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Evaluation of the Relationship Between Dopamine Receptor D2 Gene TaqIA1 Polymorphism and Alcohol Dependence Risk. 评估多巴胺受体 D2 基因 TaqIA1 多态性与酗酒风险之间的关系
IF 1.5 4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2024-07-01 Epub Date: 2023-03-31 DOI: 10.1007/s12291-023-01122-7
Pradeep Kumar, Amrita Chaudhary, Vandana Rai

Several studies are published, that investigated dopamine receptor 2 (DRD2) gene TaqIA polymorphism as a risk factor for alcohol dependence (AD) with positive and negative associations. To derive a more precise estimation of the relationship, a meta-analysis of case-control studies that examined the association between DRD2 gene Taq1A polymorphism and alcohol dependence was performed. Eligible articles were identified through a search of databases including PubMed, Science Direct, Springer link, and Google Scholar. The association between the DRD2 TaqIA polymorphism and AD susceptibility was conducted using odds ratios (ORs) and 95% confidence intervals (95% CIs) as association measures. A total of 69 studies with 9125 cases and 9123 healthy controls were included in the current meta-analysis. Results of the present analysis showed significant association between DRD2 TaqIA polymorphism and AD risk using five genetic modes (allele contrast model-OR 1.22, 95% CI 1.13-1.32, p < 0.0001; homozygote model-OR 1.35, 95%CI 1.18-1.55; p ≤ 0.0001; dominant model-OR 1.29; 95% CI 1.20-1.39; p < 0.0001; recessive model-OR 1.21; 95% CI 1.08-1.36; p = 0.0006). There was no significant association found in subgroup analysis, TaqIA polymorphism was not significantly associated with AD risk in the Asian population under all genetic models, but in the Caucasian population, TaqIA polymorphism was significantly associated with AD risk. Overall, results support the hypothesis that DRD2 Taq1A polymorphism plays a role in alcohol dependence.

已发表的几项研究调查了多巴胺受体 2(DRD2)基因 TaqIA 多态性与酒精依赖症(AD)风险因素之间的正负关系。为了更精确地估计两者之间的关系,我们对研究 DRD2 基因 Taq1A 多态性与酒精依赖关系的病例对照研究进行了荟萃分析。符合条件的文章是通过搜索包括PubMed、Science Direct、Springer link和Google Scholar在内的数据库确定的。DRD2 TaqIA基因多态性与AD易感性之间的关联采用几率比(ORs)和95%置信区间(95% CIs)作为关联测量指标。本次荟萃分析共纳入了 69 项研究,包括 9125 例病例和 9123 例健康对照。本分析结果显示,在五种遗传模式(等位基因对比模式-OR 1.22,95% CI 1.13-1.32,p p ≤ 0.0001;显性模式-OR 1.29;95% CI 1.20-1.39;p p = 0.0006)下,DRD2 TaqIA多态性与AD风险之间存在显著关联。在亚组分析中没有发现明显的关联,在所有遗传模型中,TaqIA多态性与亚洲人群的AD风险没有明显关联,但在白种人群中,TaqIA多态性与AD风险有明显关联。总之,研究结果支持 DRD2 Taq1A 多态性在酒精依赖中发挥作用的假设。
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引用次数: 0
A weaponized phage suppresses competitors in historical and modern metapopulations of pathogenic bacteria. 一种武器化噬菌体抑制了历史上和现代病原菌元种群中的竞争者。
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2024-02-02 DOI: 10.1101/2023.04.17.536465
Talia Backman, Sergio M Latorre, Efthymia Symeonidi, Artur Muszyński, Ella Bleak, Lauren Eads, Paulina I Martinez-Koury, Sarita Som, Aubrey Hawks, Andrew D Gloss, David M Belnap, Allison M Manuel, Adam M Deutschbauer, Joy Bergelson, Parastoo Azadi, Hernán A Burbano, Talia L Karasov

Bacteriophages, the viruses of bacteria, are proposed to drive bacterial population dynamics, yet direct evidence of their impact on natural populations is limited. Here we identified viral sequences in a metapopulation of wild plant-associated Pseudomonas spp. genomes. We discovered that the most abundant viral cluster does not encode an intact phage but instead encodes a tailocin - a phage-derived element that bacteria use to kill competitors for interbacterial warfare. Each pathogenic Pseudomonas sp. strain carries one of a few distinct tailocin variants, which target variable polysaccharides in the outer membrane of co-occurring pathogenic strains. Analysis of historic herbarium samples from the last 170 years revealed that the same tailocin and receptor variants have persisted in the Pseudomonas populations for at least two centuries, suggesting the continued use of a defined set of tailocin haplotypes and receptors. These results indicate that tailocin genetic diversity can be mined to develop targeted "tailocin cocktails" for microbial control.

One-sentence summary: Bacterial pathogens in a host-associated metapopulation use a repurposed prophage to kill their competitors.

噬菌体是细菌的病毒,被认为是细菌种群动态的驱动力,但它们对自然种群影响的直接证据却很有限。在这里,我们确定了野生植物相关假单胞菌属基因组元群中的病毒序列。我们发现,最丰富的病毒簇并不编码完整的噬菌体,而是编码一种噬菌体衍生元素--尾蛋白,细菌利用这种元素杀死竞争者,进行细菌间战争。每种致病假单胞菌株都携带几种不同的尾孢菌素变体之一,这些变体的目标是共生致病菌株外膜上的可变多糖。对过去 170 年历史标本馆样本的分析表明,相同的尾丝菌素和受体变体在假单胞菌种群中至少存在了两个世纪,这表明一组确定的尾丝菌素单倍型和受体仍在继续使用。这些结果表明,可以利用尾孢素遗传多样性来开发有针对性的 "尾孢素鸡尾酒",以控制微生物。
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引用次数: 0
Research and management challenges following soil and landscape decontamination at the onset of the reopening of the Difficult-to-Return Zone, Fukushima (Japan) 日本福岛难返回区重新开放初期土壤和景观净化后的研究和管理挑战
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-09-06 DOI: 10.5194/soil-9-479-2023
O. Evrard, Thomas Chalaux-Clergue, Pierre-Alexis Chaboche, Y. Wakiyama, Y. Thiry
Abstract. Twelve years after the nuclear accident that occurred at theFukushima Dai-ichi Nuclear Power Plant (FDNPP) in March 2011, radiocesiumcontamination (with a large dominance of 137Cs, with a 30-yearhalf-life) remains a major concern in various municipalities of north-easternJapan. The Japanese authorities completed an unprecedented soildecontamination programme in residential and cultivated areas affected bythe main radioactive plume (8953 km2). They implemented acomplex remediation programme scheme to remediate soils that are fundamentalto life on Earth, relying on different decision rules depending on the wastetype, its contamination level and its region of origin, after delineatingdifferent zones exposed to contrasted radiation rates. The central objectivewas not to expose local inhabitants to radioactive doses exceeding 1 mSv yr−1 in addition to the natural levels. At the onset of the fullreopening of the Difficult-to-Return Zone (DTRZ) in spring 2023, the current reviewprovides an update of a previous synthesis published in 2019(Evrard et al., 2019). Although this ambitious soil remediationand reconstruction programme has almost been completed in the 12 municipalitiesof Fukushima Prefecture in which an evacuation order was imposed in at leastone neighbourhood in 2011, from the 147 443 inhabitants who lived therebefore the accident, only 29.9 % of them had returned by 2020. Wastegenerated by decontamination and tsunami cleaning/demolition work is plannedto have been fully transported to (interim) storage facilities by the end of2023. The cost of the operations conducted between 2011 and 2020 for theso-called “nuclear recovery” operations (including decontamination) wasestimated by the Board of Audit of Japan in 2023 as JPY 6122.3 billion(∼ EUR 44 billion). Decontamination of cropland was shown tohave impacted soil fertility, and potassium fertilisation is recommended tolimit the transfer of residual radiocesium to new crops. In forests thatcover 71 % of the surface area of Fukushima Prefecture and that werenot targeted by remediation, radiocesium is now found in the upper minerallayer of the soil in a quasi-equilibrium state. Nevertheless, 137Csconcentrations in forest products (including wood for heating andconstruction, wild plants, wildlife game, mushrooms) often keep exceedingthe threshold values authorised in Japan, which prohibits their exploitationin the area affected by the main plume. Radionuclides from forests were shownto be exported in dissolved and particle-bound forms to downstream riversystems and floodplains, although multiple monitoring records showed thecontinuous decrease in radiocesium concentrations in both river water andsediment across the main plume between 2011 and 2021. Fish contamination is nowgenerally found to be below the threshold limits although reputational damageremains a major concern for local fishing communities. The remobilisation ofradiocesium from sediment
摘要2011年3月福岛第一核电站(FDNPP)发生核事故12年后,放射性污染(主要是137Cs,半衰期为30年)仍然是日本东北部许多城市的主要问题。日本当局在受主要放射性羽流影响的住宅和耕地地区(8953平方公里)完成了一项前所未有的土壤净化计划。他们实施了一项复杂的修复计划来修复土壤,土壤是地球上生命的基础,在划定了暴露于对比辐射率的不同区域之后,根据废物类型、污染程度和来源地区的不同,他们采用了不同的决策规则。中心目标是不使当地居民暴露在超过自然水平1毫西弗/年- 1的放射性剂量下。在2023年春季难以返回区(DTRZ)全面重新开放的开始,当前的综述提供了2019年发表的先前综合的更新(Evrard et al., 2019)。尽管这个雄心勃勃的土壤修复和重建计划在福岛县的12个市(2011年至少有一个社区被下令撤离)几乎已经完成,但到2020年,事故发生前居住在那里的147443名居民中,只有29.9%的人返回了家园。除污和海啸清理/拆除工作产生的废物计划在2023年底前全部运送到(临时)储存设施。据2023年日本审计委员会估计,2011年至2020年期间进行的所谓“核回收”操作(包括去污)的成本为61223亿日元(约440亿欧元)。农田去污已被证明影响了土壤肥力,钾肥被建议限制残留放射性元素向新作物的转移。在覆盖福岛县71%地表面积的森林中,并不是修复的目标,现在在土壤的上层矿物层中发现了放射性,处于准平衡状态。然而,森林产品(包括取暖和建筑用木材、野生植物、野生动物、蘑菇)中的铯浓度经常超过日本规定的阈值,日本禁止在受主要烟羽影响的地区开采这些产品。来自森林的放射性核素以溶解和颗粒结合的形式输出到下游河流系统和洪泛平原,尽管多个监测记录显示,在2011年至2021年期间,主要羽流的河水和沉积物中的放射性核素浓度持续下降。尽管声誉损害仍然是当地渔业社区主要关注的问题,但鱼类污染现在普遍低于阈值限制。该地区水库沉积物中放射性元素的再活化也是一个潜在的问题,因为它可能导致鱼类或供应给净化农田的灌溉用水受到二次污染。总的来说,这一综合表明需要继续监测这些环境中事故后的放射性转移,并保持数据共享,以改进对放射性迁移的预测性理解,并巩固可用的工具来模拟生态系统中的污染物转移。特别是在森林方面,新的对策和木材利用仍有待发展和试验。此外,不同生态系统下土壤的水文连通性对放射性元素的长期迁移影响很大。应进一步预测由于全球变化在这些受污染环境中可能变得更加频繁的极端现象(例如台风、森林火灾)的后果。
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引用次数: 1
Earthworm-invaded boreal forest soils harbour distinct microbial communities 蚯蚓入侵的北方森林土壤有独特的微生物群落
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-08-29 DOI: 10.5194/soil-9-461-2023
J. Lejoly, S. Quideau, J. Laganière, Justine Karst, C. Martineau, M. Swallow, C. Norris, A. Samad
Abstract. Earthworm invasion in North American forests has thepotential to greatly impact soil microbial communities by altering soilphysicochemical properties, including structure, pH, nutrient availability,and soil organic matter (SOM) dynamics. While most research on the topic hasbeen carried out in northern temperate forests, little is known about theimpact of invasive earthworms on soil microbial communities in hemiborealand boreal forests, characterized by a slower decay of organic matter (OM).Earthworm activities can increase OM mineralization, altering nutrientcycling and biological activity in a biome where low carbon (C) and nitrogen(N) availability typically limits microbial and plant growth. Here, wecharacterized and compared microbial communities of earthworm-invaded andnon-invaded soils in previously described sites across three major soiltypes found in the Canadian (hemi)boreal forest using a space-for-timeapproach. Microbial communities of forest floors and surface mineral soilswere characterized using phospholipid fatty acid (PLFA) analysis andmetabarcoding of the 16S rRNA gene for bacteria and archaea and of the internal-transcriber-spacer-2 (ITS2) region for fungi. In forest floors, the effects of earthworm invasion wereminor. In mineral soil horizons, earthworm invasion was associated withhigher fungal biomass and greater relative abundance of ectomycorrhizalfungi. Oligotrophic bacteria (Acidobacteriota and Chloroflexi) were lessabundant in invaded mineral soils, where Gram(+) : Gram(−) ratios were alsolower, while the opposite was observed for the copiotrophic Bacteroidota.Additionally, earthworm-invaded mineral soils harboured higher fungal andbacterial species diversity and richness. Considering the important role ofsoil microbial communities for ecosystem functioning, such earthworm-inducedshifts in their community composition are likely to impact nutrient cycling,as well as vegetation development and forest productivity at a large scale,as the invasion progresses in these (hemi)boreal systems.
摘要蚯蚓入侵北美森林有可能通过改变土壤的物理化学性质,包括结构、pH值、养分有效性和土壤有机质(SOM)动态,极大地影响土壤微生物群落。虽然大多数关于这一主题的研究都是在北温带森林中进行的,但人们对入侵蚯蚓对半北方森林和北方森林土壤微生物群落的影响知之甚少,这些森林的特征是有机物(OM)的衰变较慢。蚯蚓的活动可以增加有机质矿化,改变生物群落的营养循环和生物活性,而低碳(C)和氮(N)的可用性通常限制微生物和植物的生长。在这里,我们使用空间-时间方法对加拿大(半)北方森林中发现的三种主要土壤类型的蚯蚓入侵和非入侵土壤的微生物群落进行了表征和比较。利用磷脂脂肪酸(PLFA)分析和16S rRNA基因的元条形码编码,对细菌和古细菌以及真菌的内部转录间隔-2 (ITS2)区域进行了分析,对森林地面和地表矿物土壤的微生物群落进行了表征。在森林地面,蚯蚓入侵的影响很小。在矿质土壤层,蚯蚓入侵与较高的真菌生物量和较高的外生菌根真菌相对丰度有关。在入侵的矿质土壤中,少营养细菌(酸杆菌门和绿杆菌门)的数量较少,革兰氏(+):革兰氏(−)比值也较低,而多营养拟杆菌门的数量则相反。此外,蚯蚓入侵的矿质土壤具有更高的真菌和细菌物种多样性和丰富度。考虑到土壤微生物群落对生态系统功能的重要作用,随着这些(半)北方系统的入侵进展,蚯蚓引起的群落组成的变化可能会影响养分循环、植被发育和森林生产力。
{"title":"Earthworm-invaded boreal forest soils harbour distinct microbial communities","authors":"J. Lejoly, S. Quideau, J. Laganière, Justine Karst, C. Martineau, M. Swallow, C. Norris, A. Samad","doi":"10.5194/soil-9-461-2023","DOIUrl":"https://doi.org/10.5194/soil-9-461-2023","url":null,"abstract":"Abstract. Earthworm invasion in North American forests has the\u0000potential to greatly impact soil microbial communities by altering soil\u0000physicochemical properties, including structure, pH, nutrient availability,\u0000and soil organic matter (SOM) dynamics. While most research on the topic has\u0000been carried out in northern temperate forests, little is known about the\u0000impact of invasive earthworms on soil microbial communities in hemiboreal\u0000and boreal forests, characterized by a slower decay of organic matter (OM).\u0000Earthworm activities can increase OM mineralization, altering nutrient\u0000cycling and biological activity in a biome where low carbon (C) and nitrogen\u0000(N) availability typically limits microbial and plant growth. Here, we\u0000characterized and compared microbial communities of earthworm-invaded and\u0000non-invaded soils in previously described sites across three major soil\u0000types found in the Canadian (hemi)boreal forest using a space-for-time\u0000approach. Microbial communities of forest floors and surface mineral soils\u0000were characterized using phospholipid fatty acid (PLFA) analysis and\u0000metabarcoding of the 16S rRNA gene for bacteria and archaea and of the internal-transcriber-spacer-2 (ITS2) region for fungi. In forest floors, the effects of earthworm invasion were\u0000minor. In mineral soil horizons, earthworm invasion was associated with\u0000higher fungal biomass and greater relative abundance of ectomycorrhizal\u0000fungi. Oligotrophic bacteria (Acidobacteriota and Chloroflexi) were less\u0000abundant in invaded mineral soils, where Gram(+) : Gram(−) ratios were also\u0000lower, while the opposite was observed for the copiotrophic Bacteroidota.\u0000Additionally, earthworm-invaded mineral soils harboured higher fungal and\u0000bacterial species diversity and richness. Considering the important role of\u0000soil microbial communities for ecosystem functioning, such earthworm-induced\u0000shifts in their community composition are likely to impact nutrient cycling,\u0000as well as vegetation development and forest productivity at a large scale,\u0000as the invasion progresses in these (hemi)boreal systems.\u0000","PeriodicalId":22015,"journal":{"name":"Soil Science","volume":"25 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-08-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"91090959","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Tropical Andosol organic carbon quality and degradability in relation to soil geochemistry as affected by land use 受土地利用影响的热带土壤有机碳质量和可降解性与土壤地球化学的关系
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-07-31 DOI: 10.5194/soil-9-443-2023
Sastrika Anindita, P. Finke, S. Sleutel
Abstract. Land use is recognized to impact soil geochemistry on the centennial to millennial timescale, with implications for the distribution and stabilityof soil organic carbon (SOC). Young volcanic soils in tropical areas are subject to much faster pedogenesis, noticeable already on the centennial oreven decadal timescale. As land use is a recognized factor for soil formation, it is thus conceivable that even relatively recent land use conversion insuch areas would already bear a significant impact on the resulting formed soils., e.g., in terms of content of pedogenic oxides. Very scarceobservational evidence exists, so such indirect implications of land use on SOC cycling are largely unknown. We here investigated SOC fractions,substrate-specific mineralization (SOC or added plant residue), and net priming of SOC as a function of forest or agricultural land use on Indonesianvolcanic soils. The content of oxalate-extracted Al (Alo) correlated well with organic carbon (OC) associated with sand-sized aggregates,particularly in the subsoil. The proportion of SOC in sand-sized ultrasonication-resistant (400 J mL−1) aggregates was also higher inagricultural land use compared to pine forest land use, and a likewise contrast existed for Alo. These combined observations suggest that enhancedformation of Al (hydr)oxides promoted aggregation and physical occlusion of OC. This was, importantly, also consistent with a relatively lesserdegradability of SOC in the agricultural sites, though we found no likewise difference in degradability of added 13C-labeled ryegrass orin native SOC priming between the pine forest and agricultural land uses. We expected that amorphous Al content under agricultural land usewould mainly have promoted mineral association of SOC compared to under pine forest land use but found no indications for this. Improved small-scaleaggregation of tropical Andosols caused by conversion to agriculture and high carbon input via organic fertilizer may thus partially counter theotherwise expectable decline of SOC stocks following cultivation. Such indirect land use effects on the SOC balance appeared relevant for correctinterpretation and prediction of the long-term C balance of (agro)ecosystems with soil subject to intense development, like the here-studied tropical Andosols.
摘要土地利用在百年至千年时间尺度上影响土壤地球化学,影响土壤有机碳(SOC)的分布和稳定性。热带地区年轻的火山土壤的成土作用要快得多,这在百年甚至十年的时间尺度上已经很明显了。由于土地利用是土壤形成的一个公认因素,因此可以想象,即使在这些地区最近的土地利用转换也会对由此形成的土壤产生重大影响。,例如,就成土氧化物的含量而言。很少有观测证据存在,因此土地利用对有机碳循环的间接影响在很大程度上是未知的。本文研究了印尼火山土壤中有机碳组分、基质特定矿化(有机碳或添加的植物残渣)和有机碳净底质对森林或农业用地的影响。草酸盐提取的Al (Alo)含量与砂级团聚体的有机碳(OC)具有良好的相关性,特别是在底土中。土壤有机碳在沙粒级抗超声(400 J mL−1)团聚体中的比例在农业用地中也高于松林用地,在Alo中也存在类似的对比。这些综合观察表明,铝(氢氧)氧化物的形成增强促进了OC的聚集和物理闭塞。重要的是,这也与农业用地中相对较低的有机碳可降解性相一致,尽管我们发现添加13c标记的黑麦草或天然有机碳在松林和农业用地之间的可降解性没有类似的差异。我们预计,与松林用地相比,农业用地下无定形铝含量主要促进有机碳的矿物关联,但没有发现这方面的迹象。由农业转化和通过有机肥的高碳输入引起的热带土壤小规模聚集的改善可能部分抵消耕作后SOC储量的预期下降。这种土地利用对有机碳平衡的间接影响似乎与正确解释和预测具有强烈发展的土壤的(农业)生态系统的长期碳平衡有关,如本文研究的热带安土。
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引用次数: 0
Mapping land degradation risk due to land susceptibility to dust emission and water erosion 基于土地易受粉尘排放和水土流失影响的土地退化风险制图
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-07-13 DOI: 10.5194/soil-9-411-2023
Mahdi Boroughani, Fahimeh Mirchooli, M. Hadavifar, S. Fiedler
Abstract. Land degradation is a cause of many social, economic, and environmentalproblems. Therefore identification and monitoring of high-risk areas forland degradation are necessary. Despite the importance of land degradationdue to wind and water erosion in some areas of the world, the combined studyof both types of erosion in the same area receives relatively littleattention. The present study aims to create a land degradation map in termsof soil erosion caused by wind and water erosion of semi-dry land. We focuson the Lut watershed in Iran, encompassing the Lut Desert that is influencedby both monsoon rainfalls and dust storms. Dust sources are identified usingMODIS satellite images with the help of four different indices to quantifyuncertainty. The dust source maps are assessed with three machine learningalgorithms encompassing the artificial neural network (ANN), random forest (RF),and flexible discriminant analysis (FDA) to map dust sources paired withsoil erosion susceptibility due to water. We assess the accuracy of the mapsfrom the machine learning results with the area under the curve (AUC)of the receiver operating characteristic (ROC) metric. The water and aeolian soilerosion maps are used to identify different classes of land degradationrisks. The results show that 43 % of the watershed is prone to landdegradation in terms of both aeolian and water erosion. Most regions(45 %) have a risk of water erosion and some regions (7 %) a risk ofaeolian erosion. Only a small fraction (4 %) of the total area of theregion had a low to very low susceptibility for land degradation. Theresults of this study underline the risk of land degradation for in aninhabited region in Iran. Future work should focus on land degradationassociated with soil erosion from water and storms in larger regions toevaluate the risks also elsewhere.
摘要土地退化是许多社会、经济和环境问题的一个原因。因此,确定和监测土地退化高风险地区是必要的。尽管在世界上一些地区由于风蚀和水蚀导致的土地退化很重要,但在同一地区对两种侵蚀的综合研究相对较少受到关注。本研究旨在建立半干旱土地风蚀和水蚀引起的土壤侵蚀的土地退化图。我们关注的是伊朗的卢特流域,包括受季风降雨和沙尘暴影响的卢特沙漠。利用modis卫星图像识别尘源,借助四种不同的指数来量化不确定性。通过人工神经网络(ANN)、随机森林(RF)和灵活判别分析(FDA)等三种机器学习算法对尘源图进行评估,以绘制与水引起的土壤侵蚀敏感性配对的尘源图。我们用接受者工作特征(ROC)度量的曲线下面积(AUC)来评估机器学习结果的地图准确性。水和风成土壤侵蚀图用于识别不同类型的土地退化风险。结果表明,43%的流域在风蚀和水蚀方面都容易发生土地退化。大多数地区(45%)存在水蚀风险,一些地区(7%)存在风蚀风险。该地区只有一小部分(4%)的土地退化易感性为低至极低。这项研究的结果强调了伊朗无人居住地区土地退化的风险。未来的工作应该集中在更大地区与水和风暴造成的土壤侵蚀有关的土地退化,以评估其他地方的风险。
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引用次数: 0
Validating plutonium-239+240 as a novel soil redistribution tracer – a comparison to measured sediment yield 验证钚-239+240作为一种新的土壤再分配示踪剂-与测量的沉积物产量的比较
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-07-11 DOI: 10.5194/soil-9-399-2023
K. Meusburger, P. Porto, Judith Kobler Waldis, C. Alewell
Abstract. Quantifying soil redistribution rates is a global challenge addressed withdirect sediment measurements (e.g. traps), models, and isotopic, geochemical,and radionuclide tracers. The isotope of plutonium, namely 239+240Pu,is a relatively new soil redistribution tracer in this challenge. Directvalidation of 239+240Pu as a soil redistribution tracer is, however, stillmissing. We used a unique sediment yield time series in southern Italy,reaching back to the initial fallout of 239+240Pu to verify239+240Pu as a soil redistribution tracer. Distributed soil samples(n=55) were collected in the catchment, and at undisturbed reference sites(n=22), 239+240Pu was extracted, measured with inductively coupled plasma mass spectrometry (ICP-MS), and convertedto soil redistribution rates. Finally, we used a generalized additive model(GAM) to regionalize soil redistribution estimates for the catchment. Forthe catchment sites, mean 239+240Pu inventories were significantlyreduced (16.8 ± 10.2 Bq m−2) compared to the reference inventory(40.5 ± 3.5 Bq m−2), indicating the dominance of erosion.Converting these inventory losses into soil erosion rates resulted in anaverage soil loss of 22.2 ± SD 7.2 t ha−1 yr−1. Theuncertainties of the approach stemmed mainly from the high measurementuncertainties of some low-activity samples where samples have been bulkedover depth. Therefore, we recommend taking incremental soil samples andextracting larger soil volumes (∼ 20 g). The geographiccoordinates and the flow accumulation best described the spatial pattern oferosion rates in the GAM model. Using those predictors to upscale Pu-derivedsoil redistribution rates for the entire catchment resulted in an averageon-site loss of 20.7 t ha−1 yr−1, which corresponds very well tothe long-term average sediment yield of 18.7 t ha−1 yr−1 measured at the catchment outlet and to 137Cs-derived soilredistribution rates. Overall, this comparison of Pu-derived soilredistribution rates with measured sediment yield data validates239+240Pu as a suitable retrospective soil redistribution tracer.
摘要土壤再分配速率的量化是一项全球性挑战,可通过直接沉积物测量(如捕集器)、模型以及同位素、地球化学和放射性核素示踪剂来解决。钚的同位素,即239+240Pu,是该挑战中相对较新的土壤再分配示踪剂。然而,239+240Pu作为土壤再分配示踪剂的直接验证仍然缺失。我们在意大利南部使用了一个独特的沉积物产量时间序列,追溯到239+240Pu的初始沉降,以验证239+240Pu作为土壤再分配示踪剂。收集集水区分布的土壤样品(n=55),在未受干扰的参考点(n=22)提取239+240Pu,用电感耦合等离子体质谱(ICP-MS)测定,并转化为土壤再分配率。最后,我们使用广义加性模型(GAM)对流域土壤再分配估算进行区划。与参考库存量(40.5±3.5 Bq m−2)相比,流域平均239+240Pu库存量(16.8±10.2 Bq m−2)显著减少,表明侵蚀占主导地位。将这些库存损失转化为土壤侵蚀速率,平均土壤流失量为22.2±SD 7.2 t / h - 1年- 1。该方法的不确定度主要源于一些低活度样品的高测量不确定度,其中样品已在深度上膨胀。因此,我们建议增加土壤样品并提取更大的土壤体积(~ 20 g)。在GAM模型中,地理坐标和水流累积最能描述侵蚀速率的空间格局。利用这些预测因子对整个流域的土壤再分配率进行估算,结果表明现场平均损失为20.7 t ha - 1 yr - 1,这与在流域出口测量的长期平均产沙量18.7 t ha - 1 yr - 1和137cs导出的土壤再分配率非常吻合。总的来说,这种由pu衍生的土壤再分配率与测量的产沙量数据的比较验证了239+240Pu是一种合适的回顾性土壤再分配示踪剂。
{"title":"Validating plutonium-239+240 as a novel soil redistribution tracer – a comparison to measured sediment yield","authors":"K. Meusburger, P. Porto, Judith Kobler Waldis, C. Alewell","doi":"10.5194/soil-9-399-2023","DOIUrl":"https://doi.org/10.5194/soil-9-399-2023","url":null,"abstract":"Abstract. Quantifying soil redistribution rates is a global challenge addressed with\u0000direct sediment measurements (e.g. traps), models, and isotopic, geochemical,\u0000and radionuclide tracers. The isotope of plutonium, namely 239+240Pu,\u0000is a relatively new soil redistribution tracer in this challenge. Direct\u0000validation of 239+240Pu as a soil redistribution tracer is, however, still\u0000missing. We used a unique sediment yield time series in southern Italy,\u0000reaching back to the initial fallout of 239+240Pu to verify\u0000239+240Pu as a soil redistribution tracer. Distributed soil samples\u0000(n=55) were collected in the catchment, and at undisturbed reference sites\u0000(n=22), 239+240Pu was extracted, measured with inductively coupled plasma mass spectrometry (ICP-MS), and converted\u0000to soil redistribution rates. Finally, we used a generalized additive model\u0000(GAM) to regionalize soil redistribution estimates for the catchment. For\u0000the catchment sites, mean 239+240Pu inventories were significantly\u0000reduced (16.8 ± 10.2 Bq m−2) compared to the reference inventory\u0000(40.5 ± 3.5 Bq m−2), indicating the dominance of erosion.\u0000Converting these inventory losses into soil erosion rates resulted in an\u0000average soil loss of 22.2 ± SD 7.2 t ha−1 yr−1. The\u0000uncertainties of the approach stemmed mainly from the high measurement\u0000uncertainties of some low-activity samples where samples have been bulked\u0000over depth. Therefore, we recommend taking incremental soil samples and\u0000extracting larger soil volumes (∼ 20 g). The geographic\u0000coordinates and the flow accumulation best described the spatial pattern of\u0000erosion rates in the GAM model. Using those predictors to upscale Pu-derived\u0000soil redistribution rates for the entire catchment resulted in an average\u0000on-site loss of 20.7 t ha−1 yr−1, which corresponds very well to\u0000the long-term average sediment yield of 18.7 t ha−1 yr−1 measured at the catchment outlet and to 137Cs-derived soil\u0000redistribution rates. Overall, this comparison of Pu-derived soil\u0000redistribution rates with measured sediment yield data validates\u0000239+240Pu as a suitable retrospective soil redistribution tracer.\u0000","PeriodicalId":22015,"journal":{"name":"Soil Science","volume":"35 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2023-07-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"87083356","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Pesticide transport through the vadose zone under sugarcane in the Wet Tropics, Australia 在澳大利亚潮湿的热带地区,农药通过甘蔗下的渗透带运输
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-07-05 DOI: 10.5194/soil-9-381-2023
Rezaul Karim, L. Reading, L. Dawes, O. Dahan, Glynis Orr
Abstract. Photosystem II (PS II) pesticides, recognized as a threatto ecological health, were targeted for reduction in sugarcane farming inGreat Barrier Reef (GBR) catchments. Alternative herbicides, the non-PSII herbicides (including glyphosate, paraquat, 2,4-D, imazapic,isoxaflutole, metolachlor, and S-metolachlor), continue to be used in thesecatchments. However, the potential ecological fate, transport, and off-siteenvironmental effects of non-PS II herbicides, with respect to their usagescheme, local rainfall patterns, and infiltration dynamics, have not beeninvestigated previously. A vadose zone monitoring system, instrumentedbeneath sugarcane land in a GBR catchment, was applied for real-timetracing of pesticide migration across the unsaturated zone, past the rootzone during 2017–2019. The regularly applied pesticides (fluroxypyr andisoxaflutole) exhibited substantial migration through the unsaturated zone.Within 1 month of application of fluroxypyr, it leached to 2.87 m depthin the vadose zone, with declining concentrations with depth. Isoxaflutole,which was applied yearly, was found only once, in November 2018, at 3.28 m depth in the soil profile. Other pesticides (imazapic, metolachlor,glyphosate, and haloxyfop) applied during the same period were not detectedin the vadose zone. However, imidacloprid, which was not applied at thesite during the monitored period, was detected across the entire vadosezone, revealing substantial resistance to degradation. The results show noevidence of any regularly applied pesticides in the site bores at the end ofthe study, indicating their ultimate degradation within the vadose zonebefore reaching the groundwater.
摘要光系统II (PS II)农药被认为是对生态健康的威胁,是大堡礁(GBR)流域甘蔗种植减少的目标。替代除草剂,非psii除草剂(包括草甘膦、百草枯、2,4- d、异马唑、异草柳酮、异甲草胺和s -异甲草胺)继续在这些流域中使用。然而,非ps II除草剂在使用方案、当地降雨模式和入渗动态方面的潜在生态命运、运输和场外环境影响尚未得到研究。2017-2019年,在GBR集水区甘蔗地地下安装了一个渗透区监测系统,用于实时追踪农药在不饱和区越过根区的迁移。常用农药氟嘧菌酯和二恶氟唑通过不饱和区迁移。氟氧吡啶在施用1个月内,渗透深度达到2.87 m,浓度随深度下降。每年使用的异草氟唑仅在2018年11月在土壤剖面的3.28 m深度被发现一次。同期施用的其他农药(异马唑、异甲草胺、草甘膦和氟草磷)未在渗透区检测到。然而,在监测期间没有在现场施用吡虫啉的情况下,在整个vadosezone中都检测到吡虫啉,显示出对降解的显著抵抗。结果显示,在研究结束时,没有任何证据表明在现场钻孔中有任何定期施用农药,这表明它们在到达地下水之前在渗透区内最终降解。
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引用次数: 0
Reproducibility of the wet part of the soil water retention curve: a European interlaboratory comparison 土壤保水曲线湿润部分的再现性:欧洲实验室间比较
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-06-30 DOI: 10.5194/soil-9-365-2023
Benjamin Guillaume, Hanane Aroui Boukbida, Gerben Bakker, Andrzej Bieganowski, Yves Brostaux, Wim Cornelis, Wolfgang Durner, Christian Hartmann, Bo V. Iversen, Mathieu Javaux, Joachim Ingwersen, K. Lamorski, A. Lamparter, A. Makó, Ana María Mingot Soriano, I. Messing, A. Nemes, Alexandre Pomes-Bordedebat, Martine van der Ploeg, Tobias K. D. Weber, L. Weihermüller, J. Wellens, Aurore Degré
Abstract. The soil water retention curve (SWRC) is a key soil property required for predicting basic hydrological processes. The SWRC is often obtained in the laboratory with non-harmonized methods. Moreover, procedures associated with each method are not standardized. This can induce a lack of reproducibility between laboratories using different methods and procedures or using the same methods with different procedures. The goal of this study was to estimate the inter- and intralaboratory variability of the measurement of the wet part (from 10 to 300 hPa) of the SWRC. An interlaboratory comparison was carried out between 14 laboratories, using artificially constructed, porous reference samples that were transferred between laboratories according to a statistical design. The retention measurements were modelled by a series of linear mixed models using a Bayesian approach. This allowed the detection of sample-to-sample variability, interlaboratory variability, intralaboratory variability and the effects of sample changes between measurements. The greatest portion of the differences in the measurement of SWRCs was due to interlaboratory variability. The intralaboratory variability was highly variable depending on the laboratory. Some laboratories successfully reproduced the same SWRC on the same sample, while others did not. The mean intralaboratory variability over all laboratories was smaller than the mean interlaboratory variability. A possible explanation for these results is that all laboratories used slightly different methods and procedures. We believe that this result may be of great importance regarding the quality of SWRC databases built by pooling SWRCs obtained in different laboratories. The quality of pedotransfer functions or maps that might be derived is probably hampered by this inter- and intralaboratory variability. The way forward is that measurement procedures of the SWRC need to be harmonized and standardized.
摘要土壤保水曲线(SWRC)是预测基本水文过程所需的关键土壤性质。SWRC通常是在实验室用非统一的方法获得的。此外,与每种方法相关的程序没有标准化。这可能导致使用不同方法和程序的实验室之间缺乏可重复性,或使用不同程序的相同方法。本研究的目的是估计SWRC湿部分(从10到300 hPa)测量的实验室间和实验室内的变异性。在14个实验室之间进行了实验室间比较,使用人工构建的多孔参考样品,根据统计设计在实验室之间转移。利用贝叶斯方法,用一系列线性混合模型对滞留量测量进行建模。这允许检测样品到样品的可变性,实验室间的可变性,实验室内的可变性和测量之间样品变化的影响。SWRCs测量差异的最大部分是由于实验室间的变异性。实验室内的变异性根据实验室的不同而变化很大。一些实验室成功地在同一样品上复制了相同的SWRC,而另一些则没有。所有实验室的平均实验室内变异性小于平均实验室间变异性。对这些结果的一种可能解释是,所有实验室使用的方法和程序略有不同。我们认为,这一结果可能对通过汇集不同实验室获得的SWRC而建立的SWRC数据库的质量具有重要意义。可能得到的土壤传递函数或地图的质量可能受到这种实验室间和实验室内部变异性的影响。今后的方向是协调和标准化SWRC的测量程序。
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引用次数: 0
Quantification of the effects of long-term straw return on soil organic matter spatiotemporal variation: a case study in a typical black soil region 秸秆长期还田对土壤有机质时空变化影响的量化研究——以典型黑土区为例
4区 农林科学 Q2 Agricultural and Biological Sciences Pub Date : 2023-06-28 DOI: 10.5194/soil-9-351-2023
Yang Yan, W. Ji, Baoguo Li, Gui-Hong Wang, Songchao Chen, Dehai Zhu, Zhong Liu
Abstract. The straw return practice is essential to soil organicmatter (SOM) accumulation in the black soil area with high carbonsequestration potential. However, due to lacking accurate spatialdistribution of straw return, few studies have carried out rigorous researchon the impact of long-term straw return on SOM spatiotemporal variation on aregional scale. This study was carried out across an approximately 3000 km2 area in Lishu County, northeastern China, a typical agriculturalplain. Based on a total of 619 soil samples and 16 environmental covariates,the study mapped the spatial distributions of SOM in 2006 and 2018 by randomforest (RF) and evaluated the effects of the interaction of soil properties,land use, and straw return on SOM spatial–temporal variation. The resultsshow that in the context of long-term straw return, the mean SOM contentincreased from 18.93 to 20.84 g kg−1 during 2006–2018. And74.49 % of the region had a significant increase (maximum of 24.41 g kg−1) of SOM. The severest SOM loss occurred in the northwest due tothe light texture and the transition from paddy fields to dryland.Nevertheless, for areas from paddy fields to dryland, the SOM lossdecreased with the increased cumulative crop residue coverage (CRC). The SOM evenincreased by 1.79 g kg−1 when the cumulative crop residue coveragereached 0.60–1.00. In addition, soil with higher initial SOM and sandcontent had a lower response to straw return. The study revealed that strawreturn is beneficial to carbon sink in farmland and is a better way toprevent a carbon source caused by the conservation of paddy field todryland.
摘要在固碳潜力较大的黑土区,秸秆还田对土壤有机质积累至关重要。然而,由于缺乏准确的秸秆还田空间分布,很少有研究在区域尺度上对长期秸秆还田对土壤有机质时空变化的影响进行严谨的研究。本研究在中国东北地区典型的农业平原——梨树县约3000平方公里的区域内进行。基于619个土壤样本和16个环境协变量,利用随机森林(randomforest, RF)绘制了2006年和2018年土壤有机质的空间分布,并评估了土壤性质、土地利用和秸秆还田相互作用对土壤有机质时空变化的影响。结果表明,在长期秸秆还田的背景下,2006-2018年土壤SOM平均含量从18.93 g kg−1增加到20.84 g kg−1。74.49%的区域SOM显著增加,最大可达24.41 g kg−1。由于质地较轻和水田向旱地的过渡,西北地区土壤有机质损失最为严重。从水田到旱地,土壤有机质损失随累积作物残茬盖度(CRC)的增加而减少。当累积作物残茬覆盖达到0.60 ~ 1.00时,土壤有机质增加1.79 g kg−1。此外,初始土壤有机质和含沙量较高的土壤对秸秆还田的响应较低。研究表明,秸秆还田有利于农田碳汇,是防止水田旱地保护造成的碳源流失的较好途径。
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引用次数: 1
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Soil Science
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