施肥对设施菜地土壤磷累积及淋失潜能的影响

以不同肥力设施菜地土壤为研究对象,通过填装土柱模拟试验,研究不同施肥措施对磷素累积及淋溶的影响.结果表明:随着淋溶时间的延长,磷素淋溶量增加,但累积淋溶量较少,说明本试验中磷素淋溶损失的风险较小,主要累积在土体内的不同土层中.试验结束时,土壤肥力和施肥处理均显著影响不同土层中全磷和速效磷含量.与低肥力土壤相比,中肥力土壤全磷和速效磷增幅为14.3%和12.2%,高肥力土壤增幅为33.3%和37.7%.有机肥化肥混施处理(M+NPK)土壤全磷含量显著高于单施化肥(NPK)和有机肥(M)处理,增幅分别为5.7%和4.3%;M及M+NPK处理中速效磷含量显著高于NPK处理,增幅分别为13.0%和3.1%.10~20 cm土层全磷和速效磷含量最高,0~10和10~20 cm土层全磷和速效磷含量显著高于20~40 cm土层.     

阿特拉津降解菌ATR3的分离鉴定与土壤修复

阿特拉津因效率高、价格低廉,是我国玉米田施用最广泛的除草剂之一,但其结构稳定,残留时间长,因此对生态环境和人类健康造成了一定的危害。从长期受阿特拉津污染的玉米田土壤中筛选并鉴定阿特拉津降解菌,明确其在不同类型土壤中的去除能力。对分离出的阿特拉津降解菌ATR3进行生理生化分析和16S rRNA序列鉴定,确定菌株ATR3为节杆菌属（Arthrobacter sp.）。该菌株以阿特拉津为唯一氮源,培养48 h后对1 000 mg/L阿特拉津的去除率达到97%以上。敏感作物盆栽试验结果表明,阿特拉津在棕壤上去除最快,褐土次之,黑土最慢,说明阿特拉津在土壤中的去除过程与土壤本身的理化性质呈相关关系。同时,该菌株处理14 d后,能明显恢复玉米的各项生物学指标,说明该菌株对阿特拉津污染土壤具有良好的修复能力。为阿特拉津降解菌剂的推广利用提供参考。     

利用雨生红球藻表达系统高通量筛选活力提高的阿特拉津氯水解酶突变子

阿特拉津氯水解酶定向改造的关键是开发一种廉价的、表型改变明显的高通量筛选方法。利用高错误倾向PCR和DNA洗牌相结合的突变方法,对来源于假单胞菌ADP和节杆菌AD1的阿特拉津氯水解酶基因进行随机突变,以雨生红球藻为受体、以阿特拉津为选择压力对突变文库进行高通量筛选。筛选到的12个突变子序列分析显示,突变均为点替换,位点分散在全基因上,是在高错误倾向PCR及DNA洗牌过程中逐渐累积形成的。酶活力分析显示,突变子的酶活力均高于野生株,在添加1.0 mg/L阿特拉津培养液中的活力是野生株的1.9~3.6倍,在添     

阿特拉津降解菌T_3 AB_1的分离鉴定及土壤修复

【目的】从阿特拉津污染土壤分离高效降解菌株,进行分类学鉴定、降解特性及黑土修复能力初步研究,为阿特拉津污染土壤微生物修复提供新的菌株。【方法】通过形态特征、生理生化特征和16S rDNA序列分析方法进行菌株鉴定;通过培养时间、温度、pH值等环境因素的研究得出菌株的最佳降解条件;通过降解菌株接种于不同种类除草剂为唯一碳氮源培养基获得该菌株的降解谱;通过土壤接种和敏感作物盆栽生测试验验证菌株对阿特拉津污染土壤修复能力。【结果】本试验从黑龙江省讷河市长期施用阿特拉津的玉米田地中分离出一株能以阿特拉津为唯一碳氮源生长的细菌T3AB1,初步鉴定为节杆菌属(Arthrobacter sp.),该菌株在72 h内对500 mg/L阿特拉津(pH 8.0)的降解率高达99%,其降解能力较高的条件为pH7.0-8.0、25-30℃、摇培72-108 h,该菌株能够利用甲氧咪草烟、咪唑乙烟酸、氟磺胺草醚、氟乐灵、异噁草松为唯一碳氮源进行生长,处理168 h的降解率能够达到12.66%-40.54%,该菌株处理21 d能够显著恢复敏感作物水稻的各项生物量指标,且随着处理时间的延长,其对土壤的修复作用也会逐渐增强。【结论】从黑龙江省污染土壤中筛选得到的高效降解阿特拉津的节杆菌属近缘种T3AB1,土壤接种实验表明该菌株具有很好的土壤修复作用,可为阿特拉津生物修复的研究提供适宜菌种资源。     

长期施肥对玉米生育期土壤微生物量碳氮及酶活性的影响

以小麦-玉米轮作长期肥料定位试验为平台,探讨不同养分管理对玉米生育期塿土微生物量碳、氮和酶活性动态变化的影响。试验包括6个处理,分别为不施肥(CK)、单施氮肥(N)、氮磷配合(NP)、氮磷钾配合(NPK)、NPK+秸秆(SNPK)以及有机肥+NPK(MNPK)。结果表明玉米生育期土壤微生物量碳、氮变化显著。不同施肥管理下土壤微生物量碳、氮的高低显著性分别为MNPK>SNPK、NP、NPK>N、CK。玉米生育期内土壤酶活性也变化显著,蔗糖酶、脲酶和纤维素酶在玉米抽雄期达到活性高峰,而磷酸酶在玉米拔节期出现活性高峰。不同施肥管理对土壤酶活性的影响总体表现为MNPK处理最高,其次为SNPK处理,再次为NPK和NP处理,N和CK处理最低。不同施肥处理间土壤微生物量碳、氮以及酶活性与土壤有机碳、全氮、速效磷水平密切相关。塿土长期施用氮磷或氮磷钾化肥可以提高土壤微生物量碳、氮以及酶活性。一季作物秸秆还田配合氮磷钾化肥与氮磷钾相比有提高土壤微生物量碳、氮以及酶活性的趋势。在等氮量下,有机肥配合化肥与其他施肥模式相比,均显著提升土壤化学肥力因素、微生物量碳氮和酶活性。因此,塿土上建议进行有机无机肥配合以提高土壤肥力,保持土壤生物健康。     

华北高产农田生态系统中蚯蚓种群次生演替规律

通过对山东省桓台县不同土壤肥力的农田生态系统中蚯蚓种群的调查发现 ,该地区农田生态系统中有 7种蚯蚓 ,高肥力土壤中蚯蚓相对较丰富 ,种群密度可达 83.83条 / m2 ,梯形流蚓为优势种 ;低肥力土壤中蚯蚓种群密度 4 0 .18条 / m2 ,优势种是天锡杜拉蚓。梯形流蚓和湖北远盲蚓在高肥力土壤中的种群密度要明显高于低肥力土壤 ;而其他几种蚯蚓种群数量变化不大 ,随着土壤肥力的演变 ,低肥力土壤中天锡杜拉蚓的优势地位随着土壤肥力的提高逐渐被梯形流蚓所代替。合理的投入特别是农田有机物投入可以加速农田生态系统中生态演替 ;试验中不同处理间蚯蚓的种群生物量有以下趋势 :化肥投入 <化肥与麦秸还田 <化肥与玉米麦秸全还田 <化肥与玉米麦秸全还田以及有机肥的施用。无论在高肥力还是低肥力的土壤上都表现出相同的规律 ,但蚯蚓种群组成并没有明显差异     

长期不同施肥方式对黄潮土肥力特征的影响

依托黄潮土35 年长期定位试验,以2种土壤物理肥力指标、8种土壤化学肥力指标和5种土壤生物肥力指标进行主成分分析,最后将各主成分得分系统进行聚类分析.结果表明: 不同施肥方式对土壤肥力指标影响显著.施用有机肥处理(M、MN、MNP、MNPK)与NPK处理相比,土壤容重显著降低,而土壤孔隙度、有机质、全氮、碱解氮、全磷、有效磷、微生物生物量和过氧化氢酶、脲酶、碱性磷酸酶活性均显著增加;通过主成分分析可将原15个土壤指标降维,提取出2个主成分,反映了原信息量的85.5%,且无原变量丢失.土壤容重、孔隙度、有机质、全氮、碱解氮、全磷、有效磷、速效钾、微生物生物量、过氧化氢酶、脲酶、碱性磷酸酶、蔗糖酶活性在第1主成分上有较高因子负荷,全钾和pH在第2主成分上有较高因子负荷;以2个主成分得分为新指标进行聚类,得到长期不同施肥方式对黄潮土的培肥效果排序为MNPK＞MNP＞M、MN＞NPK＞N、NP＞CK.可见施用有机肥对黄潮土培肥效果更显著,以有机肥配施氮磷钾化肥方式效果最优.     

长期不同施肥制度对潮棕壤肥力及微生物活性的影响

利用长期定位试验研究了不同施肥制度对潮棕壤肥力及微生物活性的影响。结果表明:长期施用有机肥、无机肥显著降低土壤pH;长期施用化肥并不能增加土壤全碳、氮含量,而有机肥的长期施用却能显著提高土壤有机质含量;土壤长期无P、K肥料施入则会出现P、K的亏损。有机肥处理(M,N+M和NPK+M)的微生物量均显著高于不施肥处理(CK),且这些处理间无显著差异;NPK处理与CK处理间无显著差异,而长期施用N肥显著降低土壤微生物量;均衡施肥处理(M,N+M,NPK和NPK+M)均能显著增强土壤微生物呼吸(P0.05),而单施N处理对土壤微生物呼吸无显著影响;与CK相比,施肥处理均能显著提高土壤氨化作用(P0.05),其中以NPK+M处理最高;除N处理外,其他施肥处理均显著提高土壤硝化作用(P0.05)。相关性分析显示,土壤微生物量碳、氮,微生物呼吸,氨化和硝化作用均与土壤全碳、全氮极显著相关(P0.01),均能够较好地反映土壤肥力变化情况;而土壤微生物活性与其他理化因子相关性不一致,表明它们对土壤理化因子变化的响应程度不同。     

阿特拉津及其降解菌的使用对土壤微生物群落的影响

比较了阿特拉津及降解菌株BTAH1的使用对土壤微生物的影响.结果表明,在实验周期内阿特拉津对土壤微生物的代谢作用有较明显的刺激作用,与空白土壤(未施用阿特拉津和降解菌)相比,对照土壤(施用50 mg·kg^-1土阿特拉津)呼吸强度显著增加,且土壤中的阿特拉津浓度对土壤NH₄⁺-N和NO₃^--N浓度的影响显著.降解菌BTAH1可在1周内降解土壤中98%以上的阿特拉津,从而使土壤呼吸强度有所下降,土壤中NH₄⁺-N和NO₃^--N的浓度基本与空白土壤持平,对微生物量C和微生物量N影响不显著;放线菌和真菌数量也基本与空白持平,细菌数量较高.对土壤细菌的16S rDNA文库的ARDRA分析发现,阿特拉津及其降解菌的使用对土壤细菌群落结构有一定程度的影响,阿特拉津的使用会降低细菌群落的多样性,而降解菌的使用会恢复土壤细菌的多样性.     

阿特拉津降解菌株AD111的分离鉴定及其降解特性

【背景】玉豆轮作过程中,玉米田中长残留除草剂阿特拉津易对下茬大豆作物产生不良影响。【目的】从黑龙江省安达市的农田土筛选一株能适应该土壤环境生长的阿特拉津降解菌并研究其降解特性。【方法】利用富集培养法,分离、筛选一株阿特拉津高效降解菌并结合外观形态、生理生化及16SrRNA基因序列测定对其进行鉴定,通过单一变量法设置不同的碳源、pH、温度和阿特拉津浓度,研究降解菌株最佳发酵及降解条件。【结果】得到一株在BSM-G中能够以阿特拉津为唯一氮源生长的高效阿特拉津降解菌AD111,鉴定为马德普拉塔无色小杆菌(Achromobacter marplatensis)。菌株AD111降解阿特拉津的最适温度为35℃,最适pH为8.0,最佳碳源为蔗糖,24 h内对浓度为50 mg/L的阿特拉津降解率达到99.7%,对300 mg/L的阿特拉津降解率达到81.9%。【结论】降解菌AD111具有较好的环境适应及阿特拉津降解能力,为解决黑龙江偏碱土壤中阿特拉津残留提供了良好的候选菌株。     

砷对土壤脲酶活性影响的研究

采用模拟方法对As污染土壤脲酶特征进行了研究．结果表明,土壤中As浓度在0～200mg·kg^-1浓度范围内,反应初期脲酶活性变化无明显规律;一年后砷激活土壤脲酶活性,二者达到显著或极显著正相关．随As浓度增加,土壤脲酶Km值基本不变或略有增加,Vmax增大,从机制上揭示出As加速脲酶-尿素复合物的解离．厩肥和无肥土样脲酶对As的反应类似,只是变化幅度有所差异．     

酸雨、铜和莠去津对土壤水解酶活性的影响

运用正交试验设计方案,考察了酸雨、重金属铜和农药莠去津复合污染情况下各因素的主效应及两两交互作用对土壤脲酶、转化酶和酸性磷酸酶活性的影响。结果表明,H^+、Cu^2+对酶活性影响显著且其对3种酶的抑制效应为H^+>Cu^2+;Al^3+仅对脲酶表现出一定的激活效应;而除磷酸酶外,莠去津对脲酶、转化酶活性无明显影响。交互作用试验表明：莠去津×Cu的协同作用主要表现为对磷酸酶活性的影响;而H×Cu对脲酶、转化酶均表现为颉抗作用;在本文所考察的浓度范围内,未见莠去津与氢有显著的交互作用存在3种酶中,以磷酸酶对外来污染物最为敏感。     

Effects of Different Organic Manures on the Biochemical and Microbial Characteristics of Albic Paddy Soil in a Short-Term Experiment

This study aimed to evaluate the effects of chemical fertilizer (NPK), NPK with livestock manure (NPK+M), NPK with straw (NPK+S), and NPK with green manure (NPK+G) on soil enzyme activities and microbial characteristics of albic paddy soil, which is a typical soil with low productivity in China. The responses of extracellular enzyme activities and the microbial community diversity (determined by phospholipid fatty acid analysis [PLFA] and denaturing gradient gel electrophoresis [DGGE]) were measured. The results showed that NPK+M and NPK+S significantly increased rice yield, with NPK+M being approximately 24% greater than NPK. The NPK+M significantly increased soil organic carbon (SOC) and available phosphate (P) and enhanced phosphatase, β-cellobiosidase, L-leucine aminopeptidase and urease activities. The NPK+S significantly increased SOC and available potassium (K) and significantly enhanced N-acetyl-glucosamidase, β-xylosidase, urease, and phenol oxidase activities. The NPK+G significantly improved total nitrogen (N), ammonium N, available P, and N-acetyl-glucosamidase activity. The PLFA biomass was highest under NPK+S, followed by NPK+M and NPK+G treatments. Principal component analysis (PCA) of the PLFA indicated that soils with NPK+M and NPK+S contained higher proportions of unsaturated and cyclopropane fatty acids (biomarkers of fungi and gram-negative bacteria) and soil under NPK+G contained more straight chain saturated fatty acids (representing gram-positive bacteria). PCA of the DGGE patterns showed that organic amendments had a greater influence on fungal community. Cluster analysis of fungal DGGE patterns revealed that NPK+G was clearly separated. Meanwhile, the bacterial community of NPK+M treatment was the most distinct. RDA analysis revealed changes of microbial community composition mostly depended on β-xylosidase, β-cellobiosidase activities, total N and available K contents. The abundances of gram-negative bacterial and fungal PLFAs probably effective in improving fertility of low-yield albic paddy soil because of their significant influence on DGGE profile.     

Comparison of crop productivity and soil microbial activity among different fertilization patterns in red upland and paddy soils

Soil enzyme activity and microorganism community can be changed through different long-term fertilization patterns. However, the effect of different fertilization practices on soil microorganisms might differ among crop systems. The objective of the study was to reveal the change of soil enzyme activity and soil microorganism community in different fertilizations both in upland and paddy soils. Therefore, based on long-term fertilization experiments in upland soil started in 1986 and adjacent paddy soil experiment commenced in 1981, with both consisting of 4 treatments: Control (no fertilization), N (only nitrogen fertilizer), NPK (nitrogen, phosphate and potassium fertilizers) and NPKM (nitrogen, phosphate and potassium fertilizers plus organic manure), grain yield, soil fertility, activities of soil urease, catalase, acid phosphatase, microorganism community (the number of bacteria, fungus and actinomycete) were analyzed. The result showed that: the highest grain yield was attained under the application of chemical fertilizers plus manure, as compared with Control, NPKM significantly increased the grain yield by 908.63% in corn and 118.80% in rice (p < 0.05). Meanwhile, NPKM treatment increased significantly soil organic matter and nutrient contents in upland and paddy soils. Interestingly, there was no significant difference in soil pH among all the treatments of paddy soil, but in upland, NPKM increased pH in comparison to Control by 23.06% (1.15 units of pH). Compared with Control, soil urease, catalase activities, bacteria and actinomycete numbers of NPKM were increased by 321.39%, 129.64%, 229.79%, 85.81% in upland soil, and 25.11%, 251.12%, 292.83%, 196.34% in paddy soil. However, in paddy soil, the soil acid phosphatase activity of Control, NPK and NPKM treatments were higher than upland soil by 34.87%, 44.81%, 52.73% and 30.11%. Then, the soil fungus and actinomycete numbers of paddy soil were lower than upland soil by 20.20% and 88.29%. Therefore, it indicated that long-term application of chemical and organic fertilizers delivered highest productivity in both experiment but the effect of fertilizer practices differed between land uses.     

新型磷酰胺类脲酶抑制剂对不同质地土壤尿素转化的影响

施用脲酶抑制剂是降低尿素水解、减少氨气挥发损失、提高作物氮(N)肥利用率的重要途径之一.采用室内恒温、恒湿模拟试验方法,在25 ℃黑暗条件下培养,研究新型磷酰胺类脲酶抑制剂N-丙基磷酰三胺(NPPT)的脲酶抑制效果,比较其与N-丁基磷酰三胺(NBPT)在不同尿素用量条件下不同质地土壤中对脲酶的抑制差异.结果表明: 在壤土和黏土中,尿素作用时间≤9 d,添加抑制剂可以将尿素水解时间延长3 d以上.砂土中,尿素分解过程相对缓慢,添加抑制剂显著降低土壤脲酶活性,抑制NH₄⁺-N生成.在培养期间,不同尿素用量条件下,脲酶抑制剂在不同质地土壤中的抑制效果表现为高施N量优于低施N量.培养第6天,在尿素用量250 mg N·kg^-1条件下,NBPT和NPPT在砂土中脲酶抑制率分别为56.3%和53.0%,在壤土中分别为0.04%和0.3%,在黏土中分别为4.1%和6.2%;尿素用量500 mg N·kg^-1,NBPT和NPPT在砂土中脲酶抑制率分别为59.4%和65.8%,在壤土中分别为14.5%和15.1%,在黏土中分别为49.1%和48.1%.不同质地土壤中脲酶抑制效果表现为砂土>黏土>壤土.不同抑制剂处理在培养期间土壤NH₄⁺-N含量呈现先上升后下降的趋势,而NO₃^--N含量和表观硝化率均呈现逐渐上升的趋势.与单施尿素处理相比,添加脲酶抑制剂NBPT和NPPT显著增加土壤中的残留尿素态N,降低NH₄⁺-N生成.新型脲酶抑制剂NPPT在不同质地土壤中的抑制效果与NBPT相似,是一款有效的脲酶抑制剂.     

汞、镉对土壤脲酶活性影响的研究Ⅰ.尿素浓度

对不同尿素浓度条件下重金属与土壤脲酶活性关系进行了研究。结果表明,尿素浓度对脲酶活性具有显著的影响。在供试浓度范围内可采用线性和Langmuir模型较好地表征二者关系。并得到脲酶活性的尿浓贡献率,尿浓贡献变化率和最大表观脲酶活性等参数;Hg,Cd明显降低了前述参数值,其中Hg Cd复合污染的抑制作用最强,Hg的生态毒性最大;同时初步获得土壤酶促反应过程中存在吸附机制。     

模拟咸水入侵对崇明岛河岸带根际土壤微生物及反硝化作用的影响

通过模拟咸水入侵,研究了其对崇明岛河岸带根际土壤微生物及其反硝化过程的影响.结果表明:模拟咸水入侵后4种不同植被型河岸带土壤根际微生物区系发生显著变化,除放线菌菌群数量稍有增加外,细菌、真菌以及硝化和反硝化细菌数量均出现不同程度下降,特别是反硝化功能细菌数量较对照平均下降51.8％,说明河岸带土壤不同微生物区系对咸水入侵的响应存在显著差异.模拟咸水入侵后,河岸带土壤与氮转换相关的酶活性普遍受到抑制,且抑制作用随酶类型不同而存在差异,亚硝酸还原酶对咸水入侵最敏感,其活性较对照平均下降了43.5％,脲酶活性次之,其降幅为37.4％,而脱氢酶受咸水影响较小,其活性平均下降29.5％.模拟咸水入侵明显削弱了河岸带土壤反硝化作用,其速率平均下降34.9％.不同植被型河岸带土壤微生物对咸水入侵的生态生理响应存在显著差异,与对照相比,茭白根际土壤微生物数量和酶活性受咸水入侵的平均抑制率最大,土壤反硝化速率最小,其次是菖蒲和芦苇.在模拟咸水入侵下,菖蒲与芦苇混合群落根际土壤微生物数量、酶活性和反硝化速率抑制率明显低于单一植物模式,表明混合植被群落根际土壤微生物过程及反硝化作用对咸水入侵具有较好的缓冲性能.     

长期培肥黑土脲酶活性动态变化及其影响因素

以东北典型黑土区长期(自1980年)不同培肥试验地土壤为研究对象,采用两种不同量有机肥、化肥和不施肥4个处理,对土壤脲酶在作物生长季的动态变化进行研究。结果表明,施用有机肥,生长季黑土脲酶活性明显高于施用化肥和不施肥,其生长季脲酶保护容量在160mg·kg^-1·h^-1以上,季节性变化平稳。保持土壤脲酶免遭变性、免遭分解作用显著．脲酶活性的动态变化与绝大多数土壤生物、理化特性指标的动态变化没有明显的相关性;与土壤生物、理化特性,植物N、P、K有极显著的正相关关系;与土壤含水量、籽粒粗蛋白含量呈显著正相关关系。     

Stimulation by nickel of soil microbial urease activity and urease and hydrogenase activities in soybeans grown in a low-nickel soil

Summary The concentration of nickel in some soils may be insufficient to meet the requirements of enzymes such as urease in soybeans and hydrogenase in Rhizobium. In an initial evaluation of nickel availability, several soils were examined for nickel content and microbial urease activity. Total and extractable nickel were determined by atomic emission spectrometry. Purified glucose and urea were added to soils to stimulate microbial growth and urease activity, the latter of which was monitored by the rate of decomposition of¹⁴C urea. Nickel also was added to some samples to determine if the indigenous supply was limiting. In one low-nickel soil (total Ni 13 ppm) urease activity increased 150% in response to additional nickel, while other soils (total Ni 22–3491 ppm) failed to respond to nickel. However, additional nickel did stimulate urease activity (up to 109%) in 3 out of 10 soils to which purified CaCO₃ was added. Presumably the rise in pH associated with this treatment decreased nickel availability. Additions of Co, Mn, Fe, or Cu had no consistent effect on urease activity, thus indicating that the response to Ni was specific. Nickel fertilization increased leaf urease and nodule hydrogenase activity of soybeans grown in low-nickel soil, however, yield was not improved. These results may have practical implications in the nutrition of plants and micro-organisms that metabolize H₂ and urea.