链霉菌和壳聚糖对淮山土壤微生物活性与群落的影响

为探究链霉菌30702和壳聚糖对淮山土壤微生物活性与群落的影响,采用比色法和滴定法观测土壤酶活性的变化,采用高通量测序技术和Trimmomatic等软件,分析土壤微生物群落中细菌和真菌的发展变化。结果表明,链霉菌、壳聚糖、土壤原始微生物和培养时间等4个因素对淮山土壤的脲酶和过氧化氢酶活性均有显著影响,壳聚糖浓度在0~10.0 g/kg内,土壤酶活性随壳聚糖浓度的增大而提高;随时间的延长,先升再降;壳聚糖与链霉菌之间存在交互效应。链霉菌和壳聚糖能增加淮山土壤细菌的物种丰度,减少细菌的多样性,增加艾德昂菌属（Ideonella）和纤维弧菌（Cellvibrio）等有益菌属的相对丰度,而对真菌的物种丰度和多样性的影响较小,与对照之间的差异不显著,土壤优势菌属为腐质霉属（Humicola）、枝孢属（Cladosporium）、鞘氨醇单胞菌属（Sphingomonas）和uncultured_bacterium_ c_Subgroup_6。其中,链霉菌与2.5 g/kg壳聚糖复合处理的细菌物种丰度最大,细菌多样性最少。     

Soil available potassium affected by rice straw incorporation and potassium fertilizer application under a rice–oilseed rape rotation system

Data from 147 field trials were collected to study the influence of straw incorporation on soil potassium (K) under an intensive rice–oilseed rape rotation system, while pot experiments were conducted to evaluate the effects of rice straw incorporation on soil K availability. A significant correlation was observed between the soil available K and the relative yield (RRY) and the relative K uptake (RKU) of oilseed rape, with R² values ranging from 0.07 to 0.08 and from 0.10 to 0.11, respectively, when data were fitted to a logarithmic equation model. In approximately 30% of trials, RRY reached 90%, while soil test available K values were below the critical limit, indicating that soil K values at the time of sampling (within 1 week of rice harvest) underestimated the actual soil K supply capacity. The pot experiment results showed that soil available K was affected by straw incorporation and soil type in the fallow period. The NH₄OAc‐K and NaBPh₄‐K concentrations of soils increased at first, and then, plateaued after 28 days. Straw incorporation significantly influenced the critical soil K concentration, which is important for making accurate K fertilizer recommendation. These results suggested that straw K should be seriously considered in making K fertilizer recommendations. Extending the sampling time from 1 to 3 weeks after the harvesting of rice to stabilize the effects of straw incorporation may help achieve a more accurate evaluation of soil available K.     

供氮方式对冬马铃薯氮肥利用效率及氮素去向的影响

以马铃薯费乌瑞它为试材,采用田间微区~(15)N示踪技术,研究施N量160kg·hm~(-2)全部基施(T1)、55%基施+45%在齐苗期追施(T2)、55%基施+30%在齐苗期追施+15%在现蕾期追施(T3)3种方式,对冬马铃薯氮肥利用效率及去向的影响。结果表明:马铃薯吸收的N约46%~52%来源于当季施用的氮肥,48%~54%来自土壤和种薯;肥料N利用率为35.16%~39.99%,残留率为47.71%~51.78%,损失率为8.23%~15.50%。3种施氮方式下,肥料N主要残留在0~15cm土层。随施氮时间后移,肥料N残留在0~15cm土层呈上升趋势,在15~45cm土层呈下降趋势。施氮方式对马铃薯干物质积累总量和块茎干物质积累量影响不明显,但T3肥料N利用率、肥料N残留率明显大于T1、T2。因此,综合经济效益和环境效益,T3施氮方式的效果较为理想。本研究为马铃薯氮素养分的有效管理提供了指导依据。     

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.     

北京小西山山前洪积扇不同土地利用方式下的土壤微形态特征

通过对北京小西山山前代表性洪积扇的观察研究,探索不同土地利用方式对土壤微形态特征的影响。通过对土壤薄片的观察,分析土壤微形态特征;用ENVI及MATLAB软件处理图片,并对孔隙度进行定量分析。结果表明:1)林地(WL1)剖面表层土壤微结构为海绵状结构,而园地(WL2)和菜地(WL3)的表层土壤多呈整块状结构或孔道结构;2)各采样点土壤矿物成分相近,但骨骼颗粒形态特征有较大差异。3)WL1剖面土壤孔隙度较高,以面状孔隙为主,WL2和WL3剖面土壤孔隙度过低,以中小孔隙居多。研究认为:1)林地的土壤微结构较园地和菜地的好,由于人类的不合理利用和管理,园地和菜地使土壤微结构变差,土壤孔隙度下降。2)各采样点土壤成土母质相似,土壤骨骼颗粒形态差异受到不同土地利用方式下人类干扰程度差异的影响。     

不同施肥方式对红壤蔬菜田氨氧化细菌和氨氧化古菌群落的影响

通过构建氨单加氧酶基因(amoA)克隆文库,研究在红壤蔬菜田上只施用磷钾化肥(PK)、只施氮磷钾化肥(NPK)、施用腐熟有机肥(DNPK)和施用新鲜有机肥(FNPK)等4种不同施肥处理的土壤氨氧化细菌(AOB)和氨氧化古菌(AOA)群落多样性及与土壤脲酶活性的相关性。结果表明:施加有机肥处理(DNPK和FNPK)的蔬菜田土壤的AOB文库和AOA文库OTU数量和Shannon指数高于只施用无机肥(NPK和PK)处理的蔬菜田土壤;DNPK和FNPK处理的土壤优势AOB菌群为多形亚硝化叶菌(Nitrosolobus multiformis),比例分别为88.5%和68.5%,NPK和PK处理的土壤优势AOB菌群为亚硝化单胞菌属(Nitrosospirasp.),比例分别为54.8%和65.5%;DNPK、FNPK、NPK和PK处理土壤优势AOA菌群均为阿伯丁土壤亚硝化细杆菌侯选种(CandidatusNitrosotalea devanaterra),比例分别为90.9%、84.4%、77.8%和45.2%;施加有机肥处理(DNPK和FNPK)的土壤脲酶活性和氨氧化微生物的多样性指数都高于只施用无机肥处理(NPK和PK);AOA群落多样性指数与土壤脲酶活性呈显著正相关,而AOB群落多样性与土壤脲酶活性相关性不显著。总体来看,有机肥比无机肥处理提高了AOA和AOB群落多样性,且AOA在红壤蔬菜田土壤氨氧化过程中起着更为重要的作用。     

Nitrous oxide emission from a transplanted rice field in alluvial soil as influenced by management of nitrogen fertiliser

We investigated nitrous oxide (N₂O) emission from an irrigated rice field over two years to evaluate the management of nitrogenous fertiliser and its effect on reducing emissions. Four forms of nitrogenous fertilisers: NPK at the recommended application rate, starch–urea matrix (SUM) + PK, neem‐coated urea + PK and urea alone (urea without coating) were used. Gas samples were collected from the field at weekly intervals with the static chamber technique. N₂O emissions from different treatments ranged from 11.58 to 215.81 N₂O‐N μg/m²/h, and seasonal N₂O emissions from 2.83 to 3.89 kg N₂O‐N/ha. Compared with other fertilisers, N₂O emissions were greatest after the application of the conventional NPK fertiliser. Moreover, SUM + PK reduced total N₂O emissions by 22.33% (P < 0.05) compared with NPK during the rice‐growing period (P < 0.05). The results indicate a strong correlation between N₂O emissions and soil organic carbon, nitrate, ammonium, above‐ and below‐ground plant biomass and photosynthesis (P < 0.05). The application of SUM + PK in rice fields is suitable as a means of reducing N₂O emissions without affecting grain production.     

Managing soil quality for humanity and the planet

Rather than a human-centric, the basic strategy of achieving Sustainable Development Goals must be focused on restoring and sustaining planetary processes. The urgency of meeting the demands of the humanity must be reconciled with the necessity of enhancing the environment. Increasing and restoring soil organic matter content of the degraded and depleted soils is critical to strengthening planetary processes.     

青土湖水面形成区土壤颗粒组成与化学特性变化

青土湖输水作为石羊河流域治理的一项关键措施,对保护湖区水资源和生态环境具有重要意义。在距青土湖水面边缘东南方向0-450 m的10个样点中分3层取0-60 cm土样,测定土壤粒径的质量百分比与全氮、全磷、全钾和电导率,分析青土湖水面形成后土壤颗粒组成与化学特性变化。结果表明,随着离水面边缘距离的增加,土壤颗粒与化学特性呈有规律的增减变化,土壤粘粉粒组成与其全磷、全钾之间存在正线性相关。青土湖水面形成加剧了距水面边缘0-150 m处的土壤理化性质变化;土壤细粒及养分出现富集,分别在距水面边缘100-150 m和300 m处达到最大值。因此,土壤养分与土壤细物质的良好相关性表明,土壤粘粉粒变化可作为反映该区域土壤性状变化和评价衡量水面形成后土壤恢复程度的定量指标之一。