方面,2020年各有机物添加处理下pH均显著下降,BC和CD处理下碱化度(ESP)分别显著下降36.9%和29.3%,CD处理下蔗糖酶活性提高36.7%(P＜0.05)。主成分分析(PCA)表明,影响苏打碱化土SOC含量变化的主要因素为活性有机碳组分和ESP。牛粪和羊粪施用对苏打碱化土有机碳库质量提升作用较好,生物炭施用对盐碱化指标改良效果最明显。     

有机合成类土壤改良剂的制备及其对沙化土壤抗蚀性的改良效果

[目的] 探究以玉米芯、腐殖酸为原料制备纤维素基土壤结构改良剂对沙质土壤抗侵蚀性能的改良效果,为区域性水土流失治理工作提供科学参考。 [方法] 选择漆酶(Lac)和木素过氧化物酶(Lip)的单酶类型和双酶协同,设置3个酶活水平,2个玉米芯生物质添加处理,固定腐殖酸用量,通过水溶液聚合法制备纤维素基土壤改良剂。利用红外光谱对酶解产物及改良剂官能团进行表征,基于溶胀特性分析土壤保水持水能力和改良剂的网状特征,基于机械性和水稳性团聚体相关参数分析改良剂对沙质土壤抗蚀性的改良效果。 [结果] ①纤维素基土壤改良剂的吸纯水倍率为纯腐殖酸基改良剂的0.61～4.84倍。添加4 g漆酶(20 U)+木素过氧化物酶(20 U)酶解产物制备的土壤改良剂(LLP_3-4)的吸纯水倍率最高,为66.7 g/g。改良剂溶胀过程符合Schott二级动力学模型。 ②与CK相比,3种酶解方案制备的改良剂(Lac_3-4,Lip_3-4和LLP_3-4)1%添加处理,土壤的饱和持水量提高了20%～60%;LLP_3-4可使机械性大团聚体和水稳性大团聚体(粒径＞0.25 mm)含量分别增加了6倍和14倍,使土壤平均重量直径和几何平均直径分别增加了70.59%和46.67%,分形维数降低了21.36%。 [结论] 双酶预处理方案制备的纤维素基土壤改良剂可显著提升沙化土壤的保水持水能力及抗蚀性能。     

改良剂作用下滨海盐化潮土团聚体分布、稳定性及有机碳分布特征

通过对滨海盐化潮土小麦—玉米轮作2年田间定位试验,研究不同改良剂施用对土壤团聚体分布、稳定性及土壤团聚体中有机碳含量、各级团聚体有机碳对总有机碳贡献率的影响。试验共设置3个处理:对照(CK)、有机土壤改良剂(OSA)和有机—无机土壤改良剂(CSA),分析土壤团聚体分布、水稳性大团聚体(R_(0.25))、平均重量直径(mean weight diameter,MWD)、几何平均直径(geometric mean diameter,GMD)、分形维数(D)、有机碳储量(soil organic carbon storage,SOCS)和有机碳贡献率(contribution rate of organic carbon)。结果表明,滨海盐化潮土水稳性团聚体组成主要以0.25 mm粒径为主,改良剂施用后土壤R_(0.25)显著提高,其影响主要集中在5 mm和2～5 mm粒径级,OSA处理2个粒级团聚体含量较CK分别显著增加167.38%和59.00%,CSA处理分别显著增加89.17%和100.66%。施用OSA与CSA同时显著提高了土壤团聚体MWD和GMD值,说明2种改良剂的施用均有利于提高大团聚体数量及稳定性。施用改良剂2年处理土壤各粒级团聚体中有机碳含量均有所提高,OSA处理以1～2 mm粒级提高最多,CSA以2～5 mm粒级提高最多,且前者达显著水平。与CK相比,改良剂可促使土壤有机碳向大团聚体富集,显著提高1～2 mm粒级团聚体对土壤总有机碳的贡献率93.62%～109.76%,降低或显著降低1～2 mm粒级团聚体对土壤总有机碳的贡献率20.55%～24.92%。在小麦—玉米轮作模式下,改良剂施用不仅可以显著提高滨海盐化潮土水稳性大团聚体含量和稳定性,还可显著增加水稳性大团聚体有机碳含量与储量,是加强盐碱土壤有机碳库积累的有效措施。     

改良剂对旱地红壤微生物量碳、氮及可溶性有机碳、氮的影响

基于室内模拟培养试验,研究改良剂(生物质炭、过氧化钙)对旱地红壤微生物量碳、氮及可溶性有机碳、氮的影响。试验设置4个处理,即CK、Ca(过氧化钙,1.72g/kg)、C(生物质炭,21.46g/kg)、C+Ca。结果表明:各处理土壤微生物量碳、氮以及可溶性有机碳具有相同的变化趋势,即前期(3d内)都增加较快,在第3天达到最大值,随试验进行有所下降,配施效果优于单施。各处理可溶性有机氮在21d内缓慢增加;第21天时,C+Ca、Ca、C相比CK分别显著增加了62.1%,55.5%,40.9%;35d以后,配施(C+Ca)与单施过氧化钙(Ca)的效果显著优于单施生物质炭(C)和对照(CK)。120d培养期内,配施(C+Ca)处理能够明显提高微生物量碳、氮以及可溶性有机碳、氮的平均含量;微生物量碳的平均含量大小顺序为C+CaCCKCa,微生物量氮的平均含量C+Ca处理显著高于其他处理;可溶性有机碳的平均含量大小顺序为C+CaCaCCK,可溶性有机氮的平均含量C+Ca、Ca处理显著高于CK、C处理。微生物量碳、氮以及可溶性有机碳之间互为极显著正相关(P0.01),而微生物量碳与可溶性有机氮之间呈极显著负相关。因此,生物质炭和过氧化钙能有效提高旱地红壤微生物量碳、氮及可溶性有机碳、氮,且生物质炭与过氧化钙配合施用更有助于土壤改良。     

多功能改土剂对河西地区风沙土理化性质 以及玉米经济效益的影响

采用田间试验方法,研究了多功能改土剂对甘肃省河西地区风沙土理化性质和玉米经济性状及效益的影响。结果表明,影响玉米产量的因素由大到小依次为:牛粪(A)>糠醛渣和保水剂(B)>专用肥>聚乙烯醇。因素间最佳组合是:A1B1C2D3E3﹝牛粪(A)7.82 t,糠醛渣(B)6.00 t,专用肥(C)1.04 t,聚乙烯醇(D)0.09 t,保水剂(E)0.05 t﹞。多功能改土剂施用量与风沙土孔隙度、团粒结构、蓄水量、有机质、速效氮磷钾和土壤电导率(EC)呈正相关,与土壤容重、pH值呈负相关。随着多功能改土剂施用量的增加,边际产量、边际利润在递减,多功能改土剂施用量在15.00 t/hm2的基础上,再增加3.75 t/hm2,收益出现负值。经回归统计分析表明,多功能改土剂最佳施用量为15.00 t/hm2时,玉米的理论产量为7.03 t/hm2,计算结果与田间试验处理5基本吻合。     

不同浓度柠檬酸影响茶园土壤氟释放的动力学研究

为阐明茶树高富集土壤氟的化学机制,采用动力学方法研究了茶树根系分泌柠檬酸对茶园土壤氟形态及其在土壤固一液相分配的影响。结果表明,土壤溶出液的pH和电导率随溶出时间的增加而逐渐减小。土壤氟的释放存在快速释放和慢速释放两个阶段,呈现初始（0～6h）溶出浓度较高,而后（6～10h）逐渐减缓的趋势。一级动力学方程、Elovich方程、扩散方程、双常数方程均对土壤氟的溶出过程有较好的拟合,决定系数（R^2）均大于0．91。土壤溶出液中的游离态氟和总氟的释放量随柠檬酸浓度的升高而增加,反应开始前2h的高浓度柠檬酸溶出液中A1-F络合物的浓度较大,反应开始前1h的A1-F络合物主要以A1F3为主,占氟溶出总量的90％左右;随着溶出时间的延长,A1FI的溶出量逐渐增大,并逐渐超过A1F3。高浓度柠檬酸促进土壤氟的溶出释放,有利于A1-F络合物向AlP、AlE形态转化。     

有机物料对污染土壤上水稻重金属吸收的调控效应

采用重金属污染水稻土开展盆栽试验,研究施用有机碳源、菜籽饼和猪粪对不同水稻(汕优63,简称“SY63”;中浙优1号,简称“ZZY1”)重金属吸收的调控效应.结果表明,在重金属污染土壤上ZZY1具有一定的耐性,相同处理时ZZY1糙米、砻糠、秸秆中重金属含量均低于SY63品种,糙米中Cd含量较SY63低57.5％ ～ 83.8％,Cu含量低37.8％ ～ 69.1％,Zn含量低0.88％ ～ 31.7％,食物链风险较SY63品种低.3种有机物料中,施用菜籽饼使两水稻品种糙米中重金属含量明显低于其他处理;与对照相比,施用菜籽饼使SY63糙米中Cd、Cu和Zn含量降低73.5％、52.6％和32.1％,ZZY1糙米Cd含量降低30.5％.在供试重金属污染土壤上可选择具有一定重金属耐性的水稻品种ZZY1进行粮食生产,同时施用适量的菜籽饼以增强其抵御重金属毒害的能力,降低糙米中Cd、Cu和Zn含量及其食物链污染风险.     

Fertilization Capacity of Aquatic Plants Used as Soil Amendments in the Coastal Sandy Area of Central Vietnam

In Central Vietnam, and more especially in Thua Thien Hue Province, aquatic plants are used empirically by some farmers as an external source of organic matter to improve fertility of sandy soils. The fertilization capacities of aquatic plant species [Najas indica (Willid.) Cham., Najas minor All., Vallisneria spiralis L. (Michx.) Torr., Hydrilla verticillata (L.f.) Royle, Potamogetum malaianus Miq., Myriophyllum spicatum L., Enteromorpha flexuosa (Wulfen) J. Agardh, Rhizoclonium kerneri Stockmayer, and Eichhornia crassipes (Mart) Solms] were assessed from a pot trial including soils amended with aquatic plants (5 g dry matter kg^?1 soil) and soils supplied with increasing rates of urea nitrogen (N) fertilizers. Rice (Oryza sativa L.) at a vegetative stage was used as a convenient bio‐extractor. The fertilization capacity of aquatic plant amendments was calculated from aboveground biomass and from N accumulated in shoots as compared to treatments receiving only inorganic N fertilizers. Najas indica (Willid.) Cham. and Hydrilla verticillata (L.f.) Royle showed the greatest fertilization capacity, equivalent to 170–180 mg urea‐N kg^?1 soil as estimated from biomass yield, whereas a lesser fertilization capacity, equivalent to less than 100 mg urea‐N kg^?1 soil, was observed for Myriophyllum spicatum L., Enteromorpha flexuosa (Wulfen) J. Agardh, Rhizoclonium kerneri Stockmayer, and Eichhornia crassipes (Mart) Solms. This study provides quantitative data on the fertilization capacity of aquatic plants found in the coastal area of central Vietnam, which can improve this empirical practice and alleviate local agro‐environmental constraints related to the lack of organic matter in farming systems.     

Using Organic Matter with Chemical Amendments to Improve Calcareous Sodic Soil

Abstract

Kangping soil in northeast China is a sodic soil characterized by a high pH and excessive sodium. The high pH and excessive sodium in sodic soils generally cause loss of soil structure, reduce hydraulic conductivity (HC), increase soil hardness, and make the soil unproductive land. After we mixed organic matter (rice straw) and chemical amendments (H₂SO₄, CaSO₄, and FeSO₄), a column experiment was conducted to evaluate the physical and chemical properties of the soil influenced by the changes in HC, penetrability of soil s`urface, pH, electrical conductivity, CO₃ ^2‐, HCO₃ ^?, Ca²⁺, Na⁺, sodium adsorption rate (SAR), available phosphorus (P) and iron (Fe), and leached P.

Organic matter decreased the concentrations of CO₃ ^2‐, HCO₃ ^?, and Na⁺ in soil solution and increased the total volume of the leachate. Organic matter also reduced the amount of available Fe and increased the available P. However, organic matter did not affect the penetrability of the soil surface as much as soil hardness, HC, and SAR within the short period of this experiment. Among the chemical amendments, H₂SO₄ and FeSO₄ were more effective than CaSO₄ to restore HC, electrical conductivity, Na⁺, and SAR. The chemical amendments, compared with organic matter, significantly leached P from the soil in this study, but the leaching was independent of the concentration of available P in the soil. The CaSO₄ had the strongest effect in increasing leached P from the soil without changing the concentration of available P in the soil. Organic matter with added CaSO₄ leached P from the soil more than all other treatments.     

Relationship between Soil Temperature and N Release in Organic and Conventionally Managed Vineyards

Soil temperature is a very easily measured parameter that influences nutrient availability in vineyards. We monitored soil temperature and plant-available nitrogen (N) in a study evaluating the potential of legumes as an interrow cover crop to supply N to Concord grape (Vitis labruscana Baily). Nitrogen sources used were hairy vetch (Vicia villosa subsp. villosa L.) and yellow sweet clover [Melilotus officinalis (L.) Lam] as green manure sources and either blood meal (in a certified organic vineyard) or urea (in a conventional vineyard) as soluble sources. Plant-available N was measured both continuously using ion exchange membranes (PRS^TM) and point in time by soil sampling at regular intervals; both were analyzed for nitrate (NO₃) N and ammonium (NH₄) N, although negligible concentrations of NH₄-N were detected. PRS NO₃-N concentration varied by treatments because of differences in the chemical composition of the N source. Soil NO₃-N concentration reached a peak between 520 and 550 degree-days with no significant differences by treatment or site. These findings are similar to results from incubation and field mineralization studies of organic amendments and suggest that N availability from organic sources in vineyards can be predicted using a degree-day-type model.     

有机碳土壤改良剂对风沙土改土效应的影响

[目的]合成有机碳土壤改良剂,为河西内陆灌区制种玉米产业可持续发展提供技术支撑。[方法]选择甘肃省张掖市甘州区的风沙土,采用田间试验方法,进行有机碳土壤改良剂对风沙土改土效应研究。[结果]有机碳土壤改良剂施用量与风沙土孔隙度、团聚体、持水量、有机质、速效养分、微生物数量、酶活性和玉米产量呈正相关关系;与体积质量、pH值呈负相关关系。施用有机碳土壤改良剂与传统化肥比较,风沙土体积质量、pH值、Hg,Cd,Cr和Pb分别降低8.46%,4.87%,17.95%,27.78%,15.75%和18.03%;总孔隙度、团聚体、持水量、有机质、碱解氮、速效磷和速效钾分别增加8.15%,23.98%,8.15%,3.16%,0.10%,2.13%和1.18%;真菌、细菌、放线菌、蔗糖酶、脲酶、磷酸酶和玉米施肥利润分别增加59.18%,41.75%,23.28%,57.09%,13.54%,10.71%和2 180.40元/hm2。[结论]施用有机碳土壤改良剂,能有效地改善风沙土理化性质和生物学性质,提高玉米产量。     

The Impact of Allolobophora molleri on Soil Biology Under Different Organic Amendments

We investigated the effects of the endogenous Allolobophora molleri earthworm on the enzyme activities, the humus–enzyme complexes and the microbial community of a Plagic Antrosol soil which had been amended with different sources of organic matter. During a period of 300 days, the soil was amended with the organic fraction of a municipal solid waste at a rate of 10% or poultry manure at a rate of 7·6%, respectively, in order to apply the same amount of organic matter to the soil. At the end of the experiment, soil enzymatic activities were highest in organic amended soils with earthworms, followed by the organic‐amended soils without earthworms. The reason being, the earthworms stimulate microbial action by increasing the surface area for microbial colonization of the substrate and enzymatic through comminuting the organic wastes. The evolution of soil humus–enzyme complexes indicated the highest values of enzymes adsorbed to humus with the highest humic acid contents. The presence of A. molleri in organic‐amended soils significantly (p < 0·05) increased the soil microbial diversity. Possibly, the progressive breakdown of organic matter applied to the soil by earthworms does appear to produce new organic substrates which therefore promote the appearance of new microorganisms in the soil capable of degrading these substrates. Copyright © 2016 John Wiley & Sons, Ltd.     

西藏原始暗针叶林凋落物有机碳释放特征与土壤有机碳库关系研究

结合野外凋落物分解袋法和室内分析试验,对藏东南2种典型暗针叶林—急尖长苞冷杉(Abies georgei var.Smithii)和林芝云杉(Picea likiangensis var.linzhiensis)凋落物的分解和有机碳释放特征进行研究,分析了2种亚高山暗针叶林凋落物有机碳释放速率与土壤有机碳及其组分之间的关系。结果表明:藏东南2种原始暗针叶林凋落物分解均呈现出雨季分解快(4—9月)、旱季分解慢(10—翌年3月),前期分解快(3—9月)、后期分解慢(10—翌年2月)的特征,且冷杉(PLLF)分解速率大于云杉(AGSF),Olson指数衰减模型能够较好地模拟2种暗针叶林凋落物的分解,冷杉(PLLF)和云杉(AGSF)凋落物半分解时间为2.11,2.52年;分解95%时间为8.96,10.84年;2种暗针叶林凋落物中有机碳含量表现出先上升后下降,再平稳降低的趋势,而2种暗针叶林凋落物中有机碳释放速率表现出先短暂富集再释放的模式;2种暗针叶林土壤总有机碳(TOC)及其活性组分(MBC、POC、LOC)含量都具有明显的表聚性(p<0.01),且同一土壤层次内TOC、MBC、POC、LOC互相之间均呈极显著正相关关系(p<0.01);2种暗针叶林凋落物分解进程中有机碳的释放速率与表层土(0—10 cm)中TOC、MBC、POC、LOC含量、10—20 cm土层中的TOC、MBC含量以及20—40 cm土层中MBC含量之间呈现显著的正相关(p<0.05)。     

硼污染土壤中硼释放特征及无机离子对其释放的影响

采用连续液流法研究了硼污染土壤中硼的释放动力学过程,并采用振荡平衡法就无机离子对硼释放的影响进行了研究。结果表明,（1）供试土壤硼的累计释放量随时间的延长而增大,累计释放量与全硼含量相关性不显著,而与土壤有效硼含量呈显著正相关。（2）准二级动力学方程是描述土壤硼释放动力学过程的最佳方程。（3）供试土壤各时段硼平均释放速率的自然对数与时间呈极显著的线性相关性,随时间延长反应速率不断下降。释放速率有阶段性特点,可分为快速反应阶段、中速反应和慢速反应三个阶段,释放的硼90％以上来自前两个阶段。（4）无机离子对供试土壤中硼表现出不同的释放能力,对释放量影响的大小顺序依次为：Cl^-〉SO4^2-〉CO3^2-,Na^＋〉Ca^2＋。     

Organic Amendments with Plant-Growth-Promoting Fungi Support Paddy Cultivation in Sodic Soil

Excessive sodium content in sodic soils is an important limiting factor for cultivation of agricultural crops. The present study was conducted to explore the influence of a novel organic amendment (SF_OA) along with use of plant-growth-promoting fungi (PGPF) on soil properties and growth/yield of Oryza sativa L. The combined application of PGPF and SF_OA increased total organic carbon (TOC) (0.62%) and decreased the exchangeable sodium percentage (ESP) (15.6%) of soil more significantly from 0.56% (TOC) and 30.1% (ESP), respectively compared to SF_OA alone treatment. The combined application reduced soil bulk density, pH, and electrical conductivity (EC) and improved soil enzymatic activities. A significant negative correlation was observed between grain yield with soil ESP and bulk density (r = –0.728, and –0.789, respectively). This study showed that the combined treatment of PGPF and SF_OA could enhance the potential of organic amendments for alleviating salt stress in rice.     

不同种类有机物对污染农田土壤重金属活性的影响

为了解施用不同种类有机物对污染农田土壤重金属行为的影响,布设了田间小区试验,观察研究施用6种不同类型有机物对土壤水溶性重金属和农作物对重金属吸收等的影响。试验设7个处理,分别为对照(不施有机肥)、施新鲜水稻秸秆、新鲜鸡粪、鸡粪堆肥、新鲜猪粪、猪粪堆肥和商品有机肥,动态检测土壤中水溶性重金属含量、田面水中重金属浓度及收获水稻籽粒中重金属含量的变化。结果表明,与不施有机物的对照处理比较,施用各类有机物在试验前期均可明显提高土壤中水溶性重金属和田面水中重金属的含量,总体上以施用新鲜猪粪的最高,其次为新鲜鸡粪,施用商品有机肥的最低。土壤中水溶性重金属含量随试验时间增长逐渐下降。施用各类有机物对水稻籽粒中重金属的积累影响不明显。土壤中水溶性重金属及田面水中重金属含量均与相应的水溶性碳(DOC)浓度呈显著相关性,表明因有机物施用增加土壤中DOC浓度可能是土壤中水溶性重金属含量增加的主要原因;而不同有机物对土壤重金属活性影响的差异可能与有机物本身的分解程度及可释放DOC大小有关。但施用有机物引起的农田土壤水溶性重金属含量的增加是暂时的,对水稻生长后期籽粒中重金属积累的影响不明显。     

岩溶山区土壤溶解性有机碳对土地利用方式的响应及其与土壤养分的关系

对重庆中梁山不同土地利用方式下的表层（0-30 cm）土壤溶解性有机碳（DOC）含量和分布及其影响因素进行了研究。结果表明:土地利用方式明显影响了土壤DOC的含量和分布。不同土地利用方式下土壤DOC含量大小顺序为:橘林地（425.77 mg/kg）>菜地（342.97 mg/kg）>耕地（243.25 mg/kg）>灌丛（177.74 mg/kg）>草地（145.06 mg/kg）,土壤DOC占土壤有机碳（SOC）的比例为:橘林地>耕地>菜地>灌丛>草地。土壤DOC垂直分布规律性明显,除橘林地外,其它方式都是随着土层深度的增加而减小。相关分析表明,除了橘林地外,其余利用方式下土壤DOC均与土壤有机碳呈正相关;草地土壤微生物量碳对土壤DOC有很大的贡献,相关性达到极显著水平,其余利用方式均呈负相关。土壤DOC与土壤全氮、水解氮和速效钾相关水平达到极显著,与全磷呈显著正相关,相关系数分别为0.421,0.375,0.576,0.274,可以作为土壤肥力的变化指标。     

几种包膜缓控释肥粒养分释放特征的研究

采用水浸泡法对国内外4种包膜控释肥料的养分释放特性进行了系统的研究。结果表明,4种缓控释肥料的初期溶出率均小于12%,微分溶出率在0.4%～1.5%之间,这符合国际上公认的缓/控释肥的评价标准,初期溶出率小于15%、微分溶出率在0.25%～2.5%之间。采用水浸泡法测定包膜控释肥料养分释放特征,简便快速,检测时间短,重复次数少,养分浓度变化直接反映出包膜控释肥料的释放速率特性,还可以定量的测定其供肥性能,控释肥料有控制养分释放、延长供应时间的作用;其中腐殖酸和炭基有利于提高肥料颗粒的水稳定性,减缓养分的释放速率。     

厌氧土壤灭菌不同添加物对日光温室土壤性质及微生物群落的影响

厌氧土壤灭菌(ASD)作为替代化学农药熏蒸灭菌技术在各地逐渐推广,但不同土壤类型、不同添加物厌氧土壤灭菌效果具有较大差异,田间条件下明确当地不同添加物厌氧灭菌对土壤性质及微生物群落效应,为日光温室绿色环保的土壤灭菌方法提供科学依据。结果表明:(1)除添加碳酸氢铵(AB)处理外,其他处理均可以显著降低0—20 cm土层电导率(EC),但仅灌水不添加物料(CK)处理20—40 cm土层NO_3~--N和EC显著增加,且AB处理显著增加0—20 cm土层NH_4~+-N及20—40 cm土层NO_3~--N;添加鸡粪(CM)处理0—20 cm土层NH_4~+-N极显著增加,NO_3~--N极显著降低,EC显著降低,土壤有机质、全氮和有效养分亦显著增加。(2)添加鸡粪(CM)显著降低细菌丰富度和均匀度,但土壤中植物促生菌(PGPR)芽孢杆菌属(Bacillus)及假单胞菌属(Pseudomonas)的相对丰度极显著增加。对真菌群落,不同处理真菌丰富度和均匀度与处理前差异均不显著,但添加碳酸氢铵(AB)、木醋液(PS)和鸡粪(CM)处理病原菌-镰刀菌属(Fusarium)的相对丰度均显著降低;同时,鸡粪(CM)处理有益属曲霉属(Aspergillus)丰度显著增加。(3)综合土壤理化性质、细菌和真菌群落变化,鸡粪作为有机碳源添加厌氧土壤灭菌效果较好,既可以厌氧灭菌同时也腐熟鸡粪,且各地原料来源方便,可同时实现化肥农药双减。     

Soil Biology Changes as a Consequence of Organic Amendments Subjected to a Severe Drought

Effect of severe drought events in combination with organic amendments (municipal solid waste, MSW, sheep manure, SM, and cow manure, CM) on soil dehydrogenase, urease, β‐glucosidase and phosphatase activities and microbial community by analyzing phospholipid fatty acids was studied under controlled laboratory conditions for one year. Two levels of irrigation were used: (1) watered soils, where the soils were maintained at 60% of their water holding capacity through the experiment, and (2) non‐watered soils, without irrigation through the experiment. The severe drought conditions negatively affected the soil enzymatic activities and total bacterial and fungal PLFA concentrations. The application of organic amendments to the soil subjected to severe drought increased soil water retention and encouraged the growth and activity of soil microbial populations. However, the chemical composition of the organic matter applied to the soil also strongly influenced soil moisture. In non‐watered soils and compared with the unamended soil, the dehydrogenase activity was 71 · 3%, 60 · 9% and 38 · 6% higher in the soil with SM, CM and MSW, respectively. Urease activity was 60 · 6%, 51 · 5% and 37% higher in the soil with SM, CM and MSW, respectively. β‐glucosidase and phosphatase activities had a similar trend. Water retention was higher when the organic wastes applied to the soils had a higher content of humic acids than fulvic acid contents. Copyright © 2016 John Wiley & Sons, Ltd.