中国三大自然区域紫花苜蓿土壤速效钾丰缺指标和推荐施钾量

为给内蒙古高原区、黄土高原区和西北荒漠绿洲区紫花苜蓿测土施肥奠定科学基础,采用零散实验数据整合法以及养分平衡-地力差减法,开展了三大自然区域紫花苜蓿土壤速效钾丰缺指标和推荐施钾量研究。结果表明,内蒙古高原区紫花苜蓿土壤速效钾第1~4级指标依次为≥342mg/kg、89~342mg/kg、24~89mg/kg和<24mg/kg,黄土高原区第1~6级指标依次为≥171mg/kg、96~171mg/kg、54~96mg/kg、30~54mg/kg、17~30mg/kg和<17mg/kg,西北荒漠绿洲区第1~4级指标依次为≥303mg/kg、140~303mg/kg、65~140mg/kg和<65mg/kg;当目标产量9~27t/hm²、钾肥利用率50%时,第1~6级土壤的推荐施钾量分别为0、54~162kg/hm²、108~324kg/hm²、162~486kg/hm²、216~648kg/hm²和270~810kg/hm²。     

黑河流域中游荒漠区沙尘暴、扬沙和浮尘监测及其与气候因子的关系

[目的] 分析黑河流域中游荒漠区沙尘暴、扬沙以及浮尘频次和时长的月变化和年变化，并分析其与主要气候因子的关系，为区域沙尘天气的早期预警和荒漠区的经营和管理提供依据。[方法] 利用黑河流域红沙窝荒漠化综合防治试验站的2010—2019年的沙尘天气监测数据和气象数据进行分析。[结果] 沙尘频次和时长主要集中在春季，其次是冬季，春冬两季的频次和时长各占全年的82.3%和79.4%。10 a间沙尘暴和扬沙频次总体变化趋势逐渐减少，而浮尘频次总体变化趋势逐年增加；沙尘时长总体变化趋势逐年增加。沙尘频次月变化与土壤湿度（10 cm）和大气湿度之间呈极显著负相关（p<0.01），与风速之间呈极显著正相关（p<0.01）。扬沙年际发生频次与土壤温度（5 cm）之间呈显著负相关（p<0.05），与大气温度之间呈极显著负相关（p<0.01）。[结论] 近10 a来，黑河流域中游荒漠区的沙尘天气主要发生在春季和冬季，破坏性较大的沙尘暴和扬沙逐年减少，而浮尘逐年增加。沙尘频次的月变化主要影响因素是浅层土壤湿度、大气湿度和风速。春季的浅层土壤湿度影响了沙尘暴和扬沙年际频次变化，浅层土壤温度影响了浮尘年际频次变化；冬季的浅层土壤温湿度和降水量影响了沙尘暴的年际频次变化，浅层土壤温度和大气温度影响了扬沙的年际频次变化。     

基于SEBAL模型评估干旱半干旱区人工灌丛植被对陆表蒸散的影响

评估人工灌丛植被重建对干旱半干旱区陆地生态系统蒸散的影响,不仅能揭示植被变化与水文过程的耦合机理,又可为区域生态治理与水资源管理提供科学指导。该研究利用Landsat-8OLI/TIR遥感影像及气象数据等驱动SEBAL模型,反演宁夏盐池县的年内不同日期的陆表蒸散,结合目视解译选取的人工灌丛区与对照草地,评估了人工灌丛植被对陆表蒸散的影响。结果表明:1)SEBAL模型的蒸散反演精度与站点观测结果较为一致,可用于干旱半干旱区蒸散反演及空间特征研究;2)盐池县人工灌丛植被区日平均蒸散为1.20mm/d,高于对照草地1.17mm/d的日平均蒸散量,即干旱半干旱区人工种植灌木林增加了生态系统水分消耗,但不同季节和不同生物地理条件下的蒸散增强作用存在差异,蒸散增强在8月份最大,而3、4月份呈现负效应;3)人工灌丛的密度越大、植被盖度越高,对陆表蒸散的增强作用越强,特别在NDVI0.4的高盖度情况下蒸散增强作用更加明显。由此可知,在水资源紧缺的干旱半干旱区开展以灌木树种为主的植被重建需在合理的生态水文阈值范围内开展,才能构建出稳定可持续的人工生态系统。     

多功能土壤改良剂对河西内陆灌区棕漠土的改良效果

[目的]解决棕漠土保水肥能力弱,有机质含量低,制种玉米产量低而不稳的疑难问题,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]选择甘肃省酒泉市肃州区棕漠土,采用田间试验方法,进行多功能土壤改良剂配方筛选及对棕漠土改良效果研究。[结果]多功能土壤改良剂最佳配比为:有机生态肥∶保水剂∶制种玉米专用肥∶聚乙烯醇为0.978 3∶0.000 9∶0.019 6∶0.001 2。多功能土壤改良剂最佳施用量为68.75t/hm~2,制种玉米理论产量为6.64t/hm~2。施用多功能土壤改良剂与传统化肥比较,棕漠土总孔隙度、毛管孔隙度、非毛管孔隙度、团聚体、饱和持水量、毛管持水量、非毛管持水量分别增加22.75%,22.76%,22.74%,9.50%,22.75%,22.76%和22.74%;有机质、CEC、碱解氮、速效磷和速效钾增加35.01%,21.64%,0.63%,2.26%和2.09%;真菌、细菌和放线菌分别增加93.97%,35.35%,20.78%;蔗糖酶、脲酶、磷酸酶和多酚氧化酶分别增加61.82%,44.64%,40.00%和64.29%;制种玉米增产值和施肥利润增加39.23%和31.82%。[结论]施用多功能土壤改良剂,能有效地改善棕漠土理化性质和生物学性质,提高制种玉米产量。     

艾比湖湿地不同盐渍化土壤粒度组成及可蚀性研究

为了研究内陆干旱区不同盐渍化土壤的粒径组成及其可蚀性的空间分布,在不同盐渍化程度上探讨其与土壤中盐分含量的相互关系,本研究以新疆维吾尔自治区艾比湖湿地为研究靶区,利用2015年5月获取的66个表层土壤样品,对土壤的粒度组成、含盐量、分形维数和可蚀性因子K值进行了研究。结果表明:样品中盐土占比达到59.09%,平均含盐量达131.59 g/kg,研究区内盐渍化现象既普遍又严重;土壤颗粒以粉粒和砂粒为主,随着盐渍化程度的加剧黏粒含量不断增加,砂粒含量则相反;土壤颗粒的分形维数D值介于2.14~2.60,平均值为2.45;随着盐渍化程度加剧,分形维数逐渐变大,K值也随之逐渐增大,盐土的K值最大达0.093;土壤可蚀性因子K值与含盐量的相关性较高(r=0.596**),在一定程度上可以说明,土壤的含盐量水平越高,K值越大,越容易被侵蚀。     

水氮控制对荒漠草原中小型土壤动物群落的影响

【目的】了解水氮控制对荒漠草原中小型土壤动物的影响,进而从土壤动物角度解读全球变化对荒漠草原的生态效应。【方法】2014年植物生长季,以内蒙古自治区乌兰察布市四子王旗短花针茅荒漠草原为研究对象,设置对照(CK,自然降雨状态)、减雨(R)、增雨(W)、施氮(N)、减雨施氮(R+N)和增雨施氮(WN)6个处理,观测不同处理中小型土壤动物群落和土壤环境参数的变化。【结果】短花针茅荒漠草原共捕获中小型土壤动物333 079.5只/m~2,隶属于节肢动物门的4纲10目47科,主要为弹尾纲(Collembola)、蛛形纲(Arachnida)和昆虫纲(Insecta);优势类群为疣虫兆科(Neanoridae)和等节科(Isotomidae),优势类群和常见类群构成了研究样地中小型土壤动物群落的主体。增雨、增雨施氮有助于提高短花针茅荒漠草原中小型土壤动物个体密度,减雨、减雨施氮处理减少中小型土壤动物个体密度,且水氮交互作用对中小型土壤动物个体密度影响表现显著,而对类群数无显著影响。短花针茅荒漠草原中小型土壤动物具有明显表聚性,各处理下0~10cm土层个体密度和类群数显著高于10~20cm土层(P0.05)。【结论】在未来降雨增加和氮沉降的全球变化背景下,中小型土壤动物个体密度的变化可能会更大。     

Needle blight caused by Dothistroma pini in Slovakia: distribution,host range and mating types

Dothistroma needle blight (DNB) has been observed in Slovakia during the last two decades. Up until 2017, Dothistroma septosporum has only been detected and molecularly confirmed to cause DNB in Slovakia. Here, we report the detection of Dothistroma pini at six localities around Slovakia, representing different plantation types. Four pine species (Pinus sylvestris, P. nigra, P. mugo and P. jeffreyi) were confirmed as hosts of D. pini in Slovakia, of which only P. mugo has been previously reported as host in Slovakia. Three gene regions (ITS, EF1 –α, and ß-tubulin) of each of the 13 isolates were sequenced and assigned as D. pini. Based on ITS sequences, the studied isolates represent the haplotypes Dp_HAP.1, Dp_HAP.2. Both mating types were detected but at different localities. Our results suggest that in addition to D. septosporum, D. pini may contribute to DNB also in Slovakia.     

Breaking the ice: the introduction of biofouling organisms to Antarctica on vessel hulls

1. Few reports exist that describe marine non‐native species in the Southern Ocean and near‐shore waters around the Antarctic continent. Nevertheless, Antarctica's isolated marine communities, which show high levels of endemism, may be vulnerable to invasion by anthropogenically introduced species from outside Antarctica via vessel hull biofouling.
2. Hull surveys of the British Antarctic Survey's RRS James Clark Ross were undertaken between 2007 and 2014 at Rothera Research Station on the Antarctic Peninsula (Lat. 67°34'S; Long. 68°07'W) to investigate levels of biofouling. In each case, following transit through scouring sea‐ice, over 99% of the vessel hull was free of macroscopic fouling communities. However, in some surveys microbial/algal biofilms, balanomorph barnacles and live individuals of the cosmopolitan pelagic barnacle, Conchoderma auritum were found in the vicinity of intake ports, demonstrating the potential for non‐native species to be transported to Antarctica on vessel hulls.
3. Increasing ship traffic volumes and declining duration of sea ice in waters to the north and west of the Antarctic Peninsula mean the region may be at increased risk of non‐native species introductions. Locations at particular risk may include the waters around popular visitor sites, such as Goudier Island, Neko Harbour, Whalers Bay, Cuverville Island and Half Moon Island, and around northern peninsula research stations.
4. Simple and cost‐effective mitigation measures, such as intentionally moving transiting ships briefly through available offshore sea ice to scour off accessible biofouling communities, may substantially reduce hull‐borne propagule pressure to the region. Better quantification of the risk of marine non‐native species introductions posed by vessel hulls to both Arctic and Antarctic environments, as sea ice patterns and shipping traffic volumes change, will inform the development of appropriate regional and international management responses.

Copyright © 2016 The Authors. Published by Wiley Periodicals, Inc.     

制种玉米连作恒量施磷对灌漠土与潮土中磷素利用的影响

[目的]研究恒量外源磷施用对玉米种子生产的影响,为合理施磷提供依据。[方法]通过大田定位与实验室分析相结合,选用河西走廊石灰性潮土及灌漠土定位施肥。[结果]制种玉米连作8a,恒量磷二铵525kg/(hm~2·a)施用,除无机态二钙磷(Ca_2-P)外,2种不同土类总磷(T-P)、速效性磷(Av-P)、总无机磷(T-IP)、总有机磷(T-OP),以及其他各分级无机、有机磷组分均显著增加。无机磷占全磷总量65.2%~70.2%,有机磷占全磷总量6.5%~11.4%。无机磷中十钙磷(Ca_(10)-P)八钙磷(Ca8-P)铝磷(Al-P)铁磷(Fe-P)闭蓄态磷(O-P)。有机磷中活性有机磷(MLO-P)高稳性(HRO-P)中稳性有机磷(MROP)活性有机磷(LO-P)。随连作年限增加,灌漠土Ca_(10)-P在连作第5a达到最大,Al-P,O-P均持续增加;潮土Ca_(10)-P持续增加,Fe-P,O-P在连作第5a达到最大,磷增加量为3.94%~37.28%。0—60cm土层,两种土类无机磷各组分含量均呈现由表层至下层递减特点,但不同分级磷在不同土层所占比例不同,Ca_(10)-P,Al-P,O-P,MRO-P底聚,Ca_2-P,HRO-P表聚,制种玉米连作生产8a,磷肥最大表观利用率为4.89%,磷素活化系数2%,外源磷肥以174.3kg/(hm~2·a)残余在土壤中。[结论]制种玉米连作,总磷转化率低,磷素移动缓慢,大部分以溶解性较低的磷素形态在土壤表层积累,但随连作年限增加,土壤对磷素的固持及转化率下降,表现底聚趋势,对生态环境健康存在极大风险,应减量或停止施磷。潮土磷肥施用应采取更加合理措施。