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1.
六盘山辽东栎、少脉椴天然次生林夏季蒸散研究   总被引:8,自引:2,他引:6  
2004年8~9月份,利用热扩散技术,结合微型蒸渗仪和水文学方法,研究了辽东栎、少脉椴次生林蒸散组成及其与林分结构的关系.结果表明,辽东栎和少脉椴树干的液流密度在“相对静止期”内比较稳定和微弱,其值在0.05 μl·cm-2·min-1以下;在“活跃期”内树干液流密度上升较快,并呈单峰、双峰或多峰曲线,其值在0.25 μl·cm-2·min-1以下;两树种单株蒸腾量有明显的种间差异,前者晴天和阴雨天单株蒸腾量分别为5.31和2.48 L·d-1,为后者的2.35倍和3.75倍.林下灰木旬子和黄刺玫蒸腾速率日均值接近,分别为0.331和0.321 g·g-1·h-1.次生林日均蒸散量1.45 mm·d-1,其中蒸腾量0.72 mm·d-1、土壤蒸发量0.19 mm·d-1、林冠截留量0.54 mm·d-1,各占总量的49.6%、13.3%和37.1%.乔、灌木树种组成对次生林蒸腾量影响的表现不同,前者表现为个体蒸腾量的种间差异,而后者取决于单位林地面积上各树种的叶量.乔木层、灌木层和草本层(含土壤层)日均蒸散量分别为0.96、0.30和0.19 mm·d-1,各占总量的65.8%、20.9%和13.3%,说明乔木层对林分日蒸散量大小起主要作用,灌木层次之,草本和土壤蒸发量的贡献最小.  相似文献   

2.
土壤水分对返青期断根冬小麦补偿效应的影响   总被引:2,自引:1,他引:1  
通过盆栽试验研究了不同土壤水分条件下返青期断根冬小麦的补偿效应.结果表明,断根小麦的早期生长受到抑制,叶面积在返青 拔节期间显著下降,到开花期能恢复至对照水平.高水分条件下断根小麦拔节期的叶绿素荧光参数包括表观光合电子传递速率、实际光化量子产量、光化学淬灭系数、非光化学淬灭值均显著大于对照,开花后单茎干物质积累为0.81 g,显著大于对照(0.56 g),花后干物质积累系数比对照提高了38.79%,断根小麦根量虽有所下降但差异不显著;低水分条件下断根小麦的叶绿素荧光参数和花后干物质积累与对照之间没有显著差异,但断根小麦的根系生物量(7.83 g·pot-1)显著小于对照(9.77 g·pot-1).土壤水分对断根小麦的地上生物量和籽粒产量的补偿效应没有显著影响.断根处理的冬小麦在两种土壤水分条件下均显著降低了耗水量,在整个生育期,高水分条件下冬小麦断根处理可节水2 000 ml左右,水分利用效率为1.97 g·kg -1,显著大于对照的1.70 g·kg -1;低水分条件下也可节水1 500 ml左右,水分利用效率虽有所提高,但未达到显著性差异.  相似文献   

3.
农田蒸散是农田水分消耗的主要方式,是农田管理和规划必须考虑的重要因素之一。本试验在郑州农业气象试验站开展,用Penman-Monteith公式计算了2017和2018年两年冬小麦越冬期-成熟期的参考作物蒸散量,利用大型称重式蒸渗仪观测了充分灌水(T2)和自然降水(T1)两种状况下冬小麦农田的实际蒸散量,进而计算充分灌溉下冬小麦的作物系数和自然降水条件下的冬小麦实际作物系数,并分析它们的变化规律及其与气象要素的相关关系。结果表明:不同水分条件下冬小麦农田蒸散量均呈现先升高后降低的单峰变化趋势,其中T2处理的蒸散量和波动幅度明显高于T1处理;冬小麦试验观测时期内,T2、T1处理两年总蒸散量均值分别为535.8和256.4 mm,日均蒸散量分别为3.7和1.7 mm;不同发育期日均蒸散量均是孕穗、抽穗期最高,越冬期最低;冬小麦作物系数明显高于自然降水条件下的实际作物系数,总体上均呈现降低-升高-降低的变化趋势; T1处理实际作物系数与空气湿度相关性最好,与平均气温相关性最差; T2处理作物系数与平均气温、总辐射和风速均有较好相关性,而与空气湿度相关性较差。  相似文献   

4.
半干旱区不同垄沟集雨种植马铃薯模式对土壤蒸发的影响   总被引:13,自引:0,他引:13  
通过垄沟集雨种植马铃薯试验,研究了不同垄沟集雨种植模式对土壤蒸发的影响.结果表明,在马铃薯全生育期,垄上覆盖塑料薄膜(CR)处理土壤蒸发量为122.9~165 mm,垄上原土夯实不覆膜(UR)处理土壤蒸发量为90.9~101.2 mm,无垄带状种植(CK) 土壤蒸发量为80.7 mm.其中,覆膜垄处理CR60在马铃薯成熟期土壤蒸发强度最大,达2.6 mm·d-1,平均为1.46 mm·d-1,而对照的土壤蒸发强度为0.65 mm·d-1;不覆膜土垄处理(UR30)土壤蒸发强度苗期最小,只有0.2 mm·d-1,平均为0.39 mm·d-1,而对照的土壤蒸发强度为0.58 mm·d-1.在马铃薯生长的现蕾期和开花期,水面蒸发量最大,日平均水面蒸发量分别为8.3和9.0 mm,与土壤蒸发不同步.马铃薯成熟期,各处理棵间土壤蒸发量都达到最大值.覆膜垄蒸发量最大,集雨效果显著,所以应采取抑制土壤蒸发措施,以便进一步提高水分利用效率.  相似文献   

5.
黄土高原吕二沟流域侵蚀产沙对土地利用变化的响应   总被引:11,自引:0,他引:11  
研究了甘肃天水黄土高原吕二沟流域土地利用变化对流域产沙的影响.结果表明,与1982年相比,1989年该流域林草面积增加约5%,梯田增加2.09%,裸地略有增加,坡耕地减少约1.5%,灌木林略有减少.1998~2000年,在植被覆被增加、陡坡坡耕地减少情况下,随降水增多,其减沙效应明显,如803 mm和786 mm降雨条件下,后期较前期(1982~1989年)分别减少85 326 t和52 937 t,降水较少,减沙效应较不明显;从年内含沙量变化来看,后期土地利用的减沙效应主要集中在5~10月,与降水的季节分配一致,各月降水越多,月日均含沙量减少越多,50 mm的月降水月日均含沙量减少6 kg·m-3,100 mm月降水月日均含沙量减少12 kg·m-3.两期土地利用在重现期小于5年时,后期土地利用洪水含沙量较前期稍大,主要由于两期的降水频率分布曲线不一致;若两期降水频率分布曲线一致,则同一频率降水产洪的洪水含沙量后期将小于前期.  相似文献   

6.
 依托FACE(Free-air CO2 enrichment)研究平台, 利用特制分根集气生长箱, 采用静态箱-GC(Gas chromatography)法, 连续两年研究 了大气CO2浓度升高和不同氮肥水平对冬小麦拔节期、孕穗抽穗期和灌浆末期的根系呼吸及生物量的影响。两季结果表明, CO2浓度升高和高氮 肥量均不同程度地增加了3个阶段的地上部和地下部的生物量, 这有利于增加根茬的还田量; CO2浓度升高对冬小麦不同生长阶段的根系呼吸影 响不同, 在拔节期影响较小;孕穗抽穗期显著增加了根系呼吸, 2004~2005季分别增加33.8%(148.1 mg N&;#8226;kg-1 干土, HN)和43.9%(88.9 mg N&;#8226;kg-1 干土, LN), 2005~2006季分别为23.8%(HN)和28.9%(LN); 而灌浆末期显著降低了根系呼吸, 2004~2005季分别降低31.4%(HN)和23.3% (LN), 2005~2006季分别为25.1%(HN)和18.5%(LN); 高施氮量比低施氮量促进了根系呼吸; 随着作物生长根系呼吸与地下生物量呈显著线性负相 关, 高CO2环境中的R2变小,表明随着作物生长发育高CO2浓度降低了作物根系呼吸与地下部生物量积累间的相关性.  相似文献   

7.
地面覆盖和保水剂对冬小麦生长和降水利用的影响   总被引:18,自引:0,他引:18  
在河南省西部丘陵旱耕地上,研究了保水剂(0、45、60 kg·hm-2)、秸秆覆盖(3000和6000 kg·hm-2)和地膜覆盖(<0.005 mm)对冬小麦生长发育、土壤水分和降水利用的影响.结果表明:3种措施均能促进冬小麦生长,改善土壤水分和养分状况,提高冬小麦产量和降水利用效率,特别是保水剂与秸秆覆盖、保水剂与地膜覆盖相结合效果更显著.与对照相比,不同措施使冬小麦不同生育期土壤含水量提高0.1%~6.5%,拔节期前地膜覆盖处理保墒效果最佳,拔节期后保水剂处理保墒效果较佳,扬花期和灌浆期墒情最差.不同措施使冬小麦产量比对照提高2.6%~20.1%,并以秸秆覆盖+保水剂处理最佳,增产14.2%~20.1%;其次为地膜+保水剂处理,平均增产11.9%.不同措施降水利用效率存在相同趋势,比对照提高0.4~3.2 kg·mm-1·hm-2.表明地面覆盖和保水剂的应用改善了农田土壤水分状况和养分状况,提高了降水利用率,从而促进了冬小麦分蘖,提高了穗粒数和千粒重.  相似文献   

8.
刺参对浅海筏式贝类养殖系统的修复潜力   总被引:3,自引:0,他引:3  
浅海筏式养殖滤食性贝类产生大量的粪便和假粪(总称生物沉积物),对海水养殖环境产生一系列影响;而沉积食性海参能够有效清除颗粒有机物,在海水养殖系统中扮演“清道夫”的生态角色.为评估刺参在浅海筏式贝类养殖系统中的生物修复潜力,本文在不同季节现场研究了贝 参混养模式下刺参对贝类生物沉积物的摄食及生长和排泄特征.结果表明: 刺参能够在新设计的养殖设施中与滤食性贝类混养,最大生长率达0.34%·d-1; 并可通过摄食有效清除贝类生物沉积物, 摄食率为0.1746 g·g-1·d-1(夏季,21.2 ℃)、0.0989 g·g-1·d-1(秋季,19.2 ℃)和0.0050 g·g-1·d-1(冬季,7.7 ℃);刺参主要通过排泄溶解形态的NH4+N和PO43- -P来促进沉积物中营养盐的再生,其排泄率也呈现明显的季节变化.基于现场试验数据,估算了刺参在桑沟湾的生物修复潜力, 刺参与贝类混养可摄食4.5~159.6 kg·hm-2·d-1生物沉积物、排泄1 382.5~3 678.1 mmol·hm-2·d-1NH4+ -N及74.6~335.7 mmol·hm-2·d-1PO43--P.表明刺参对浅海筏式贝类养殖系统具有较大的生物修复潜力,贝-参混养模式不仅能够取得较大的生态效益,而且能显著增加养殖生产的经济效益.  相似文献   

9.
DNDC模型在农田氮素渗漏淋失估算中的应用   总被引:12,自引:0,他引:12  
采用田间原装渗漏计测定了山东省济南市典型种植模式下,2008年冬小麦整个生长季水分和 氮素淋失量,并利用该数据对DNDC(DeNitrification-DeComposion)模型进行检验和敏感性分析.结果表明:模型对该地区农田土壤水分运动的模拟效果较好,模拟结果的精度总体上可以接受,但对氮素淋失量的模拟结果存在一定偏差,冬小麦整个生长季的氮素淋失量模拟值(18.35 kg N·hm-2)比实测值(14.89 kg N·hm-2)高3.46 kg N·hm-2,相对偏差在20%左右,模型参数尚需作进一步调整.模型敏感性分析显示,农田氮素淋失更易受到灌水量和施肥量的影响.DNDC模型在该地区有一定的适用性.  相似文献   

10.
黄土旱塬区冬小麦不同施肥处理的土壤呼吸及土壤碳动态   总被引:16,自引:0,他引:16  
依据黄土旱塬区黑垆土上中国科学院长武站长期定位试验 (始于1984年),于2008年3月到6月,测定了冬小麦连作系统中返青期、拔节期、抽穗期、灌浆期和收获期土壤呼吸日变化、生育期变化以及土壤可溶性有机碳(Dissolved organic C, DOC)和微生物量碳(Soil microbial biomass C, MBC),研究了施肥措施对土壤呼吸、DOC和MBC的影响以及土壤呼吸与碳组分之间的关系.研究涉及6个处理:休闲地(F)、不施肥(CK)、有机肥(M)、氮肥(N)、氮磷肥(NP)和氮磷有机肥(NPM).结果表明,冬小麦连作系统中土壤呼吸的日变化格局呈单峰曲线,最高值出现在12:00左右(拔节期)和14:30左右(成熟期),最小值出现在0:00~3:00之间或6:00左右;冬小麦土壤呼吸速率拔节期最高,其次是灌浆后期,抽穗期最低;不同施肥条件下,各生育期土壤呼吸速率大小顺序:NPM>M>NP>N>CK>F.土壤水分亏缺是导致抽穗期和灌浆期土壤呼吸速率降低的重要原因.各施肥处理DOC含量高低顺序为灌浆期>抽穗期>成熟期>返青期>拔节期;除M,NPM处理MBC含量拔节期>灌浆期外,各施肥处理MBC含量高低顺序为成熟期>抽穗期>灌浆期>拔节期>返青期.同一处理不同生育期土壤呼吸速率与DOC,MBC的相关性较低,但同生育期不同施肥处理土壤呼吸与土壤有机碳组分间存在显著的相关性.以F处理土壤呼吸为基础,估算CK、N和NP处理生育期根系对土壤呼吸的平均贡献率依次为36%、45%和54%.  相似文献   

11.
Crop yield and water use efficiency (WUE) in a wheat-maize double cropping system are influenced by short and uneven rainfalls in the North China Plain (NCP), A 2-year experiment was conducted to investigate the effects of irrigation on soil water balance, crop yield and WUE to improve irrigation use efficiency in the cropping system, Soil water depletion (~SWS) by crop generally decreased with the increase of irrigation and rainfall, while ASWS for the whole rotation was relatively stable among these irrigation treatments, High irrigations in wheat season increased initial soil moisture and ASWS for subsequent maize especially in the drought season, Initial soil water influenced mainly by the irrigation and rainfall in the previous crop season, is essential to high yield in such cropping systems, Grain yield decreased prior to evapotranspiraUon (ET) when ET reached about 300mm for wheat, while maize showed various WUEs with similar seasonal ET, For whole rotation, WUE declined when ET exceeded about 650 mm, These results indicate great potential for improving irrigation use efficiency in such wheat-maize cropping system in the NCP, Based on the present results, reasonable irrigation schedules according to different annual rainfall conditions are presented for such a cropping system.  相似文献   

12.
Crop yield and water use efficiency (WUE) in a wheat-maize double cropping system are influenced by short and uneven rainfalls in the North China Plain (NCP). A 2-year experiment was conducted to investigate the effects of irrigation on soil water balance, crop yield and WUE to improve irrigation use efficiency in the cropping system. Soil water depletion (△SWS)by crop generally decreased with the increase of irrigation and rainfall, while △SWS for the whole rotation was relatively stable among these irrigation treatments. High irrigations in wheat season increased initial soil moisture and △SWS for subsequent maize especially in the drought season. Initial soil water influenced mainly by the irrigation and rainfall in the previous crop season, is essential to high yield in such cropping systems. Grain yield decreased prior to evapotranspiration(ET) when ET reached about 300 mm for wheat, while maize showed various WUEs with similar seasonal ET. For whole rotation, WUE declined when ET exceeded about 650 mm. These results indicate great potential for improving irrigation use efficiency in such wheat-maize cropping system in the NCP. Based on the present results, reasonable irrigation schedules according to different annual rainfall conditions are presented for such a cropping system.  相似文献   

13.
栽培模式、施氮和品种对冬小麦冠层结构和产量的影响   总被引:4,自引:2,他引:2  
在黄土高原南部半湿润易早区土垫旱耕人为土上进行大田试验,研究氮肥、品种和栽培模式对冬小麦叶面积指数(IAI)和透光率(DIFN)及产量的影响。结果表明,小麦生长过程中IAI先增大后减小.在开花期最大。成熟期最小。施氮能够显著增加IAI;DIFN的变化规律与LAI相反。不同品种间IAI和DIFN差异显著。全程覆膜和覆膜150d的LAI极显著大于常规栽培、集雨面栽培和三密一稀栽培模式,DIFN与此相反;施氮后籽粒产量极显著增加。在不同栽培模式下,以全程覆膜、覆膜150d和集雨面栽培模式的产量较高,但从维持土壤质量角度考虑,则覆膜150d和集雨面2种栽培模式优于其它几种栽培模式;从冠层结构特征分析,这2种栽培模式更有利于增加群体光合能力。  相似文献   

14.
本研究基于5年的耕作定位试验,设置深耕(DT)、深耕有机肥(DTF)、浅耕(ST)、浅耕有机肥(STF)、免耕(NT)和免耕有机肥(NTF)处理,以期通过改良耕层土壤结构,优化小麦冠层结构特性.结果表明: 同一耕作处理下,增施有机肥可降低土壤容重、提高土壤孔隙度,提高20~40 cm土层2~5和0.25~2 mm粒级土壤团聚体含量,降低>5 mm粒级团聚体含量、>0.25 mm粒级团聚体的平均质量直径(MWD)和几何平均直径(GMD).与其他处理相比,NTF处理改善了0~20 cm土层土壤容重、增加土壤孔隙度;DTF处理降低了40~60 cm土壤容重和>0.25 mm粒级机械团聚体的稳定性,增加了土壤透气性.花后各时期,有机肥处理的叶片角度指数降低,叶面积指数(LAI)和旗叶净光合速率(Pn)提高.STF处理的角度指数最低,DTF处理的Pn最高,显著大于其他处理.通径分析表明,自变量容重、孔隙度、>0.25 mm粒级团聚体的数量(R0.25)和MWD对因变量角度指数、LAI和Pn的直接通径系数均达到极显著水平.0~20 cm土层,MWD值增大有利于Pn和LAI的提高;20~40 cm土层,土壤容重在一定范围内的增加可优化叶夹角,提高冠层透光率;40~60 cm土层,高的土壤容重和低的孔隙度限制了LAI和Pn的增加.综上,豫中补灌区增施有机肥下的深耕或浅耕处理有利于改良土壤结构、增加土壤通透性,优化冠层结构,提高冠层受光率、叶面积指数和光合速率.  相似文献   

15.
王海波  马明国 《生态学报》2014,34(19):5617-5626
遥感数据具有很好的时空连续性,它是区域蒸散发通量估算的有效方法。引入了一个简单的具有生物物理基础的Penman-Monteith(P-M)模型,分别利用黑河流域高寒草地阿柔站和干旱区农田盈科站2008—2009年的气象数据和MODIS(Moderate Resolution Imaging Spectroradiometer)叶面积指数(LAI),实现了2008—2009年日蒸散发的估算,并同时实现了对植被蒸腾和土壤蒸发的分别估算。结果表明,利用P-M公式模拟的蒸散发与实测的蒸散发具有较好的一致性,日蒸散发模拟的决定系数(R2)超过0.8。估算的高寒草甸和干旱区农田玉米全年平均的蒸腾分别为0.78 mm/d和1.20 mm/d,分别占总蒸散发的60%和61%,土壤蒸发分别为0.53和0.77 mm/d,占总蒸发的40%和39%。可见两种生态系统的作物蒸腾均强于土壤蒸发,同时农田玉米蒸腾强于高寒草甸蒸腾。研究结果证明了基于遥感的P-M公式可以很好地实现对高寒草地和干旱区农田生态系统蒸散发的估算。通过考虑土壤水分变化对气孔导度的影响,可以提高模型对农田蒸散发的模拟精度。  相似文献   

16.
绿洲生态条件下春小麦蒸发蒸腾特征及其影响因子   总被引:13,自引:0,他引:13       下载免费PDF全文
 在河西走廊临泽绿洲北部试验区,对春小麦进行3种水分处理并同时观测了全生育期内的蒸发蒸腾(ET)及环境中各生态因子和植物生理指标。结果表明:当年全生育期内,春小麦ET在充分供水条件下为593mm;在中等供水条件下为365mm;在少量供水条件下为280mm。其日蒸散量分别为5.5mm,3.4mm和2.8mm。讨论了影响ET和植物蒸腾的各植物生理指标和环境因子,发现在植物诸指标与蒸腾相关程度的顺序为:叶片水势、气孔导度和叶温(充分供水)及叶片水势、叶温和气孔导度(水分胁迫)。在环境诸因子中与ET的相关程度顺序是:有效光合辐射、净辐射、20cm土温、大气饱和水汽压差,15cm土温、气温、10cm土温、土壤表面温度及5cm土温。  相似文献   

17.
张晓龙  沈冰  权全  董樑  田开迪 《生态学杂志》2016,27(8):2551-2560
基于对半湿润易旱区的渭河平原农田2013—2014年冬小麦生长期土壤呼吸(SR)及环境因子和生物因子的观测,研究了冬小麦土壤呼吸日变化、季节变化特征,综合分析了温度(T)、土壤含水量(W)、总初级生产力(GPP)和叶面积指数(LAI)对土壤呼吸的影响.结果表明: 冬小麦土壤呼吸日变化呈单峰型,呼吸速率变化范围为1.5~6.94 μmol CO2·m-2·s-1,最大值出现在12:00—14:00;温度是影响土壤呼吸日变化的驱动因子,其中地表温度(Ts)能解释土壤呼吸时间变异的80.9%;土壤呼吸速率与温度的昼夜变化对应关系呈顺时针近椭圆曲线.冬小麦土壤呼吸速率从出苗后到冬季呈下降趋势,在冬季时保持较低水平,进入返青期后迅速增加,在抽穗期和灌浆期达到最大,成熟期后有所下降,变化范围为0.65~4.85 μmol CO2·m-2·s-1;土壤呼吸季节变化与温度、土壤含水量、GPP、LAI均呈显著(P<0.01)正相关关系;土壤温度和水分是影响土壤呼吸季节变化的关键因素,使用复合模型SR=e(a+bT5 cm+cW10 cm+dW10 cm2),可以解释土壤呼吸时间变异的82.6%,比单因子模型(不超过65.7%)的解释能力显著提高.经模型计算,该区域2013—2014年冬小麦生长期平均土壤呼吸速率为1.67 μmol CO2·m-2·s-1.  相似文献   

18.
Reynolds  James F.  Kemp  Paul R.  Tenhunen  John D. 《Plant Ecology》2000,150(1-2):145-159
We used the patch arid land simulator (PALS-FT) – a simple, mechanistic ecosystem model – to explore long-term variation in evapotranspiration (ET) as a function of variability in rainfall and plant functional type (FT) at a warm desert site in southern New Mexico. PALS-FT predicts soil evaporation and plant transpiration of a canopy composed of five principal plant FTs: annuals, perennial forbs, C4 grasses, sub-shrubs, and evergreen shrubs. For each FT, the fractional contribution to transpiration depends upon phenological activity and cover as well as daily leaf stomatal conductance, which is a function of plant water potential, calculated from root-weighted soil water potential in six soil layers. Simulations of water loss from two plant community types (grass- vs. shrub-dominated) were carried out for the Jornada Basin, New Mexico, using 100 years of daily precipitation data (1891–1990). In order to emphasize variability associated with rainfall and fundamental differences in FT composition between communities, the seasonal patterns cover of perennials were held constant from year to year. Because the relative amount of year to year cover of winter and summer annual species is highly variable in this ecosystem, we examined their influence on model predictions of ET by allowing their cover to be variable, fixed, or absent.Over the entire 100-yr period, total annual ET is highly correlated with total annual rainfall in both community types, although T and E alone are less strongly correlated with rainfall, and variation in transpiration is nearly 3 times greater than evaporation and 2 times greater than variation in rainfall (CV of rainfall = 35%). Water use shows a relatively high similarity between the grass- and shrub-dominated communities, with a 100-yr average T/ET of 34% for both communities. However, based on a year-by-year comparison between communities, T/ET was significantly greater in the grass-dominated community, reflecting the fact that over the long term more than half of the rain occurs in the summer and is used slightly more efficiently (T¿E) by the C4-grass community than the shrub community, although we found some rainfall patterns that resulted in much greater T/ET in the shrub community in a given year. Percent of water lost as transpiration (T/ET) suggests that while there is a general trend toward increased T/ET with rainfall in both community types, T/ET is extremely variable over the 100-yr simulation, especially for normal and below normal amounts of rainfall (T/ET values range from 1 to 58% for the grass-dominated site and 6 to 60% for the shrub-dominated site).These predictions suggest that because of the relatively shallow distribution of soil water, there is little opportunity for vertical partitioning of the soil water resource by differential rooting depths of the plant FTs, in contrast to the two-layer hypothesis of Walter (1971). However, functional types may avoid competition by keying on particular `windows' of moisture availability via differences in phenologies. We found very little differences in average, long-term model predictions of T, E, and ET when annual plant cover was variable, fixed, or absent. The results of our simulations help reconcile some of the disparate conclusions drawn from experimental studies about the relative contribution of transpiration vs. evaporation to total evapotranspiration, primarily by revealing the great year-to-year variability that is possible.  相似文献   

19.
有限供水下冬小麦全程耗水特征定量研究   总被引:5,自引:1,他引:4  
张兴娟  薛绪掌  郭文忠  李亮  王志敏 《生态学报》2014,34(10):2567-2580
为明确冬小麦不同水分条件下全生育过程日耗水及阶段耗水特征,在北京地区利用蒸渗仪系统连续监测了几种灌溉处理(W4:起身水+孕穗水+开花水+灌浆水;W2:拔节水+开花水;W1:拔节水;W0:无灌水)耗水动态变化。结果表明:冬小麦全生育期的耗水动态可分为3个阶段:(1)播种至11月底的冬前阶段,这个阶段日耗水量波动明显,一般低于3 mm/d;(2)12月上旬至来年2月底的冬季阶段,这个阶段日耗水量低于0.4 mm/d,且波动很小;(3)3月初小麦返青至收获的春后生长阶段,这个阶段日耗水量总体上是一个先升高后降低的过程,但波动很大,每次灌水都会引起1个日耗水高峰的出现。耗水日变化呈单峰或双峰曲线,高峰出现在正午前后,高峰值因灌水处理而有明显差异,灌水多则耗水峰值显著升高,而夜间耗水量及其在不同处理间差异均很小。拔节至成熟期是冬小麦耗水的主要时期,该期耗水占总耗水60%以上。减少灌溉会增加土壤贮水消耗,但降低了总耗水量。综合比较表明,在有限灌溉下,拔节水和开花水组合是高产和高水分效率相统一的灌溉模式。  相似文献   

20.
Asseng  S.  Turner  N. C.  Keating  B. A. 《Plant and Soil》2001,233(1):127-143
Water-use efficiency (WUE [g grain yield m–2 mm–1 ET]) and nitrogen-use efficiency (NUE [ g grain yield g–1 Napplied]) are important measures that can affect the productivity of crops in different environmental systems. However, measurement and interpretation of WUE and NUE in the field are often hampered by the high degree of complexity of these systems due to season-to-season variability in rainfall, the variation in crop responses to soil types and to agronomic management. To be able to guide agronomic practice, experimentally-derived measurements of WUE and NUE need to be extrapolated across time and space through appropriate modelling. To illustrate this approach, the Agricultural Production Systems Simulator (APSIM), which has been rigorously tested for wheat (Triticum aestivum L.) in a Mediterranean environment, was used to estimate and analyse the WUE and NUE of wheat crops in the Mediterranean-climatic region of the central Western Australian agricultural zone. The APSIM model was run for three locations (average annual rainfall of 461 mm [high rainfall zone], 386 mm [medium] and 310 mm [low]) and two soil types that had contrasting plant-available water-holding capacities in the rooting zone (sand: 55 mm, clay soil: 109 mm). Simulations were carried out with historical weather records (82–87 years) assuming current crop management and cultivars. The modelling analyses highlighted the inherently high degree of seasonal variability in yield, WUE and NUE of wheat, depending on soil type, N fertiliser input, rainfall amount and, in particular, rainfall distribution. The clay soil tended to be more productive in terms of grain yield, WUE and NUE in the high and medium rainfall zones, but less productive in most years in the low rainfall zone. The sandy soil was less productive in the high rainfall zone due to the high nitrate leaching potential of this soil type, but more productive than the clay in the low rainfall zone due to poorer pre-anthesis growth and less water use, less water loss by soil evaporation and relatively more water use in the post-anthesis phase. When a wheat crop was sown early on clay soil in the low rainfall zone, it yielded as high as in the other rainfall zones in seasons when rainfall was above average or there was a good store of water in the soil prior to sowing. The simulations confirmed findings from a limited number of field experiments and extended these findings both qualitatively and quantitatively across soil types, rainfall regions and crop management options. Furthermore, by using long-term historical weather records, the simulations extended the findings across the wide range of climatic scenarios experienced in mediterranean-climatic regions.  相似文献   

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