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1.
炭基肥和竹炭对土壤氮素淋失和微生物的影响   总被引:1,自引:0,他引:1  
为了研究竹炭和炭基缓释肥添加对毛竹林土壤氮素流失和细菌群落结构的影响,采用室内土柱淋溶试验,测定了淋溶水中NH_4+—N和NO_3-—N浓度,分析了细菌群落多样性和组成。结果表明,与对照相比,炭基缓释肥的添加可以使土柱NH_4+—N和NO_3-—N累积淋溶量分别降低12.5%和13.6%。此外,竹炭的添加可以显著降低NH_4+—N累积淋溶量(P<0.05),但是对NO_3-—N的影响不显著。炭基缓释肥的添加可以增加土壤Nitrospira(硝化螺菌属)、Nitrosospria(亚硝化螺菌属)和Nitrobacter(硝化杆菌属)细菌的相对丰度,提高下层淋溶土壤反硝化优势菌群(丰度>0.1%)Burkholderia(伯克霍尔德菌属)、Cupriavidus(贪铜菌属)和Bradyrhizobium(慢生根瘤菌属)的相对丰度。炭基缓释肥添加对土壤NH_4+—N和NO_3-—N的淋溶影响可能与土壤氮素循环微生物密切相关。  相似文献   

2.
摘 要:灭蚁灵是一类高毒性的有机氯农药,当灭蚁灵通过直接或间接的人为途径进入到土壤生态环境系统后,会对生物体产生显著的毒害作用。土著菌群与蚯蚓肠道菌群都是对外源农药极其敏锐的感知受体,然而,它们对于抵御灭蚁灵毒害作用的微生物响应机制尚不清楚,值得探究。因而,本研究采集实际场地中不同梯度浓度(0~27.7 mg/kg)灭蚁灵污染土壤,设置蚯蚓土培实验,采用高通量测序技术,分析蚯蚓肠道菌群和土著菌群的结构和功能;通过MetagenomeSeq分析、LEfSe(Linear Discriminant Analysis Effect Size)分析和随机森林(Random Forests)分析以及网络分析,识别其核心类群。发现:1)灭蚁灵胁迫下蚯蚓肠道菌群相较之土著菌群的结构、组成受到的扰动更显著(p < 0.05);2)不同梯度灭蚁灵胁迫下,蚯蚓肠道菌群和土著菌群组合存在稳定的核心物种,主要为气单胞菌属(Aeromonas)、黄杆菌属(Flavobacterium)、盖勒氏菌属(Gallerella)、微枝形杆菌属(Microvirga)、地杆菌属(Pedobacter)、亨氏菌(Ramlibacter)、Zavarzinella;3)这些核心种群在互作网络的平均度中心性、紧密中心性、特征向量中心性分别为136.72、0.44、0.52,均高于非核心种群的对应指标(91.52、0.42、0.33),表明核心种群具有更高的网络连通性,且此类核心种群具有碳氮转化和农药降解能力,说明蚯蚓肠道菌群和土著菌群可以通过共享核心物种与其它微生物联系紧密,具备发挥农药降解代谢的潜在功能,实现协同抵御土壤中灭蚁灵胁迫。本研究结果可为探明土著菌群与蚯蚓肠道菌群共享核心物种在抵御土壤中有机氯农药毒害作用的协同机制,提供新的科学认识。  相似文献   

3.
不同施肥模式对土壤氮循环功能微生物的影响   总被引:3,自引:1,他引:2  
  【目的】   微生物在土壤氮循环过程中发挥着重要作用。通过研究农田土壤氮循环过程中不同功能微生物群落基因丰度对施肥模式的响应及其关键影响因素,探讨不同施肥模式调控下氮素转化的微生物学机制,为改善农业生产中氮素的管理策略提供理论依据。   【方法】   田间试验始于2011年,试验地点位于江苏省常州市溧阳市南渡镇,供试土壤为白土型水稻土,种植制度为稻麦轮作。试验包括单施化肥 (NPK)、化肥+畜禽有机肥 (NPKM)、化肥+秸秆还田 (NPKS) 以及相邻江苏省耕地质量监测点不施肥对照 (CK),共 4个处理。于2014年水稻成熟期采集土壤样品,采用实时荧光定量PCR法分析了土壤硝化 (amoA)、反硝化 (narG、nirS、nirK、norB、nosZ)、固氮 (nifH)、硝酸盐异化还原 (napA) 等氮循环过程的相关功能微生物基因丰度的变化。以氨氧化微生物为模式微生物,测定添加与不添加1-辛炔情况下的土壤硝化潜势,分析氨氧化古菌 (AOA) 与氨氧化细菌 (AOB) 功能基因丰度与土壤硝化功能的内在联系。   【结果】   与CK相比,NPK处理显著增加了土壤中AOB-amoA、narG、nosZ和nifH基因的丰度。与NPK处理相比,NPKS处理进一步提高了土壤中AOB-amoA、narG、nosZ、nifH以及nirK基因的丰度。与CK相比,除AOA-amoA、nirS、napA基因以外,NPKM处理显著提高了土壤中所有氮循环功能基因的丰度。AOB-amoA基因丰度的变化对土壤氮循环功能基因丰度的整体变异影响最大。AOB主导了施肥土壤的硝化过程 (81.90%~84.42%)。土壤总硝化潜势与AOB-amoA基因丰度显著相关,但与AOA-amoA基因丰度相关性不显著。氮循环功能微生物基因丰度主要受到土壤pH、土壤有机碳(SOC)和NO3–含量的影响。   【结论】   畜禽有机肥与秸秆的施用能够进一步刺激氮循环功能基因丰度的增长,促进土壤氮循环。土壤pH、SOC和NO3–含量是影响土壤氮循环功能微生物丰度的关键因素。施肥主要通过提高土壤AOB-amoA功能基因的丰度,进而提高土壤硝化潜势,因此在控制土壤硝化作用时应重点关注AOB微生物群落。  相似文献   

4.
【目的】研究秸秆分解过程中同化利用秸秆碳源的微生物生态演替过程,明确参与秸秆分解的主要微生物类群,为秸秆高效利用提供科学依据。【方法】采用13C标记高丰度玉米秸秆。微宇宙室内培养试验的供试土壤为华北平原石灰性潮土。共设置3个处理:不添加秸秆(soil)、添加自然丰度秸秆(soil+12C-straw)和添加13C标记秸秆(soil+13C-straw)。培养30天时,结合同位素示踪与高通量测序等技术,测定秸秆添加对土壤有机碳的激发效应,分析利用秸秆碳源的细菌、真菌群落结构及其与土壤胞外酶活性的关系。【结果】1)秸秆添加显著提高了土壤CO2排放,添加秸秆对土壤有机碳的激发效应在培养第1天达到峰值,土壤和秸秆CO2排放比例均在培养第3天达到峰值。2)整个培养时期共发现参与秸秆碳同化利用的细菌微生物操作分类单元(operational taxonomic units,OTUs) 238个,真菌OTUs 24个。细菌OTUs主要属于细菌变形菌门(Proteobac...  相似文献   

5.
氯氰菊酯污染土壤的微生物修复及对土著微生物的影响   总被引:6,自引:0,他引:6  
在实验室条件下,在含有氯氰菊酯的土壤中添加氯氰菊酯和3-苯氧基苯甲酸(3-PBA)降解菌CDT3(Rhodococcussp.)和PBM11(Pesudomonassp.),同时设不加菌的对照。分别于0、3、7、15、30 d取样,测定土壤中氯氰菊酯和3-PBA的残留,同时用平板计数和变性梯度凝胶电泳(DGGE)方法分析土壤微生物群落的变化。结果显示:CDT3和PBM11在土壤中协同作用能够更好地降解氯氰菊酯及其中间产物3-PBA。氯氰菊酯对土著微生物有较强的抑制作用。投加降解菌可以消除农药对土壤微生物的抑制,有助于土著微生物种群的恢复,但短期内无法改变农药对土壤微生物结构的破坏。  相似文献   

6.
  【目的】  研究青海高原麦秸和豆科绿肥混合添加下土壤温室气体排放规律及其碳氮转化机制,为该地区农田系统秸秆和绿肥科学利用提供依据。  【方法】  采用室内模拟试验,设无添加对照(CK)、单独添加毛叶苕子(VS)、单独添加麦秸(WS)、麦秸与毛叶苕子混合添加(VWS),共4个处理。测定了温室气体排放速率、土壤活性碳氮组分、土壤酶活性、细菌、古菌、真菌、amoA、nirK和narG基因丰度。  【结果】  VWS处理与VS处理相比,CO2和N2O的累积排放量分别减少24.8%和74.6%,CH4累积吸收量增加9.1%,综合增温潜势(global warming potential, GWP)显著降低76.1% (P<0.05);与WS处理相比,CO2累积排放量增加33.7%,CH4累积吸收量与N2O累积排放量分别降低12.0%和43.1%,GWP降低49.4%。有机物料添加可调节土壤pH,增加土壤碳氮含量。VWS处理的土壤pH显著高于CK和VS处理;土壤水溶性有机碳(DOC)和微生物量碳(SMBC)含量较VS处理分别增加了21.6%和4.9%,无机氮(Nmin)、土壤水溶性有机氮(DON)和微生物量氮(SMBN)含量分别降低了77.3%、59.5%和6.3%;土壤Nmin、DOC、DON、SMBC和SMBN含量较WS处理分别增加64.0%、22.5%、56.5%、23.2%和27.8%。VWS处理较其他处理,α-葡萄糖苷酶(AG)和β-葡萄糖苷酶(BG)活性显著提高,亚硝酸还原酶(NIR)活性显著降低。VWS处理的真菌和古菌群落丰度较WS处理分别提高83.8%和69.8%,较VS处理分别降低62.6%和20.3%;VWS处理细菌群落丰度较VS处理降低33.4%。VWS处理下,AOB amoA、nirK和narG基因丰度较VS处理分别降低56.6%、41.4%和16.3%,较WS处理分别降低30.3%、25.9%和12.0%。相关分析结果表明,CO2和CH4排放与土壤有机碳、全氮、DOC、SMBC和SMBN含量,AG、NAG和NR活性,真菌、细菌、nirK和narG基因丰度呈显著正相关;N2O排放与土壤全氮、DON、SMBC和SMBN含量、真菌、AOB amoA和nirK基因丰度呈显著正相关,与土壤pH和BG活性呈显著负相关。偏最小二乘路径模型分析(PLS-PM)表明,AOB amoA是调控土壤N2O排放的主要功能菌群。  【结论】  麦秸、毛叶苕子单独添加以及二者混合添加均可促进土壤CO2排放,减少CH4吸收。相较于二者单独添加,混合添加可通过降低土壤AOB群落丰度等途径,实现N2O减排和综合增温潜势下降,可作为青海高原旱地土壤温室气体减排的一项有效措施。  相似文献   

7.
添加生物炭改善菜地土壤氨氧化细菌群落并提高净硝化率   总被引:2,自引:0,他引:2  
  【目的】  氨氧化过程是硝化作用的限速步骤,对氮循环有着重要影响。本研究通过分析生物炭输入下土壤氨氧化微生物群落的变化,揭示其影响土壤硝化作用的生物学机制。  【方法】  以华北潮土区设施菜地土壤为对象,设置生物炭梯度 (C0、C0.5、C1.5、C4.0) 土壤培养试验,结合PCR和T-RFLP等分析技术,观测生物炭输入下土壤氨氧化细菌群落变化动态,解析生物炭、土壤硝化作用与氨氧化细菌群落之间的关系。  【结果】  添加生物炭明显改变了土壤氨氧化微生物群落结构及氮素硝化过程。与未添加生物炭处理相比,生物炭添加处理培养前期土壤氨氧化细菌群落Shannon、Evenness指数分别升高5.4%~18.8%、26.2%~33.8%,后期Shannon指数降低20.7%~34.2%。生物炭输入对AOA群落没有明显影响,AOB群落256、58 bp代表物种丰度分别增加61.4%~56.0%、60.6%~78.6%,488 bp代表物种丰度降低22.8%~26.9%。21 bp代表物种丰度前期增加后期降低,与491 bp代表物种丰度变化相反。添加生物炭土壤AOB amoA基因丰度增加48.9%~53.2%。土壤NO3–-N含量提高1.7%~25.6%,NH4+-N含量下降13.4%~31.1%,土壤净硝化速率提高21.8%~70.2%。  【结论】  生物炭的输入可以改善以AOB为主的土壤氨氧化微生物群落结构,提高amoA酶活性,但是对氨氧化古菌微生物群落结构未产生明显影响。因此,生物炭提高土壤净硝化速率的作用与其对土壤氨氧化细菌群落和组成的影响密切相关。  相似文献   

8.
为揭示长期耕作对农田黑土几丁质降解菌群及酶活性的影响及其驱动因子,以黑土区耕法长期定位试验为平台,采用荧光定量和高通量测序技术研究不同耕作措施(灭茬起垄、免耕、间隔深松和翻耕)下0~40 cm土层chiA几丁质降解菌基因丰度、微生物群落结构和酶活性。结果表明:0~20 cm土层,免耕显著提高chiA基因丰度;20~40 cm土层,免耕降低chiA基因丰度、alpha多样性和变形菌门(Proteobacteria)相对丰度,但是增加放线菌门(Actinobacteria)相对丰度。土壤pH、平均重量直径和养分含量显著影响chiA基因丰度和群落结构。与灭茬起垄相比,免耕显著提高0~20cm土层几丁质酶活性,而间隔深松和深翻显著提高0~40 cm土层几丁质酶活性。结构方程模型模拟发现耕作方式、土壤深度、平均重量直径、土壤有机碳、全氮、全磷、chiA基因丰度和放线菌门相对丰度对几丁质酶活性具有显著直接效应。研究结果为明确黑土区不同耕作措施对土壤几丁质降解的影响提供理论基础。  相似文献   

9.
  【目的】  土壤中的氧化亚氮 (N2O) 来源于硝化与反硝化作用,锰可与硝化或反硝化作用产物反应产生N2O或氮气,已有研究表明土壤中锰含量高会影响硝化作用。因此,本试验以水钠锰矿 (KMnO2·H2O) 与土壤硝化作用与反硝化作用的生物化学耦合反应为切入点,研究水钠锰矿的添加对土壤N2O释放速率及微生物的影响,进一步认识N2O释放与土壤环境因子的相互关系。  【方法】  以红壤性水稻土为供试土壤,通过微宇宙培养试验,在土壤中添加不同质量百分比的水钠锰矿 (0%、0.1%、0.3%、0.7%、1.5%),预培养7 天后,加入硫酸铵N 100 mg/kg继续培养14天。在培养第1、3、7、14天,采用气密性注射器抽取10 mL气体样品,气相色谱仪测定N2O含量;同时取土壤样品,比色法测定铵态氮与硝态氮含量。培养结束时,测定土壤pH,采用实时荧光定量PCR测定土壤16S rDNA与氨氧化细菌 (AOB) amoA基因拷贝数,高通量测序技术分析微生物群落组成及多样性。  【结果】  水钠锰矿提高了土壤N2O释放速率,增加了土壤N2O累积释放量,以添加0.1%水钠锰矿的N2O累积释放量最高,添加1.5%的最低。土壤铵态氮含量随培养时间的延长而迅速降低,硝态氮含量则迅速增加。水钠锰矿显著提高了土壤pH与表观N2O产量 (N2O-N/NO3?-N),pH随着水钠锰矿添加量的增加整体提高,N2O-N/NO3?-N则随着水钠锰矿添加量的增加呈降低趋势。适量水钠锰矿显著增加了土壤细菌16S rDNA与氨氧化细菌 (AOB) amoA基因拷贝数,并显著提高了土壤16S rDNA与AOB amoA基因拷贝数的比值,但随着水钠锰矿添加量的增加,细菌16S rDNA和AOB amoA基因拷贝数的增加量整体降低;放线菌、变形菌与拟杆菌是所有处理中的优势菌门,通过非度量多维尺度分析发现不同处理间的微生物群落结构差异显著,未添加水钠锰矿处理与添加水钠锰矿1.5%处理的微生物群落结构差异最大,其他处理的微生物群落结构介于两者之间。  【结论】  土壤中添加0.1%质量比的水钠锰矿,可以通过增加AOB的数量促进红壤性水稻土N2O的释放,显著影响微生物物种丰度与群落结构。但水钠锰矿高添加量处理对AOB的刺激作用减弱,因此,应将土壤锰含量作为影响土壤N2O释放的因素加以考虑。  相似文献   

10.
【目的】研究苏南地区稻麦轮作农田转变为桃园对土壤理化及生物学性质的影响,旨在为苏南地区土地合理利用和土壤质量管理提供数据支撑。【方法】于2017年麦季 (5月) 和稻季 (7月) 采集研究区稻麦轮作田及由其改为桃园的土壤样品,采用常规方法测定土壤理化性质,96微孔酶标板荧光分析法测定土壤酶活性,实时荧光定量方法测定细菌16S rRNA和真菌ITS基因丰度。【结果】当土地利用方式由稻麦轮作田转变为桃园后,土壤理化性质发生明显变化。与水旱轮作田相比,桃园土壤容重增加,总孔隙度没有明显改变,但毛管孔隙度显著降低,而非毛管孔隙度显著增加,土壤更加紧实,pH有进一步降低的趋势;土壤有机质含量下降,全磷和有效磷含量增加;土壤细菌16S rRNA基因丰度下降,真菌ITS rRNA基因丰度升高,有机质降解的微生物群落由“细菌型”向“真菌型”转化。相应地,土壤中与氮转化相关酶和过氧化氢酶活性降低。从春季到夏季,稻麦轮作田和桃园土壤有机碳含量均下降,稻田降幅较大。另外,两种利用方式下土壤的细菌16S rRNA基因丰度、真菌ITS rRNA基因丰度、纤维素酶和蔗糖酶的活性均显著下降。【结论】苏南地区农业土地利用方式的转变显著增加了土壤容重,改变了土壤孔隙性,增加了土壤全磷和有效磷含量,降低了土壤pH,进而大幅度降低了土壤中氮转化酶活性,并促使土壤微生物菌群由细菌型向真菌型转变,最终影响土壤的养分循环及固碳潜力。因此,土地利用方式改变后,应注重土壤养分的管理。  相似文献   

11.
低氮和干旱胁迫对富士和秦冠生长及氮素利用的影响   总被引:2,自引:2,他引:0  
【目的】以富士(Fuji)、 秦冠(Qinguan)嫁接在平邑甜茶(Malus hupehensis Rehd.)上的当年生盆栽苗为试验材料,采用砂培方法,研究了缺氮胁迫和干旱对富士和秦冠生长情况、 光合参数、 植株各部位氮磷钾含量及氮素利用效率的影响,分析比较了低氮干旱条件下富士和秦冠生长及氮素利用的差异,以期为果树生产高效肥水利用提供理论指导。【方法】试验共设四个处理: 正常氮正常水(ZZ)、 低氮正常水(DZ)、 正常氮干旱(ZG)、 低氮干旱(DG)。氮素和水分均设置两个水平,分别为正常氮(6 mmol/L NO-3-N)、 低氮(0.3 mmol/LNO-3-N)、 正常供水(保持盆中砂子相对含水量为饱和含水量的80%~85%)、 干旱处理(保持盆中砂子相对含水量为饱和含水量的60%~65%)。【结果】富士和秦冠的生物量(茎和叶)、 株高茎粗等生长指标以及光合速率、 气孔导度、 蒸腾速率均为正常氮正常水(ZZ)>低氮正常水(DZ)>正常氮干旱(ZG)>低氮干旱(DG),并且相对应处理下秦冠的以上指标均高于富士;正常供水下,缺氮处理使富士、 秦冠的根冠比比正常氮处理均有所增加,富士提高了2.05%,秦冠提高了22.40%。富士和秦冠的氮、 磷、 钾含量均表现出正常氮正常水(ZZ)>低氮正常水(DZ)>正常氮干旱(ZG)>低氮干旱(DG); 氮、 钾元素含量在植株各部位的分布顺序依次是叶>根>茎,磷元素则是根>叶>茎;光合氮素利用效率(PNUE)和氮素利用效率表现为秦冠处理之间差异极显著,富士处理之间差异不显著;秦冠的PNUE和NUE明显高于富士,在低氮正常水(DZ)处理下,秦冠氮肥利用率比富士高42.07%,在低氮干旱(DG)处理下高64.14%;低氮胁迫下富士和秦冠的NUE显著提高,并且秦冠提高的幅度高于富士。【结论】施用氮肥能够显著提高富士与秦冠的干物质量,同等水肥条件下,秦冠生长优于富士;水分亏缺会减少叶片对氮的吸收,干旱条件下适度增施氮肥,可提高果树的抗旱能力;低氮干旱胁迫下秦冠的生长指标、 光合指标及氮素利用效率指标均优于富士,表现出较强的抗低氮干旱胁迫的能力。  相似文献   

12.
Laser-induced breakdown spectroscopy (LIBS) is a new technique for the analysis of plant material. This study investigates the application of LIBS to pasture-based plant samples. The LIBS measurements were obtained from pelletized pasture samples (100 samples) that had been also analyzed by inductively coupled plasma–optical emission spectroscopy (ICP-OES) following microwave digestion for calibration and comparison purposes. Comparisons for elements sodium (Na), potassium (K), magnesium (Mg), calcium (Ca), manganese (Mn), iron (Fe), copper (Cu), zinc (Zn), boron (B), phosphorus (P), and sulfur (S) showed that LIBS could be used for almost all the standard profile total elements with concentrations down to low mg/kg levels (observed error of Na: 0.024 percent, K: 0.18 percent, Mg: 0.016 percent, Ca: 0.073 percent, P: 0.017 percent, Mn: 31 mg/kg, Fe: 150 mg/kg, Zn: 6.6 mg/kg, and B: 1.1 mg/kg). Elemental analysis at less than mg/kg levels was not possible using LIBS. The elements S and Cu were particularly difficult to analyze with reliability using LIBS at the concentration levels found in the plant samples. Replacing microwave digestion and subsequent ICP analysis with a direct analysis of dried plant samples using LIBS has the potential to improve the productivity and reduce the cost of testing.  相似文献   

13.
正The Center for Agricultural Resources Research(CARR),the Institute of Genetics and Developmental Biology(IGDB),Chinese Academy of Sciences,invites applicants for several research group leader positions.CARR is one of the research organizations in Chinese Academy of Sciences(CAS).We seek nominations and applications from individuals who have expertise and a record of accomplishment in research areas related to ecology,agro-hydrology,  相似文献   

14.
The responses of tallgrass prairie plant communities and ecosystem processes to fire and grazing are well characterized. However, responses of invertebrate consumer groups, and particularly soil-dwelling organisms, to these disturbances are not well known. At Konza Prairie Biological Station, we sampled soil macroinvertebrates in 1994 and 1999 as part of a long-term experiment designed to examine the effects and interactions of annual fire, mowing, and fertilization (N and P) on prairie soil communities and processes. For nearly all taxa, in both years, responses were characterized by significant treatment interactions, but some general patterns were evident. Introduced European earthworms (Aporrectodea spp. and Octolasion spp.) were most abundant in plots where fire was excluded, and the proportion of the total earthworm community consisting of introduced earthworms was greater in unburned, unmowed, and fertilized plots. Nymphs of two Cicada genera were collected (Cicadetta spp. and Tibicen spp.). Cicadetta nymphs were more abundant in burned plots, but mowing reduced their abundance. Tibicen nymphs were collected almost exclusively from unburned plots. Treatment effects on herbivorous beetle larvae (Scarabaeidae, Elateridae, and Curculionidae) were variable, but nutrient additions (N or P) usually resulted in greater densities, whereas mowing usually resulted in lower densities. Our results suggest that departures from historical disturbance regimes (i.e. frequent fire and grazing) may render soils more susceptible to increased numbers of European earthworms, and that interactions between fire, aboveground biomass removal, and vegetation responses affect the structure and composition of invertebrate communities in tallgrass prairie soils.  相似文献   

15.
“Wicked” problems are those that are complex and that change when solutions are applied. Many conflicts in conservation fall into this category. The study approached the problem of how to constrain the apparent wickedness of a problem in the conservation management of a species by using simple empirical indicators to carry out iterative assessment of the risk to a population and to document how this risk evolves in relation to the addition of new data and the implementation of management actions. Effects of high levels of uncertainty within data and also concerning population structure were examined through stochastic simulation and by exploration of scenarios. Historical trends in the example used, the Steller sea lion, showed rapid declines in abundance in some regions during the 1980s. The current total population is 130,000-150,000 Steller sea lions through Alaska and British Columbia and this number has been stable since about 1990 in spite of regional differences in population dynamics. Regional differences in the sequence of changes in the number of pups and non-pups, suggested that an internal re-distribution of juveniles could have happened between 1980 and 1990. Current productivity also appears close to the long-term mean. Stochastic population projection using various scenarios showed that, based upon this history, the risk of extinction for the population has declined and is below reasonable thresholds for considering the population to be endangered. The trends in risk suggest that management actions taken since 1990 have probably been effective. Consequently, the conservation management objectives for the Steller sea lion are probably being met. The approach provides a mechanism, based upon experience and scenario analysis, for exploring future policy options and may help to constrain the debate amongst stakeholders about the cost-benefit trade-offs associated with different options.  相似文献   

16.
Nutrient distributions under no tillage (NT) compared with conventional disk-and-bed tillage (CT) management in the warm, humid region of the southeastern USA need to be assessed so that future placement, quantity, and type of fertilizers can be altered, if necessary, to efficiently match crop demands. We determined soil-profile distributions of pH, N, P, S, K, Ca, Mg, Na, Zn, Fe, Mn, and Cu to a depth of 0.9 m at the end of 8.5 years of continuous CT and NT management on a Weswood silty clay loam (fine, mixed, thermic Fluventic Ustochrept) in southcentral Texas. Most dramatic changes occurred within the 0–0.05 m depth, where soil under NT had lower pH, Fe, and Cu than under CT, but greater P, K, Zn, and Mn. Greater P and K under NT than under CT also occurred below the till-zone (0.15–0.3 m). At a depth of 0–0.3 m, soil under NT contained greater amounts of extractable P, K, Zn, Fe, Mn, and Cu than under CT. Nitrogen fertilization had little effect on nutrient distributions, except resulting in greater extractable K at 0–0.05 m and greater nitrate at 0–0.15 m. Few changes in soil-profile distributions were observed for extractable S, Ca, Mg, and Na. Long-term continuous use of NT on this fine-textured, high-fertility (except for N) soil had no apparent adverse effects on nutrient distributions relative to CT, but enhanced conservation and availability of P, K, Zn, Fe, Mn, and Cu near the soil surface where crop roots proliferate.  相似文献   

17.
Abstract

A 3-year study was carried out to investigate quality parameters in 14 tree fruit and berry species grown in southern Norway. The species were blueberry, apple, aronia, sour cherry, sweet cherry, red raspberry, strawberry, blackcurrant, gooseberry, red currant and elderberry, harvested along with wild bilberry, cloudberry and lingonberry. Significant differences between species were identified for all quality parameters. The coefficient of variation between species was lowest for pH (12.5%), dry matter (18.9%) and soluble solids (25.3%), followed by titratable acids (59.3%), total phenolics (83.8%), antioxidant capacity FRAP (85.7%) and antiradical power by the DPPH-assay (97.8%), total monomeric anthocyanins (132%) and ascorbic acid (137%). Average coefficient of variation within species were lower and ranged from 4 (pH) to 62% (ascorbic acid). Only the FRAP values were significantly affected by harvesting year with lower levels in 2004 than in 2005 and 2006. There were significant interactions between species and harvesting year for dry matter, soluble solids, pH, ascorbic acid and FRAP. The results indicate generic ranges in composition within species independent upon growing location and climate, and the composition of the tree fruits and berries is not likely to deviate from these ranges. It is concluded that desirable composition of tree fruits and berries and their products should primarily be achieved by selection among species rather than searching fors broadened variation within individual species.  相似文献   

18.
Potassium (K) fixation and release in soil are important factors in the long-term sustainability of a cropping system. Changes in K concentration and characteristics of K fixation and release in rhizosphere and nonrhizosphere soils in the rapeseed (Brassica napus L.)–rice (Oryza sativa L.) rotation were investigated using a rhizobox system. The concentrations of different forms of K in both rhizosphere and nonrhizosphere soils decreased with plants compared to without plants, regardless of K fertilizer application. Potassium uptake by crops mainly came from the rhizosphere soil. In the treatment without K fertilizer (–K), the main form of K supplied by the soil to the crops was 1.0 mol L?1 nitric acid (HNO3) nonextractable K, followed by nonexchangeable K, and then exchangeable K. In the treatment with K fertilizer (+K), the main K forms supplied by the soil to the crops were exchangeable K and nonexchangeable K. The amount and rate of K fixation after one cycle of the rapeseed–rice rotation was greater in rhizosphere soil than in nonrhizosphere soil. The amount and rate of K fixation of soil in the +K treatment were significantly less than in the –K treatment. The cumulative amounts of K released with 1.0 mol L?1 ammonium acetate (NH4OAc) and 1.0 mol L?1 HNO3 extraction increased with the increasing numbers of extractions, but the K-releasing power of soil by successive extraction decreased gradually and finally became almost constant. The release of K was less in rhizosphere soil than in nonrhizosphere soil. The release of K in the +K treatment was similar to that in the –K treatment in rhizosphere soil, but the K release in nonrhizosphere soil was greater with the +K than the –K treatment. Overall, the information obtained in this study will be helpful in formulating more precise K fertilizer recommendations for certain soils.  相似文献   

19.
Biologically enhanced dissolution offers a method to speed removal of chlorinated solvent dense non-aqueous-phase liquid (DNAPL) sources such as tetrachloroethene (PCE) and trichoroethene (TCE) from aquifers. Bioremediation is accomplished by adding an electron donor to the source zone where fermentation to intermediates leading to acetic acid and hydrogen results. The hydrogen and possibly acetic acid are used by dehalogenating bacteria to convert PCE and TCE to ethene and hydrochloric acid. Reductive dehalogenation is thus an acid forming process, and sufficient alkalinity must be present to maintain a near neutral pH. The bicarbonate alkalinity required to maintain pH above 6.5 is a function of the electron donor: 800 mg/L of bicarbonate alkalinity is sufficient to achieve about 1.2 mM TCE dechlorination with glucose, 1.7 mM with lactate, and a much higher 3.3 mM with formate. Laboratory studies indicate that in mixed culture, formate can be used as an electron donor for complete conversion to ethene, contrary to pure cultures studies indicating it cannot. Various strategies can be used to add electron donor to an aquifer for DNAPL dehalogenation while minimizing pH problems and excessive electron donor usage, including use of injection-extraction wells, dual recirculation wells, and nested injection-extraction wells.  相似文献   

20.
To evaluate the feasibility of long-term desert reforestation technology of mixed vegetation, cardon cactus (Pachycereus pringlei) seedlings from indoor and outdoor nurseries were planted in the field adjacent to one seedling of potential legume nurse trees: mesquite amargo (Prosopis articulata), yellow palo verde (Parkinsonia microphylla), and blue palo verde (Parkinsonia florida). Some of the planting holes were also supplemented with common dairy compost. Additionally, the combinations of legume tree–cactus were inoculated with either a consortium of desert arbuscular mycorrhizal (AM) fungi, plant growth promoting bacteria (PGPB; the diazotroph Azospirillum brasilense Cd, and the phosphate solubilizer Paenibacillus sp.), or a mixture of all. The field experiments were evaluated periodically during 30 months for survival and growth. Cardons reared in an outdoor screen house survived better in the field than those reared in a controlled growth chamber and hardened later outdoors. Association with any legume nurse tree increased survival and enhanced growth of untreated cardons. For cardons growing alone, application of either compost, AM fungi, and all the treatments combined increased survival. For these plants, no treatment affected plant growth during the first 3 months after transplanting. Later, all treatments, except for AM fungi, enhanced plant growth. However, only 2 years after transplanting the enhanced growth effect of AM fungi was also significant. In the presence of the legume nurse trees, transient positive effects on cardon growth were recorded. General evaluation after 30 months of cultivation showed that the treatments positively affected cardon growth when growing alone or in combination only with mesquite amargo but not with the other two legume trees. This study proposes that young legume trees have the capacity to enhance survival and growth of cardon cactus, depending on the legume cactus combination. Additional treatments such as compost or PGPB can either amplify the effect or else attenuate it.  相似文献   

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