国内外有机肥标准对比及风险评价

中国是人口最多的发展中国家，生产生活中产生的有机废弃物数量巨大，堆制有机肥是降低有机废物污染风险的重要方式，而有机肥标准则是防止有机肥成为新的土壤污染源，规范有机肥产业健康发展的重要保障。目前我国有机肥不合格现象时有发生，针对有机堆肥的标准仅有一个8年前的行业标准（NY 525—2012）的现状，本文对比了中国、日本、澳大利亚、欧盟、美国有机肥标准的重要指标，对存在的重金属残留、抗生素污染、病原体污染、营养富集及土壤盐渍化等有机肥质量安全风险问题进行分析，为我国有机肥行业未来绿色、健康、可持续发展提出建议。尽管我国现有有机肥质量标准，在具体指标要求方面优于美国，但和欧盟相比还有差距，比如我国重金属Cu、Zn、Ni限量缺失，对Cd等重金属限值要求不够严格，长期施用会导致土壤重金属含量超过风险筛选值，严重影响农作物安全；同时，由于部分畜禽养殖业不合理使用抗生素，加之有机肥生产企业技术的欠缺，农户施用时缺乏指导，监管部门执法不严等因素，我国有机肥施用过程存在较大风险隐患。因此，进一步完善有机肥标准体系，强化对原料中有毒有害物质的限制，要求选用原料批批检，加大准入和过程的落实力度，才能保障我国有机肥产业有序健康发展。     

石灰联合碳铵熏蒸对连作香蕉生长和根际微生物群落结构的影响

摘 要：由于长期连作导致香蕉枯萎病大量爆发，造成香蕉种植面积锐减，已严重影响海南香蕉产业的发展，因而急需寻求能够缓解或克服香蕉连作障碍的有效措施。本实验旨在探究使用绿色土壤熏蒸剂对长期连作蕉园的香蕉枯萎病的防控效果，特别是对植株生长发育、土壤化学性质和根际微生物区系的影响。田间试验共设置两个处理：石灰碳铵熏蒸处理（LAB）和对照处理（CK）。结果表明: LAB处理可以显著降低香蕉枯萎病发病率，与CK处理相比两季分别降低40%和46.62%，显著增加香蕉亩产量，与CK处理相比两季分别增产45.56%和75.99%。LAB处理可以显著提高土壤pH，改善土壤酸化，使酸性土壤维持中性水平，同时，增加土壤有机质含量，并且显著提高土壤速效磷（两季分别提高28.33%和89.14%）和速效钾含量（23.92%和38.67%）。并且LAB处理明显改变香蕉根际微生物群落结构，可以显著降低变形菌门和子囊菌门相对丰度，显著增加放线菌门等相对丰度，同时显著降低病原菌镰刀菌属相对丰度，并且显著提高部分土壤拮抗菌属的相对丰度，如链霉菌属、红球菌属和曲霉属。因此，石灰碳铵熏蒸有效改善香蕉根际微生物群落结构，有效防控香蕉枯萎病的发生并促进其植株生长。     

芦笋种植对冷凉沙化区土壤改良的效果研究

为探索芦笋种植对冷凉沙化区土壤的改良效果,在山西省朔州市右玉县,以未种植芦笋裸沙地为对照（CK）,设置种植芦笋1、2、3和4年共4个处理,通过田间试验测定不同种植年限芦笋田土壤理化特性和芦笋生长发育情况。结果表明,与CK相比,随种植年限增加,土壤黏粒和粉砂粒含量递增,砂粒含量递减,土壤容重递减,土壤田间持水量递增;土壤pH和可溶性盐浓度（EC）递减;土壤有机质、全氮、有效磷和速效钾含量逐年递增。种植芦笋3年的土壤粒级、土壤容重、田间持水量、pH、EC值、土壤肥力发生显著变化;连续种植芦笋4年的土壤黏粒含量较CK增加到29.8%,粉砂粒含量增加到12.6%,砂粒含量降低到57.6%,田间土壤持水量显著提高,土壤容重显著降低,土壤由砂质壤土向砂质黏土转变;土壤pH降低0.75,EC值降低0.08mS/cm;土壤有机质含量增加28.89%,全氮、有效磷和速效钾含量分别增加95.12%、94.92%和45.40%;芦笋产量达6 037.5kg/hm ²。综合分析,连续种植芦笋4年可改善沙化土壤的物理结构,提高土壤养分,降低盐碱程度。芦笋是冷凉沙化区土壤改良的先锋作物之一,可实现生态效益与经济效益并举。     

Resettling,disconnecting or displacing? Attending to local sociality,culture and history in disaster settings

In many disaster settings, top‐down responses emphasise ‘expert‐led’ solutions that often involve relocating disaster‐affected communities. While the intention might be to move people from harm's way and facilitate recovery, failure to attend to local pre‐disaster circumstances as well as the interplay between power, resilience and vulnerability within and around affected communities often sees resettlement reconfigure as displacement or disconnection. This oversight may even usher in a new phase of dispossession and disadvantage for marginalised groups (particularly in colonial settings). This paper explores experiences in Australia, Japan and Taiwan to reflect on what issues of local sociality, local culture and local resilience need to be attended to in framing ‘better’ disaster responses.     

不同因素影响下层状土壤水分入渗特征及水力学参数估计

层状土壤是自然界常见的土体结构,其水分运移规律不同于均质土;大气降水、灌溉水等水分的入渗是土壤水文过程的一个重要环节,同时它也与地下水补给、污染物运移等过程紧密相关。土壤初始含水量、土体构型及供水强度等因素均会影响水分的入渗过程。为探究积水深度、土体构型、初始含水量三种因素对层状土壤水分运移的影响,通过室内积水入渗试验对湿润锋、累积入渗量、土壤剖面压力水头进行观测,并利用Hydrus-1D模型反演水力参数并对相应条件下的水分运移规律进行模拟和分析。结果表明,层状土壤中湿润锋随时间的推进方式由非线性过渡至线性,入渗率逐渐减小。三种因素作用下,层状土壤水分运移特征有明显差异:积水深度、土壤初始含水量增加时,湿润锋运移速率和入渗率均增大,且各观测点压力水头升高加快,土壤不饱和程度降低;上砂壤下粉砂壤构型较上粉砂壤下砂壤构型而言,整体湿润锋推进速率和入渗率较大,出流快,且入渗后期界面处的压力水头高于其他观测点。且结果表明,反演的水力学参数较拟合实测的参数更适用于层状土壤入渗的模拟和预测。该研究旨在揭示和掌握层状土壤水分运移规律和影响因素的作用机制,并进一步为农田灌溉措施的合理制定提供科学依据。     

Long-term fertilization leads to specific PLFA finger-prints in Chinese Hapludults soil

Soil microbes play essential roles in the biogeochemical processes of organic carbon and nutrient cycling. Many studies have reported various short-term effects of fertilization on soil microbes. However, less is known about the effects of longterm fertilization regimes on the rhizosphere. Therefore, the objective of this study was to explore how the soil microbial communities in the rhizosphere respond to different long-term fertilization strategies. Based on a 21-year field treatment experiment in Guizhou, China, we extracted phospholipid fatty acids(PLFAs) to determine the microbial community structure in both the non-rhizosphere(NR) and rhizosphere(R). Six treatments were included: no fertilizer(CK), mineral nitrogen fertilizer(N), N with potassium(NK), phosphorus with K(PK), NPK, and NPK combined with manure(MNPK). The results showed that total PLFAs under unbalanced mineral fertilization(N, NK and PK) were decreased by 45% on average in the NR compared with CK, whereas MNPK increased fungi and G~– bacteria abundance significantly in both the NR(by 33 and 23%) and R(by 15 and 20%), respectively. In addition, all microbial groups in the R under these treatments(N, NK and PK) were significantly increased relative to those in the NR, except for the ratio of F/B and G~+/G~–, which might be due to the high nutrient availability in the R. Soil pH and SOC significantly regulated the soil microbial community and structure, explaining 51 and 20% of the variation in the NR, respectively. However, the rhizosphere microbial community structure was only significantly affected by soil pH(31%). We concluded that the soil microbial community in the NR was more strongly affected by long-term fertilization than that in the R due to the rhizosphere effect in the agricultural ecosystem. Rhizosphere nutrient conditions and buffering capacity could help microbial communities resist the change from the long-term fertilization.     

Bacterial communities associated with natural and commercially grown rooibos (Aspalathus linearis)

Aspalathus linearis is a commercially important plant species endemic to the Cape Floristic Region of South Africa and is used to produce a herbal tea known as rooibos tea. Symbiotic interactions between A. linearis and soil bacteria play an important role in the survival of Aspalathus plants in the highly nutrient-poor, acidic fynbos soil. The aim of this study was to characterize and compare rhizosphere and bulk soil bacterial communities associated with natural and commercially grown A. linearis, as well as the effect of seasonal changes on these communities. Bacterial communities were characterized using high throughput amplicon sequencing, and their correlations with soil chemical properties were investigated. The N-fixing bacterial community was characterized using terminal restriction fragment length polymorphism and real time quantitative polymerase chain reaction. Actinobacteria, Proteobacteria, and Acidobacteria were the most dominant bacterial phyla detected in this study. Highly similar bacterial communities were associated with natural and commercially grown plants. Significant differences in the bacterial community were observed between rhizosphere and bulk soils collected in the dry season, while no significant differences were detected in the wet season. This study provides insights into bacterial community structure and potential factors shaping bacterial community structure with commercially important A. linearis.     

典型喀斯特洼地植被恢复过程中土壤碳氮储量动态及其对极端内涝灾害的响应

西南喀斯特地区是我国主要的生态脆弱区之一,石漠化严重,旱涝灾害频发。植被恢复是提升脆弱生态系统土壤碳氮固持的有效方式,但该区不同植被恢复方式土壤碳氮动态监测的研究还很缺乏。本研究以典型喀斯特峰丛洼地为对象,选取人工林、牧草地、人工林+牧草地、撂荒地自然恢复4种最主要的植被恢复方式为研究对象,以耕地作为对照,对比分析退耕前(2004年)、退耕10年(2014年)和13年后(2017年)土壤碳氮储量动态变化特征。其中2004—2014年研究区未发生极端内涝灾害, 2014—2017年连续发生2次极端内涝灾害事件。研究结果表明,退耕10年后, 4种恢复方式下土壤有机碳(SOC)储量均显著增加,但退耕13年后,除撂荒地SOC持续增加外,其他3种恢复方式下SOC表现出下降趋势。植被恢复后土壤全氮(TN)储量提升相对缓慢,退耕10年仅牧草地显著增加,退耕13年后人工林+牧草和撂荒地TN增加,且撂荒地在退耕后呈持续增加趋势。相关性分析结果表明,土壤交换性Ca~(2+)与SOC、TN均呈显著正相关关系,且与2014年相比, 2017年不同植物恢复方式下土壤交换性Ca~(2+)均显著下降,这可能与研究区2015年和2016年连续内涝灾害有关。以上结果说明,不同恢复方式均能显著提升喀斯特地区土壤碳氮固持,并以自然恢复最佳,其生态系统能有效抵御极端气候灾害带来的负面影响。     

旱作农田种植碳排放主要因素 及减排措施研究

农业生产是温室气体排放第二大排放源,降低农业生产的碳排放具有意义重大。本文梳理了种植生产过程中碳排放相关的文献,发现种植过程产生碳排放的主要因素之一是化肥的生产和使用。通过优化秸秆和肥料利用模式成为化肥减施和替代的重要途径,综合考虑了农田碳排放和土壤固碳,为进一步研究旱作农田减排措施提供参考。     

基于landsat8的贵州省2015年农业干旱监测研究

在全球气候变暖背景下,干旱普遍发生,而农业干旱对国民经济发展的影响尤为明显,同时农业干旱还威胁着国家的粮食安全和生态安全。基于贵州省2015年不同季节的landsat8 OIL遥感数据,利用影像数据所获取的植被覆盖指数和地表温度数据,拟合植被指数(NDVI)和地表温度(LST)的特征空间,设计得到贵州省2015年春、夏、秋、冬四个不同季节的不同的土壤湿度,将TVDI作为监测农业干旱状况的指标,得到贵州省2015年的农业干旱时空分布图。结果表明,土壤含水率的高低与植被覆盖和地表温度有关,且TVDI更适宜中等植被覆盖的土壤湿度反演。贵州省2015年全年旱情较缓,各地区均不存在春旱或伏旱,只有冬季绝大部分地区土壤含水率较低,更有力地促进了农业干旱的发生。因此,对农业干旱的监测研究为贵州省农业干旱的监测管理提供有力依据,为今后减少农业干旱的影响和进一步促进农业社会经济可持续发展具有重要的现实意义。