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。     

秸秆深还机具特点和作业效率分析

秸秆深埋还田(秸秆深还)作为一种新兴的秸秆还田模式,其机具有别于地表覆盖还田和铧式犁翻压还田。为了科学管理、合理运用秸秆深还机械,提高机组的作业效率,在调查测试秸秆深还作业的基础上,对机具的特点进行了分析,同时对测试机组分别进行了时间利用率和作业效率分析。结果表明:对于各个机具的作业时间利用率和总作业效率影响因素有所不同。作业速度、幅宽、故障维修和地头转向是影响机械作业效率的主要因素。根据调查和分析的结果,针对秸秆深还作业中存在的问题提出了机组的合理运行模式。     

大凌河流域生态综合治理项目效益分析

葫芦岛市建昌县2014年国家农业综合开发大凌河流域生态综合治理项目分布在建昌县新开岭乡新开岭村、贺杖子乡碾房村、素珠营子乡梁杖子村.通过该项目治理后,生态环境得到明显改善,经济效益十分显著,社会效益巨大,促进了区域经济社会发展.同时工程建设也起到了科技示范作用,为推动生态环境建设奠定了坚实基础保障.     

蚯蚓粪缓解草莓连作土壤障碍的作用

【目的】土壤灭菌处理已成为草莓生产中土传病害综合管理的重要措施,但是土壤灭菌明显抑制了土壤微生物的活性,影响草莓植株的生长。有机肥中含有大量的生物活性物质,尤其是蚯蚓粪。本研究通过观测连作土壤灭菌后施用不同有机肥对草莓植株地上部和地下部的影响,为减缓草莓植株生长的连作障碍提供有机肥选择。【方法】采用温室盆栽草莓模拟试验,首先在去除土壤化感效应影响基础上设置土壤灭菌和正常土壤栽培两个处理,探讨土壤灭菌对草莓植株不同阶段地上部叶片及地下部根系生长影响,在此基础上以相同连作土壤进行另一个盆栽试验,设置不灭菌土壤加无机肥料(LW)、 加牛粪(LN)、 加蚯蚓粪(LQ)处理,灭菌土壤加无机肥料(LMW)、 加牛粪(LMN)、 加蚯蚓粪(LMQ)共6个处理。调查了不同处理开花前苗期草莓植株地上部叶片及地下部根系的生长状况。【结果】土壤灭菌处理较相应未灭菌处理显著抑制了草莓花前幼苗阶段植株地下部的生长(P＜0.05),在果实成熟期、 盛果期及盛果末期植株生长均存在补长效应。土壤灭菌改变了草莓植株地上部和地下部正常的生长发育进程,植株不同发育阶段根冠比发生变化。无论连作土壤灭菌与否,施用无机肥料处理较施用有机肥处理显著抑制了根系生长(P＜0.05)。在不灭菌土壤上,施用蚯蚓粪处理草莓植株根系总长、 根系总表面积、 根尖数及根叉数与施用牛粪处理差异不显著,但灭菌土壤上,施加蚯蚓粪与施加牛粪相比,显著增加了草莓植株根系总长、 根系表面积及根叉数(P＜0.05)。【结论】蚯蚓粪与牛粪和无机肥料相比具有显著的生物活性。在草莓连作土壤灭菌后施用具有生物活性的蚯蚓粪,可以促进根系生长,缓解土壤灭菌对草莓植株生长发育的影响,是值得推荐的有效措施。     

Estimation of Crown Temperature of Winter Wheat and the Effect on Simulation of Frost Tolerance

Accurate estimation of winter wheat frost kill in cold‐temperate agricultural regions is limited by lack of data on soil temperature at wheat crown depth, which determines winter survival. We compared the ability of four models of differing complexity to predict observed soil temperature at 2 cm depth during two winter seasons (2013‐14 and 2014‐15) at Ultuna, Sweden, and at 1 cm depth at Ilseng and Ås, Norway. Predicted and observed soil temperature at 2 cm depth was then used in FROSTOL model simulations of the frost tolerance of winter wheat at Ultuna. Compared with the observed soil temperature at 2 cm depth, soil temperature was better predicted by detailed models than simpler models for both seasons at Ultuna. The LT50 (temperature at which 50 % of plants die) predictions from FROSTOL model simulations using input from the most detailed soil temperature model agreed better with LT50 FROSTOL outputs from observed soil temperature than what LT50 FROSTOL predictions using temperature from simpler models did. These results highlight the need for simpler temperature prediction tools to be further improved when used to evaluate winter wheat frost kill.