新疆农田土壤有机质含量及组成特征

目前新疆农田土壤有机质含量在5．30～24．21g／kg之间，平均14．65g／kg，与第二次土壤普查相比，新疆农田土壤有机质含量呈上升趋势；胡敏素碳含量占到有机质碳量的53％～70％，平均61％，腐殖酸碳量只占39％。     

旱作条件下转甜菜碱醛脱氢酶基因水稻籽粒灌浆特性的研究

在旱作条件下,对转甜菜碱醛脱氢酶(BADH)基因水稻的3个品系(52-7、51-15、51-22)、受体亲本中花8号(ck1)和当地推广的以色列陆稻白珍珠(ck2)的籽粒灌浆特性进行了比较分析。结果表明:5个品种(系)的强、弱势粒灌浆过程均符合Richards模型,强、弱势粒灌浆为异步灌浆型。三个转BADH基因品系与其受体亲本相比,强、弱势粒的灌浆速率提高,活跃灌浆期延长,灌浆高峰期的籽粒重增加;籽粒灌浆中、后期,强势粒的灌浆天数缩短,强、弱势粒的平均灌浆速率提高,且不同粒位籽粒灌浆速率差异减小,最终使不同粒位籽粒大小的差异缩小和粒重增加。最大灌浆速率、平均灌浆速率和灌浆高峰期的粒重与千粒重存在显著正相关。     

干椒新品种蓉椒6号的选育

自交系9804和9909杂交配制成杂交一代干椒，植株生长旺盛，座果力强，较抗病毒病和疫病，果实指形，纵长17～19cm，横径1．2cm，青熟果绿色，老熟果鲜红色，单果重8．3g，味辣，品质佳，中熟品种，从定植到采收55d(天)，一般每667m^2产1500～1900kg。     

不同能量摄入水平对围产期奶牛生产性能及血浆瘦素浓度影响的研究

将健康的围产期奶牛30头随机分为3组, 每组10头。其中Ⅱ组为对照组, Ⅰ组和Ⅲ组分别为试验组。Ⅰ、Ⅱ、Ⅲ组均于产前28d开始分别饲喂NRC标准减少20%日粮(能量摄入80%组)、NRC标准日粮(能量摄入100%组)、NRC标准增加20%日粮(能量摄入120%组), 产后各组奶牛均饲喂标准日粮, 至产后56d结束。观察妊娠后期奶牛不同能量水平对干物质摄入量、产奶量、乳成分及体重等生产性能和血浆瘦素浓度的影响。试验结果表明: 奶牛产后干物质摄入量、产奶量、乳中蛋白质、乳脂率和非固体物质为Ⅰ组高于Ⅱ组、Ⅱ组又高于Ⅲ组(P>0 05 ); 同时血浆瘦素浓度为Ⅰ组高于Ⅱ组、Ⅱ组又高于Ⅲ组, 经统计分析组间差异极显著(P<0 01) 或差异显著(P<0 05); 但产前28~14d瘦素浓度组间差异均不显著(P>0 05 ), 此后Ⅰ组和Ⅲ组差异显著(P<0 05 )。此外, Ⅰ组体重消耗最小, Ⅲ组体重消耗最大, 各组间差异极显著(P<0 01)。可见, 围产期健康奶牛不同能量水平与干物质摄入量、产奶量、乳成分、体重等生产性能及血浆瘦素浓度之间存在着密切的关系。     

不同轮作序列对旱地胡麻土壤有机碳稳定性的影响

为了探索陇中黄土高原半干旱丘陵沟壑区胡麻轮作序列对土壤碳库的影响,2012-2016年通过4年定位试验,以连作为对照,研究了不同胡麻频率下的轮作序列(F:休闲;PWFW:25%Flax、马铃薯-小麦-胡麻-小麦;WFWP:25%Flax、小麦-胡麻-小麦-马铃薯;FWPF:50%Flax、胡麻-小麦-马铃薯-胡麻;WPFF:50%Flax、小麦-马铃薯-胡麻-胡麻;FFFF:100%Flax、胡麻-胡麻-胡麻-胡麻)对土壤团聚体、总有机碳(TOC)、土壤颗粒有机碳(POC)、土壤微生物碳(MBC)和氮(MBN)的影响。结果表明,休闲、不同轮作序列和低胡麻频率显著增加了030 cm土层<0.25 mm粒级的土壤团聚体含量、TOC和POC含量,而随胡麻频率的增加三者的含量呈下降趋势。其中,25%Flax处理下土壤团聚体含量较播前和休闲处理分别显著增加了2.02%4.04%和9.56%11.73%;土壤有机碳(SOC)较连作显著增加5.95%7.48%。50%Flax处理下胡麻位置对土壤SOC影响显著,且轮作(FWPF)显著高于连作(WPFF)。060 cm土层土壤SOC含量表现为休闲>播前≈25%Flax>50%Flax>100%Flax。与连作相比,轮作显著提高了010 cm土层土壤TOC和POC含量,呈现表层富集现象。土壤POC含量表现为25%Flax≈休闲>50%Flax>100%Flax。此外,轮作换茬显著增加了土壤MBC含量,且随着胡麻频率的增加,030 cm土层土壤MBC含量逐渐降低。与播前、休闲、轮作相比,连作显著降低土壤微生物碳氮比,50%Flax(WPFF)轮作序列和土层深度对土壤有机碳和微生物量的互作效应显著。综合来看,休闲可以显著改善土壤理化性状,25%胡麻频率的轮作序列利于保持土壤团聚体稳定性,增加土壤TOC、SOC和POC含量,而50%Flax轮作序列(WPFF)能够提高土壤微生物量和微生物碳氮比。表明25%胡麻频率的轮作序列均可维持土壤有机碳的稳定性,是旱地胡麻比较理想的轮作序列。     

南果梨周年干物质与氮磷钾积累动态

【目的】明确南果梨干物质积累特征和氮磷钾养分周年动态积累规律,为南果梨优化施肥量和施肥时期提供依据。【方法】以12年生南果梨树为试材,采用田间采样和树体分解方法,分别于萌芽后10 d(萌芽期)、 30 d(花期)、 65 d(幼果膨大期)、 100 d(果实膨大或新稍停止生长期)、 130 d(果实着色前)、 155 d(果实采收期)、 185 d(采收后)、 210 d(落叶前)8个生育期,选干周和树高一致的3株树,将树体连根从土壤中挖出,分出果实、 叶片、 枝条、 主干、 主根、 侧根、 须根,各器官单独称重,并取200 g左右的鲜样按清水、 洗涤剂、 清水、 1%盐酸、 3次去离子水冲洗、 杀青、 烘干后,电磨粉碎过0.15 mm筛,测定样品中氮、 磷、 钾含量。【结果】1)南果梨周年生育期内,树体干物质当年净积累量为18.4 kg/plant,干物质累积速率出现两次累积高峰,分别是幼果膨大期(0.15 kg/d)和采收期(0.11 kg/d)。2)南果梨树体总氮周年积累量为154.0~301.0 g,新生器官为0~116.2 g,果实膨大期达到最高;多年生器官氮积累量为154.0~194.8 g,落叶前达到最高。3)南果梨树体总磷周年积累量为17.1~37.2 g,果实着色前最高。其中新生器官为13.7 g,果实采收期最高;多年生器官为17.1~24.9 g,果实转色期最高。4)南果梨树体总钾周年积累量为27.9~174 g。新生器官钾为97.3 g,采收期最高;多年生器官钾为27.6~76.6 g,落叶前最高。5)产量大约为17 t/hm2的12年生南果梨从萌芽到落叶前树体当年氮磷钾的单株净累积量分别为146.2、 20.1、 146.1 g,折合1000 kg果实经济产量需吸收氮(N)、 磷(P)、 钾(K)5.4、 0.7、 5.4 kg。【结论】南果梨周年干物质单株积累总量为41.4 kg,当年净积累量为19.7 kg。南果梨干物质积累主要集中在花期到果实膨大期和果实转色到落叶前,分别占47.3% 和47.5%。南果梨从萌芽到落叶前氮、 磷、 钾的单株净累积量分别为146.2、 20.1、 146.1 g,每1000 kg果实经济产量需吸收氮(N)、 磷(P)、 钾(K)5.4、 0.7、 5.4 kg。从开花到果实膨大期和从果实着色到采收后30天对氮吸收分别占总氮累积量的39.0%和49.0%,而磷、 钾的累积从萌芽到开花较快,到果实膨大期磷的累积达67.4%,钾的累积达65.1%,果实膨大期是干物质和氮磷钾积累的关键时期。     

Response of labile organic C and N pools to plastic film removal from semiarid farmland soil

To examine the effects of plastic film removal on grain yield and soil organic matter (SOM), a spring maize (Zea may L.) field experiment was conducted for 5 yr at Changwu Agricultural and Ecological Experimental Station of Northwest China. Compared with traditional plastic film mulching during entire growing stages (FM), plastic film removal at the silking stage (RM) resulted in a 6.3% higher average maize yield. Under the RM treatment, soil organic carbon and total nitrogen significantly increased after the 5‐yr cultivation in the 0‐ to 20‐cm layer. Significant increases in extractable organic C (EOC), KMnO₄‐oxidizable C (KMnO₄‐C) and C management index (CMI) in the 0‐ to 20‐cm layer, and light fraction organic C and EOC in the 20‐ to 40‐cm layer were observed in response to plastic film removal after the 1‐yr treatment; the responses were more significant after 5 yr. Under the RM treatment, significant increases in microbial biomass C, light fraction organic N, extractable organic N, KMnO₄‐C and CMI were also observed after five years in the 20‐ to 40‐cm layer. Moreover, KMnO₄‐C and EOC were much more sensitive than other labile SOM fractions to the application of RM, even after only 1 yr of cultivation. Therefore, compared with mulching for the whole growing season, plastic film removal at the maize silking stage is an effective option for increasing yields and enhancing SOM concentration and soil sustainability in the regions with semiarid monsoon climates that have sufficient rainfall during maize reproductive stages.     

丘陵山地水田旱地交错分布区耕地地力评价

在自然条件下,通过比较水田和旱地地块的肥力差异,选择合适的评价模式,以制定合理的耕地利用依据。结合研究区丘陵山地水田和旱地交错的分布特点,依据最小控制斑块面积确定评价单元数,重点分析了水田和旱地在实际耕作中的差异性,并结合操作实践合理分配水田和旱地在评价体系中各指标的权重系数。结果表明,评价单元数的多少对评价结果的影响比较明显,综合研究区耕地地力实际情况和节约计算耗时的实际,建议最小控制斑块面积在临界值(推荐值)的10%为佳;另外通过水旱分开评价和水旱统一评价两种评价模式的比较,发现水旱分开能使评价结果更加贴近实际情形,反映实际耕地地力状况,能够更加有效地指导农业生产实践。     

Limited effects of land use on soil dissolved organic matter chemistry as assessed by excitation–emission fluorescence spectroscopy and molecular weight fractionation

Dissolved organic matter (DOM) in soil solution represents a complex mixture of organic molecules and plays a central role in carbon and nitrogen cycling in plant–microbial–soil systems. We tested whether excitation–emission matrix (EEM) fluorescence spectroscopy can be used to characterize DOM and support previous findings that the majority of DOM is of high molecular weight (MW). EEM fluorescence spectroscopy was used in conjunction with MW fractionation to characterize DOM in soil solution from a grassland soil land management gradient in North Wales, UK. Data analysis suggested that three distinct fluorescence components could be separated and identified from the EEM data. These components were identified as being of humic‐like or fulvic‐like origin. Contrary to expectations, the majority of the fluorescence signal occurred in the small MW (<1 kDa) fraction, although differences between soils from the differently managed grasslands were more apparent in larger MW fractions. We conclude that following further characterization of the chemical composition of the fluorophores, EEM has potential as a sensitive technique for characterizing the small MW phenolic fraction of DOM in soils.     

Evaluating biodegradability of soil organic matter by its thermal stability and chemical composition

The stability of soil organic matter (SOM) as it relates to resistance to microbial degradation has important implications for nutrient cycling, emission of greenhouse gases, and C sequestration. Hence, there is interest in developing new ways to quantify and characterise the labile and stable forms of SOM. Our objective in this study was to evaluate SOM under widely contrasting management regimes to determine whether the variation in chemical composition and resistance to pyrolysis observed for various constituent C fractions could be related to their resistance to decomposition. Samples from the same soil under permanent pasture, an arable cropping rotation, and chemical fallow were physically fractionated (sand: 2000-50 μm; silt: 50-5 μm, and clay: <5 μm). Biodegradability of the SOM in size fractions and whole soils was assessed in a laboratory mineralization study. Thermal stability was determined by analytical pyrolysis using a Rock-Eval pyrolyser, and chemical composition was characterized by X-ray absorption near-edge structure (XANES) spectroscopy at the C and N K-edges. Relative to the pasture soil, SOM in the arable and fallow soils declined by 30% and 40%, respectively. The mineralization bioassay showed that SOM in whole soil and soil fractions under fallow was less susceptible to biodegradation than that in other management practices. The SOM in the sand fraction was significantly more biodegradable than that in the silt or clay fractions. Analysis by XANES showed a proportional increase in carboxylates and a reduction in amides (protein) and aromatics in the fallow whole soil compared to the pasture and arable soils. Moreover, protein depletion was greatest in the sand fraction of the fallow soil. Sand fractions in fallow and arable soils were, however, relatively enriched in plant-derived phenols, aromatics, and carboxylates compared to the sand fraction of pasture soils. Analytical pyrolysis showed distinct differences in the thermal stability of SOM among the whole soil and their size fractions; it also showed that the loss of SOM generally involved preferential degradation of H-rich compounds. The temperature at which half of the C was pyrolyzed was strongly correlated with mineralizable C, providing good evidence for a link between the biological and thermal stability of SOM.