滴灌灌水均匀系数与灌水量对土壤水分分布及温室番茄产量的影响

为探索灌水均匀系数与灌水量对温室番茄产量和土壤水分变化的影响,确定合理的滴灌灌水均匀系数,本研究设置65%、75%和85%3个灌水均匀度水平, 190 mm、220 mm和250 mm 3个灌水量水平,测量番茄生育期内土壤含水率及番茄产量,计算土壤含水率均匀系数和番茄灌溉水利用效率。结果表明,当灌水均匀系数为65%～85%时,土壤水分均匀系数均值(82.57%～93.76%)接近或高于设置的滴灌灌水均匀系数的最大值(85%)。滴灌灌水均匀系数对土壤含水率均匀系数影响权重最大,灌水量、灌水均匀系数、土壤初始含水率均值3个影响因素与土壤含水率均匀系数均值之间呈线性关系(P0.05),决定系数为0.918。当土壤初始含水率占田间持水量比重60%,灌水量低于15mm时,灌水均匀系数与灌水量二者的交互作用与土壤含水率均匀系数为显著线性关系(P0.05),其他情况下均无显著性关系。灌水量对产量为显著影响(P0.05),灌水均匀系数及二者的交互作用对番茄产量无显著影响,考虑产量及灌溉水分利用效率,灌水量220 mm、灌水均匀系数75%组合为最优组合。因此在西北地区,综合考虑经济性和系统的可靠性,建议下调现行滴灌灌水均匀系数标准。     

Indicators and trade-offs of ecosystem services in agricultural soils along a landscape heterogeneity gradient

Soil functions can be classified as supporting (nutrient cycling) and provisioning (crop production) ecosystem services (ES). These services consist of multiple and dynamic functions and are typically assessed using indicators, e.g. microbial biomass as an indicator of supporting services. Agricultural intensification negatively affects indicators of soil functions and is therefore considered to deplete soil ES. It has been suggested that incorporating leys into crop rotations can enhance soil ES. We examined this by comparing indicators of supporting soil services – organic carbon, nitrogen, water holding capacity and available phosphorous (carbon storage and nutrient retention); net nitrogen mineralisation rate and microbial biomass (nutrient cycling and retention) – in barley fields, leys and permanent pastures along a landscape heterogeneity gradient (100, 500 and 1000 m radii). In addition, barley yields (provisioning service) were analysed against these indicators to identify trade-offs among soil services. Levels of most indicators did not differ between barley and ley fields and were consistently lower than in permanent pastures. Leys supported greater microbial biomass than barley fields. Landscape heterogeneity had no effect on the indicators or microbial community composition. However, landscape heterogeneity correlated negatively with yield and soil pH, suggesting that soils in heterogeneous landscapes are less fertile and therefore have lower yields. No trade-offs were found between increasing barley yield and the soil indicators. The results suggest that soil ES are determined at the field level, with little influence from the surrounding landscape, and that greater crop yields do not necessarily come at the expense of supporting soil services.     

沼液淹没土壤抑制根结线虫及对土壤线虫群落的影响

为探索沼液抑制根结线虫的效果,本研究通过盆栽试验,以番茄为试供作物,对比了种植前沼液淹没土壤(BSS)、种植期间浇灌沼液(BS)和加热(HE)3种方法对根结线虫的防控效果。结果表明,与不采取任何措施的对照(CK)处理相比, BSS处理抑制根结线虫效果最为明显,防效高达97.1%,根结指数分别比HE和BS处理降低96.9%和92.9%。HE处理尽管在处理土壤后显著降低了根结线虫数量,但在最后破坏性取样时(结束试验)出现反弹,根结线虫数量甚至高于CK处理。对于土壤线虫群落,CK处理中以植食性线虫为主(81.8%);两个沼液处理中食细菌线虫占优势(平均78.3%),且其中的杂食捕食性线虫在土壤前处理后消失,在试验结束时又重新出现,但所占比例依然非常低。沼液淹水方式的高效防控效果揭示了利用沼液防控根结线虫的关键期在于线虫入侵到植物根部之前的幼虫期。然而,在盆栽系统中,沼液淹水的方式也对作物生长表现出了一定的抑制趋势。高量沼液施用防控病害的同时引发的植物毒害作用以及环境污染风险,需要进一步开展田间研究。     

有机肥等氮替代化肥对红壤团聚体及玉米产量和品质的影响

为研究有机肥等氮替代化肥对土壤结构、玉米产量和品质的影响,设置有机肥等氮替代化肥的10%（M10）、20%（M20）、30%（M30）、40%（M40）,以单施化肥（M0）和不施肥（CK）为对照6个施肥处理,测定玉米不同生育期的土壤团聚体变化状况。结果表明：随有机肥等氮部分替代化肥比例的增加,玉米各生育期土壤>0.25mm水稳性团聚体（R_0.25）、平均质量直径（MWD）、几何平均直径（GWD）不断增加,团聚体破坏率（PAD）、分形维数（D）不断降低。与M0处理相比,M30和M40处理显著提高了玉米子粒产量,表现为M30>M40;M20、M30、M40处理较M0处理玉米子粒蛋白质含量显著增加了13.29%~25.03%,淀粉含量显著增加了39.84%~114.06%,可溶性糖含量显著增加了36.49%~54.05%;蛋白质含量表现为M30和M20处理显著大于M40处理,M30与M20处理间差异不显著;淀粉含量表现为M40>M30>M20,差异显著;可溶性糖含量表现为M40和M30处理显著大于M20处理,M30与M40处理间差异不显著。玉米子粒产量和品质与抽雄期、成熟期土壤团聚体R_0.25呈极显著正相关（P<0.01）,与PAD、D值呈极显著负相关（P<0.01）。因此,玉米生产中,利用有机肥等氮替代化肥培肥土壤,需兼顾玉米产量和品质,30%为适宜的有机肥等氮替代化肥比例。     

不同施氮量对冬小麦产量、效益及土壤理化性状的影响

为探明豫北地区高肥力地块不同施氮量对冬小麦产量、经济效益及土壤理化性状的影响,在安阳市北关区壤质潮土上开展了冬小麦不同施氮量试验,设常规施磷钾肥（W1,CK）、常规施肥减施氮肥30%（W2）、常规施肥减施氮肥15%（W3）、常规施肥减施氮肥5%（W4）、常规施肥（W5）和常规施肥增施氮肥5%（W6）6个处理。结果表明,随着氮肥施用量的减少冬小麦主茎叶龄、次生根数、茎蘖数、株高及穗长等农艺性状呈下降趋势,以W6处理最佳。冬小麦产量随着施氮量的增加呈上升趋势,W4、W5、W6处理与W1处理相比增幅分别达48.7%、48.9%、49.1%,W4、W5、W6处理间差异不显著;但与W2、W3处理间差异达到显著水平。不同施氮量处理经济效益较W1处理均有不同程度增加,W4较W1处理净增效益5 869.80元/hm ²,较W5处理净增效益24.45元/hm ²。不同施氮量处理对土壤有机质、全氮、有效磷、速效钾、缓效钾含量和土壤容重有显著影响,但对pH影响不显著。土壤全氮含量随施氮量的增加呈上升趋势;W4处理土壤容重最低。综合分析,以常规施肥减施氮肥5%处理效果最佳。     

Can differences in 15N natural abundance be used to quantify the transfer of nitrogen from legumes to neighbouring non-legume plant species?

Natural variations in the stable isotope ¹⁵N are often exploited in studies of N cycling in ecosystems. Lower ¹⁵N natural abundance in non-legume plants growing in association with legumes, compared with the non-legume grown alone in pure stands have been observed in cropping, forage, and agroforestry systems. Such observations have frequently been attributed to the transfer of biologically-fixed nitrogen (N) from the legume to the companion non-legume, and various methodologies have been employed to calculate the extent of the N transfer. While some of these ¹⁵N natural abundance-based estimates of N transfer were within the range previously reported using equivalent ¹⁵N-enriched techniques (<20% of non-legume plant N and <10 kg N ha⁻¹ derived from fixed N contributed by neighbouring legumes), many of the values obtained using natural abundance were much higher (30%–83% of the non-legume N derived from fixed N representing up to 30–40 kg N ha⁻¹) than generally measured by ¹⁵N-enriched methods; with even greater estimates being determined where data were available to allow N transfer to be re-calculated on the basis of total legume N rather than fixed N (42% to >100%, and up to 110 kg N ha⁻¹ per year). This review raises concerns about the assumptions behind the natural abundance approach, and provides some alternative interpretations for the observed differences in natural ¹⁵N abundance between plants grown in the presence and absence of legumes. It was concluded that simple comparative measures of non-legume δ¹⁵N alone cannot provide a quantitative estimate of N transfer between plant species if the dominant source and the isotopic identity of the transferred N cannot be validated, and if the extent of any isotopic fractionation associated with relevant N transformations occurring during transfer cannot be defined. To date this information is not forthcoming. There is a need to greatly improve our understanding of the transfer processes before the real value of the δ¹⁵N technology can be realized. In the first instance this will primarily be achieved by carefully executed experiments under controlled conditions, and in the field, employing both ¹⁵N natural abundance and enrichment approaches so estimates of transfer can be compared, and the data interrogated using modelling approaches to explore isotopic fractionation.     

Cross‐linked polyacrylates in post‐mining substrates: persistence and effects on plant growth

Application of hydrophilic polymers composed of cross‐linked polyacrylate can improve soil water‐holding capacity and accelerate the restoration of post‐mining substrates. In this work, we studied the persistence of a polyacrylate polymer incorporated into a soil and its impact on plant nutrients at a reclamation site of former lignite mining in Lusatia (Germany). In contrast to autumn application, the incorporation of the polymer enhanced the sequestration of plant‐derived carbon in the soil, which was reflected by a significant increase in the concentration of a lignin marker. Attenuated total reflexion–Fourier transform infrared spectra (ATR‐FTIR) and total elemental contents in the applied polymer suggested an intensive cation exchange between the polymer framework and the soil‐forming substrate. In addition, there was an enrichment of carbonaceous material, which seems to reduce the swelling and thus the water‐holding capacity of the cross‐linked polyacrylate. Conversely, this process protected the polymer structure from rapid decomposition.     

不同发育阶段日本落叶松人工林枯落物层微生物群落特征

为探寻日本落叶松人工林在中龄林或近熟林阶段地力衰退的机制，以分子生物学实验手段与常规实验分析方法结合，分别对不同发育阶段林分枯落物未分解层、半分解层以及全分解层微生物的数量、群落结构以及理化性质进行分析，并采用冗余分析法探索枯落物层微生物群落结构与理化性质的相关性。结果表明：枯落物储量及养分储量随林分发育呈倒“V”字型变化趋势，在近熟林阶段最大，微生物数量、均匀度指数在中龄林或近熟林最低。不同发育阶段林分优势细菌种类基本相同，但相对含量不同；优势真菌的种类明显不同，尤其是在近熟林半分解层。中龄林与近熟林未、半分解层受环境因素影响较大，主要受pH、有效磷、碱解氮、速效钾、全钾、C/N以及林下植被生物量影响。因此，日本落叶松纯林在中龄林与近熟林阶段需强化植被管理，适时开展修枝间伐等经营措施，促进林下植被发育、改善枯落物性质，加速养分循环，缓解地力衰退。     

局地尺度高寒草原土壤真菌多样性对地上植物多样性与生产力关系的调控作用

为研究局地尺度高寒草原土壤真菌多样性对地上植物多样性与生产力关系的调控作用，本研究以青海省湟源县局地尺度高寒草原为研究对象，对不同植物多样性梯度的地上生产力、土壤理化性状和土壤真菌多样性等指标进行调查、采样和分析。通过偏回归分析（partial least squares regression，PLSR）、方差分解分析（variance partitioning analysis，VPA）、构建结构方程模型（structural equation model，SEM）等分析手段，分析了土壤真菌多样性对地上植物多样性与生产力关系的调控作用。结果表明，高寒草原植物多样性与地上生产力存在显著线性正相关关系；土壤真菌多样性分别与植物多样性和地上生产力呈显著正相关关系；通过PLSR，VPA，SEM等方法控制土壤非生物因子效应后，真菌多样性与二者的显著正相关关系仍存在。综上所述，局地尺度下青海省湟源县高寒草原土壤真菌多样性是调控地上植物多样性与生产力正向关系的关键生物因子。     

滴灌条件下秸秆覆盖和土壤含水量对冬小麦灌浆特性的影响

为阐明滴灌条件下秸秆覆盖和土壤含水量以及两因素交互作用对冬小麦籽粒灌浆、产量形成的影响,以冬小麦矮抗58为试验材料,设计了秸秆处理(覆盖T、不覆盖T0)与土壤相对含水量(40%(W1)、50%(W2)、60%(W3)、70%(W4)4个水平)两因素裂区试验。结果表明:Richards方程拟合秸秆覆盖和水分调控下冬小麦籽粒灌浆过程的决定系数在0.977 5~0.999 6,达到极显著水平。秸秆覆盖和水分调控间的交互作用对除最大灌浆速率和平均灌浆速率(V)外其他冬小麦籽粒灌浆特征参数的影响达到显著或极显著水平。其中,秸秆覆盖下土壤相对含水量60%(TW3)处理组合具有最长的灌浆持续期T(51.91 d),最长的灌浆中期持续期T_2(15.230 d)和灌浆后期持续期T_3(26.556 d),最大的灌浆中期灌浆速率R_2(0.897 mg/d)和灌浆后期灌浆速率R_3(1.365 mg/d)。产量、水分利用效率和耗水量的二次曲线关系表明,在耗水量240~270 mm可达到产量与水分利用效率双高的效果。本试验中以秸秆覆盖与土壤相对含水量60%(TW3)处理组合水分利用效率最高(29.02 kg/(mm·hm~2)),较秸秆覆盖下土壤相对含水量的70%(TW4)提高了5.30%;产量为7 097.7 kg/hm~2,与TW4处理组合差异不显著。