不同栽培模式对冬小麦-夏玉米轮作系统产量、氮素累积和平衡的影响

以河北山前平原区秸秆还田条件下小麦-玉米轮作体系为研究对象,设置农民习惯、高产高效、再高产和再高产高效4个模式,通过定位试验探讨各栽培模式对3个轮作周期作物产量、土壤硝态氮累积量及氮平衡的影响.结果表明: 小麦、玉米产量均以再高产模式最高,高产高效和再高产高效模式次之,均显著高于农民习惯模式;小麦季和玉米季氮肥利用效率(PFP)均以高产高效模式最高,显著高于其他模式;0～400 cm土体硝态氮累积量在 768.4～1133.3 kg·hm^-2之间,其中80%～85%累积在根下90～400 cm土层;4种模式的土壤硝态氮均有明显向下淋移现象,120～150 cm和270～330 cm处均出现了累积峰,以270～330 cm土层硝态氮累积量最大;高产高效模式的土壤硝态氮含量整体水平均低于其他模式,浓度基本维持在30 mg·kg^-1以下,在一定程度上能有效缓解环境压力;冬小麦季0～90 cm土体氮素盈余量均小于夏玉米季,并以高产高效模式的氮素表观损失量最低,显著低于其他模式.综合考虑产量、氮肥利用效率、硝态氮累积和氮平衡,以高产高效模式表现最优,但还有一定的提升空间.     

基于耦合模型的干旱区植被净初级生产力估算

净初级生产力是陆地生态系统物质与能量运转研究的基础, 在干旱区生态环境演变及其与气候相互作用和影响方面极为敏感,是揭示干旱区生态环境特征的重要指标.本研究基于RS和GIS技术,利用地面气象数据、涡度相关数据、Landsat 8数据和MODIS数据,通过SEBAL模型和光能利用率模型的耦合,估算了新疆玛纳斯河流域植被净初级生产力(NPP),分析了其空间格局及与高程和坡度的关系.结果表明: SEBAL模型与光能利用率模型的耦合对玛纳斯河流域山地-绿洲-荒漠生态系统植被NPP的模拟效果较合理,能较好地反映植被净初级生产力的实际情况;2013年,玛纳斯河流域植被NPP总量为7066.72 Tg C·a^-1,平均值为278.06 g C·m^-2·a^-1,总体分布趋势是自南向北先增加后减少再增加最后减少,随着地貌和土地利用类型的变化呈现明显的分布规律,且其月变化比较明显,7—8月达到最大值,占总量NPP的52.2%;植被净初级生产力随海拔和坡度的增加整体呈下降趋势,但随海拔增加植被NPP出现3次波动.这些波动主要由地表植被覆盖类型和环境因素所引起.     

水氮互作对固定道垄作栽培春小麦根系生长及产量的影响

为探讨固定道小麦栽培方式下适宜的水氮组合,以低水1200 (W₁)、中水2400 (W₂)、高水3600 m³·hm^-2 (W₃)为主处理,0 (N₀)、低氮90(N₁)、中氮180 (N₂)、高氮270 kg·hm^-2 (N₃)为副处理,采用裂区设计,对固定道垄作栽培方式下水氮互作对春小麦根系生长及产量的影响进行了研究.结果表明:水氮互作能显著影响春小麦根干质量密度(RWD),RWD随着小麦生育期的进程表现为先增大后减小的趋势,在灌浆期达最大;RWD对施氮量的响应取决于灌溉量,在W₁下,RWD在N₁处理下最大,在W₂下,RWD随着施氮量的增加在N₂处理下最大,在W₃下,RWD随着施氮量的增加在N₃ 处理下最大;不同灌溉处理下RWD表现为W₂>W₃>W₁;施氮与灌水显著影响RWD,表现为灌水>氮肥>水氮互作,在W₂N₂处理下最大.根冠比随着灌水量与施氮量的增加逐渐减小,在W₁N₀处理下根冠比最大;85%以上的小麦根系分布于0～40 cm土层,产量与0～40 cm土层RWD呈显著抛物线回归关系,与40～60 cm土层RWD呈显著线性正回归关系.W₂灌溉条件可以促进小麦根系向中下层(40～60 cm)分布;灌水施氮能显著影响春小麦籽粒产量与生物产量,生物产量随着施氮量和灌水量的增加而增加,籽粒产量在W₂N₂最大;灌水生产力随灌水量的增加逐渐降低,氮肥农学利用率随施氮量的增加而减小.因此,在固定道垄作栽培方式下,施肥量与灌水量控制在N₂ (180 kg·hm^-2)与W₂(2400 m³·hm^-2)条件下有利于促进根系生长,进而提高春小麦籽粒产量及水氮利用效率,是河西灌区固定道小麦栽培方式下适宜的水氮组合.     

五种荒漠灌木群落土壤有机碳垂直分布及其与根系分布的关系

研究土壤有机碳与根系分布之间关系对评估碳储量和固碳潜力具有重要意义,而我国荒漠区灌木群落土壤有机碳与植物根系之间的关系尚不清楚。本研究选取深根性表层型灌木(表层根系生物量最大)梭梭(Haloxylon ammodendro)和中间锦鸡儿(Caragana intermedia)、深根性非表层型(表层根系生物量不是最大)灌木白刺(Nitratia tangutorum)、浅根性表层型灌木红砂(Reaumuria songarica)及浅根性非表层型灌木霸王(Sarcozygium xanthoxylon)为优势种的5种荒漠灌木群落为研究对象,测定100 cm深度内不同层次根系生物量及土壤有机碳含量,探讨灌木群落土壤有机碳的垂直分布格局及其与根系之间的关系。结果显示:(1)0~100 cm土壤有机碳密度与群落0~20 cm根系生物量碳密度显著正相关,与其他层次或累积深度不显著相关;(2)梭梭群落0~100 cm土壤有机碳密度显著低于与其他4个群落(P0.01),其他4个群落无显著差异(P0.05);(3)优势种为表层型的梭梭、中间锦鸡儿和红砂群落土壤有机碳密度与群落及优势种根系变化趋势一致,优势种为浅根性非表层型的霸王群落仅表层40 cm土壤有机碳与优势种灌木根系分布规律一致,优势种为深根性非表层型的白刺群落土壤有机碳与优势种根系分布规律一致。本研究表明,荒漠灌木群落0~100 cm土壤有机碳储量与群落0~20 cm根系生物量显著相关,群落优势种根系分布类型是影响土壤有机碳垂直分布格局的重要因素。     

Screening and identification of a microsatellite marker associated with sex in Wami tilapia, <Emphasis Type="Italic">Oreochromis urolepis hornorum</Emphasis>

In this study, primer pairs of 15 microsatellite markers associated with sex determination of tilapia were selected and amplified in Wami tilapia, Oreochromis urolepis hornorum. While one marker, UNH168, on linkage group 3 (LG3) was associated (P < 0.001) with the phenotypic sex in the experimental population, nine genotypes were detected in both sexes. Only 99-bp allele was detected in the female samples, while 141, 149 and 157-bp alleles were present in both male and female samples. UNH168 was localized by fluorescence in situ hybridization (FISH) on the long arm of the largest tilapia chromosome pair (chromosome 1, equivalent to LG3). This sex-linked microsatellite marker could potentially be used for marker-assisted selection in tilapia breeding programmes to produce monosex male tilapia.     

Purification, crystallization and X-ray diffraction analyses of the T. elongatus PSII core dimer with strontium replacing calcium in the oxygen-evolving complex

The core complex of photosystem II (PSII) was purified from thermophilic cyanobacterium Thermosynechococcus elongatus grown in Sr(2+)-containing and Ca(2+)-free medium. Functional in vivo incorporation of Sr(2+) into the oxygen-evolving complex (OEC) was confirmed by EPR analysis of the isolated and highly purified SrPSII complex in agreement with the previous study of Boussac et al. [J. Biol. Chem. 279 (2004) 22809-22819]. Three-dimensional crystals of SrPSII complex were obtained which diffracted to 3.9 A and belonged to the orthorhombic space group P2(1)2(1)2(1) with unit cell dimensions of a=133.6 A, b=236.6 A, c=307.8 A. Anomalous diffraction data collected at the Sr K-X-ray absorption edge identified a novel Sr(2+)-binding site which, within the resolution of these data (6.5 A), is consistent with the positioning of Ca(2+) in the recent crystallographic models of PSII [Ferreira et al. Science 303 (2004) 1831-1838, Loll et al. Nature 438 (2005) 1040-1044]. Fluorescence measurements on SrPSII crystals confirmed that crystallized SrPSII was active in transferring electrons from the OEC to the acceptor site of the reaction centre. However, SrPSII showed altered functional properties of its modified OEC in comparison with that of the CaPSII counterpart: slowdown of the Q(A)-to-Q(B) electron transfer and stabilized S(2)Q(A)(-) charge recombination.