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Correction: Soil organic carbon content: decreases partly attributed to dilution by increased depth of cultivation in southern Ontario 更正:土壤有机碳含量:减少的部分原因是安大略省南部种植深度增加造成的稀释
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-10-28 DOI: 10.1139/cjss-2022-0106
C. J. Warren, D. Saurette, A. Gillespie
: Soil organic carbon contents and depths of Ap horizons (i.e
:土壤有机碳含量与Ap层深度(即
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引用次数: 0
Growth and nutrient uptake of haloxylon and atriplex as affected by mycorrhizal symbiosis under combined drought and salinity stresses 干旱和盐胁迫下菌根共生对梭梭和凤梨生长和养分吸收的影响
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-10-27 DOI: 10.1139/cjss-2022-0069
Mohammad Hossein Noshad, E. Chavoshi, M. Mosaddeghi, V. Dorostkar, F. Hosseini
Abstract This study was conducted to determine the effect of arbuscular mycorrhizal fungi (AMF) symbiosis on plant growth and nutrient uptake under combined drought and salinity stresses. A pot experiment was carried out with a factorial arrangement of treatments in a completely randomized design with three replications. Experimental treatments included two plant types (Atriplex canescens and Haloxylon ammodendron) with three levels of inoculation of fungal species (Funneliformis geosporus, Funneliformis mosseae, and control), two levels of soil salinity stress (7 and 14 dS m–1), and two levels of drought stress (50% and 80% of management allowable depletion). Vegetative parameters, as well as root N, P, and K concentrations and uptakes, mycorrhizal growth response, mycorrhizal nitrogen response, mycorrhizal phosphorus response, mycorrhizal potassium response, and root colonization were measured. The results showed that the application of AMF increased the plant growth variables such as stem diameter, root length, shoot dry weights, and shoot to root ratio as well as nitrogen and phosphorus uptakes. The application of both AMF types was effective as compared to the control. However, F. mosseae indicated better performance especially, in terms of the effect on plant growth variables. Also, F. mosseae was more effective to relieve stress (i.e., salinity and drought) than F. geosporus. There was a significant difference between plant types and H. ammodendron had better efficiency than A. canescens under drought and salinity stresses. Based on the results, planting of H. ammodendron inoculated with F. mosseae might be recommended for soil conservation in the arid environments.
摘要本试验旨在研究干旱和盐胁迫下丛枝菌根真菌(AMF)共生对植物生长和养分吸收的影响。盆栽试验采用全随机设计,3个重复。试验处理包括两种植物类型(黑藤和梭梭),接种三种真菌(地孢漏斗形真菌、mosse漏斗形真菌和对照),两种土壤盐胁迫(7和14 dS m-1)和两种干旱胁迫(管理允许耗水量的50%和80%)。测定了营养参数、根系N、P、K浓度和吸收量、菌根生长响应、菌根氮响应、菌根磷响应、菌根钾响应和根定植。结果表明,AMF的施用增加了植株的茎粗、根长、茎干重、茎根比和氮磷吸收量。与控制相比,两种AMF类型的应用都是有效的。但在对植物生长变量的影响方面,苔藻表现出更好的性能。此外,藓苔比地孢更能有效地缓解胁迫(即盐度和干旱)。不同植物类型间存在显著差异,在干旱和盐胁迫下梭梭的效率优于梭梭。基于上述结果,在干旱环境下,推荐种植接种了苔藓镰刀菌的梭梭属土壤保持植物。
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引用次数: 1
Enzyme activity after applying alkaline biosolids to agricultural soil 在农业土壤中施用碱性生物固体后的酶活性
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-10-21 DOI: 10.1139/cjss-2022-0056
B. Sun, C. Kallenbach, M. Boh, O. G. Clark, J. Whalen
Abstract Municipal wastewater biosolids are nutrient-rich residuals with potential as crop fertilizer, if their alkalinity does not adversely affect soil biochemical processes. This study assessed the potential soil enzyme activity after three annual applications of biosolids in a conventionally tilled field under silage corn (Zea mays L.). Biosolids were municipal wastewater sludge treated by mesophilic anaerobic digestion, lime stabilization, or composting, compared with urea fertilizer and an unfertilized control. Generally, the potential soil enzyme activity did not change with biosolids application, but the N-acetylglucosaminidase activity increased in soil amended with lime-stabilized biosolids, which also had higher soil pH and greater soil NH4+ concentration.
摘要城市污水生物固体是营养丰富的残留物,如果其碱度不会对土壤生化过程产生不利影响,则有可能作为作物肥料。本研究评估了在青贮玉米(Zea mays L.)下传统耕作的田地中每年施用三次生物固体后的潜在土壤酶活性。与尿素和未施肥对照相比,生物固体是通过中温厌氧消化、石灰稳定或堆肥处理的城市废水污泥。一般来说,潜在的土壤酶活性不会随着生物固体的施用而改变,但在石灰稳定的生物固体改良的土壤中,N-乙酰氨基葡糖苷酶活性增加,土壤pH值更高,土壤NH4+浓度更高。
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引用次数: 1
Mapping the maximum peat thickness of cultivated organic soils in the southwest plain of Montreal 绘制蒙特利尔西南平原栽培有机土壤的最大泥炭厚度
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-10-14 DOI: 10.1139/cjss-2022-0031
Raphaël Deragon, D. Saurette, Brandon Heung, J. Caron
Abstract Large organic deposits in the southwestern plain of Montreal have been converted to agricultural land for vegetable production. In addition to the variable depth of the organic deposits, these soils commonly have an impermeable coprogenous layer between the peat and the underlying mineral substratum. Estimations of the depth and thickness of these materials are critical for soil management. Therefore, five drained and cultivated peatlands were studied to estimate their maximum peat thickness (MPT)—a potential key soil property that can help identify management zones for their conservation. MPT can be defined as the depth to the mineral layer (DML) minus the coprogenous layer thickness (CLT). The objective of this study was to estimate DML, CLT, and MPT at a regional scale using environmental covariates derived from remote sensing. Three machine-learning models (Cubist, Random Forest, and k-Nearest Neighbor) were compared to produce maps of DML and CLT, which were combined to generate MPT at a spatial resolution of 10 m. The Cubist model performed the best for predicting both features of interest, yielding Lin’s concordance correlation coefficients of 0.43 and 0.07 for DML and CLT, respectively, using a spatial cross-validation procedure. Interpretation of the drivers of CLT was limited by the poor predictive power of the final model. More precise data on MPT are needed to support soil conservation practices, and more CLT field observations are required to obtain a higher prediction accuracy. Nonetheless, digital soil mapping using open-access geospatial data shows promise for understanding and managing cultivated peatlands.
摘要蒙特利尔西南平原的大型有机矿床已被转化为蔬菜生产的农业用地。除了有机沉积物的深度可变外,这些土壤通常在泥炭和下层矿物基质之间有一层不可渗透的共生层。估计这些材料的深度和厚度对于土壤管理至关重要。因此,对五个排水和耕种的泥炭地进行了研究,以估计其最大泥炭厚度(MPT)——这是一种潜在的关键土壤特性,有助于确定保护泥炭地的管理区。MPT可以定义为到矿物层的深度(DML)减去共生层厚度(CLT)。本研究的目的是使用遥感得出的环境协变量在区域尺度上估计DML、CLT和MPT。比较了三个机器学习模型(Cubist、Random Forest和k-Nearest Neighbor),以生成DML和CLT的地图,将其组合以生成10m空间分辨率的MPT。Cubist模型在预测两个感兴趣的特征方面表现最好,DML和CL的Lin一致性相关系数分别为0.43和0.07,使用空间交叉验证程序。CLT驱动因素的解释受到最终模型预测能力差的限制。需要更精确的MPT数据来支持土壤保护实践,需要更多的CLT现场观测来获得更高的预测精度。尽管如此,使用开放获取地理空间数据的数字土壤测绘显示出了解和管理耕种泥炭地的前景。
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引用次数: 5
Gray Luvisols are polygenetic 灰色luvisol是多基因的
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-09-28 DOI: 10.1139/cjss-2022-0035
M. Dyck, P. Sorenson, J. Lejoly, S. Quideau
Abstract With respect to the pedosphere, human activities in the last 100 years have been the major driver of soil change. Despite human activities being one of the main soil forming factors recognized by soil scientists (in addition to climate, organisms, parent material, relief, groundwater, and time), the Canadian System of Soil Classification (CSSC) emphasizes soil as a natural body. We argue human agricultural activities are direct and indirect drivers of significant changes to the carbon balance and cycling in A horizons of Gray Luvisolic soils in western Canada, resulting in changes to A horizon carbon stocks, structure, and micromorphology. Evidence from scientific literature, in-field soil profile observations, and the National Pedon Database are presented in support of our argument. We propose a polygenetic, two-stage model of Gray Luvisol soil formation. The first stage is dominated by the climate forcing of the Holocene, resulting in a relatively stable boreal forest ecosystem including perturbations from natural and human-induced wildfire and other disturbances. The second stage is dominated by direct, human-driven disturbances such as cultivation, release of exotic fauna (earthworms), and indirect human-driven disturbances associated with anthropogenic climate change. Further, we propose modest amendments to the CSSC to reflect a polygenetic model of soil genesis in Gray Luvisolic soils that preserve the balance between observation and interpretation inherent in the system.
就土壤圈而言,人类活动在过去100年中一直是土壤变化的主要驱动力。尽管人类活动是土壤科学家公认的主要土壤形成因素之一(除了气候、生物、母质、地形、地下水和时间),但加拿大土壤分类系统(CSSC)强调土壤是一个自然体。作者认为,人类农业活动是加拿大西部灰色陆域土壤A层碳平衡和循环显著变化的直接和间接驱动因素,导致A层碳储量、结构和微观形态的变化。来自科学文献、实地土壤剖面观测和国家Pedon数据库的证据支持了我们的论点。我们提出了一个多成因的、两阶段的灰色土壤形成模型。第一阶段以全新世气候强迫为主,形成了一个相对稳定的北方森林生态系统,包括自然和人为野火等扰动。第二阶段主要是直接的、人为的干扰,如种植、释放外来动物(蚯蚓),以及与人为气候变化有关的间接人为干扰。此外,我们建议对CSSC进行适度修正,以反映灰色Luvisolic土壤中土壤发生的多遗传模型,以保持系统固有的观测和解释之间的平衡。
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引用次数: 2
Perennial grain Kernza® fields have higher particulate organic carbon at depth than annual grain fields 多年生谷物Kernza®田比一年生谷物田具有更高的深层颗粒有机碳
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-09-23 DOI: 10.1139/cjss-2022-0026
L. K. van der Pol, Brian Nester, B. Schlautman, T. Crews, M. Cotrufo
Abstract Conversion from annual to perennial grains such as intermediate wheatgrass Kernza® could sequester soil organic carbon (SOC). To date, no studies have quantified SOC under Kernza on working farms. We sampled three sites with paired fields under annual grains and converted to Kernza 5–17 years ago to 100 cm and compared their SOC stocks as distributed between mineral-associated organic matter (MAOM) and particulate organic matter (POM). POM-C was higher under Kernza cultivation but total and MAOM-C were similar. Our findings suggest that Kernza increases SOC at depth as POM. Further study is needed to assess whether this will result in long-term SOC sequestration. Résumé Passer des céréales annuelles à des céréales vivaces comme l’agropyre intermédiaire Kernza® permettrait de séquestrer le carbone organique du sol (COS). Jusqu’à présent, aucune étude n’a quantifié le COS dans les exploitations agricoles qui cultivent Kernza. Les auteurs ont prélevé des échantillons jusqu’à une profondeur de 100 cm à trois endroits où des champs servant à la culture de céréales annuelles avaient été convertis à la culture du Kernza 5–17 années plus tôt. Ensuite, ils ont comparé les réserves de COS sous forme de matière organique liée aux minéraux (MOAM) et de particules de matière organique (PMO). La concentration de C-PMO était plus importante dans les parcelles de Kernza, mais la teneur totale et la concentration de C-MOAM étaient similaires. Ces résultats laissent croire que Kernza augmente la quantité de COS en profondeur sous forme de PMO. Des études plus poussées seraient nécessaires pour déterminer s’il y a subséquemment séquestration à long terme du COS. [Traduit par la Rédaction]
从一年生谷物到多年生谷物的转化,如中间小麦草Kernza®,可以固存土壤有机碳(SOC)。到目前为止,还没有研究量化Kernza对工作农场的SOC。我们选取了3个样地,并在5-17年前将其转换为Kernza至100 cm,并比较了它们的有机碳储量在矿物伴生有机质(MAOM)和颗粒有机质(POM)之间的分布。Kernza栽培下POM-C较高,但总POM-C和mam - c相近。我们的研究结果表明,Kernza增加了POM深度的有机碳。需要进一步的研究来评估这是否会导致长期的有机碳封存。(3)通过对csm的分析,确定了csm与csm的关系,并确定了csm与csm的关系。Jusqu ' s ' prassine, auune ' cassine和' quantififii ' s的意思是:' Jusqu ' s ' prassine, ' aucune ' cassine, ' comune ' cassine, ' comune ' cassine。Les auteurs ont prsamevevest des samchantillons jusqu ' comune profondeur de 100 cm trois endroit où des champs servant culture de csamracriales annuelles avaient samtere convertis la culture du Kernza 5-17 annacimes plus tôt。Ensuite, ils - ont compcompore, les rs - acri - sous form de matimatire organic (MOAM)和de particles de matimatire organic (PMO)。La concentration de C-PMO sameta加上重要的dans les parceles de Kernza, mais La teneur totale和La concentration de C-MOAM sameta类似。在此之前,我曾说过:“我的工作是为了提高我的工作质量,而不是为了提高我的工作质量。”Des练习曲+种seraient necessaires倒限定词年代有subsequemment封存terme du COS。[贸易协定]
{"title":"Perennial grain Kernza® fields have higher particulate organic carbon at depth than annual grain fields","authors":"L. K. van der Pol, Brian Nester, B. Schlautman, T. Crews, M. Cotrufo","doi":"10.1139/cjss-2022-0026","DOIUrl":"https://doi.org/10.1139/cjss-2022-0026","url":null,"abstract":"Abstract Conversion from annual to perennial grains such as intermediate wheatgrass Kernza® could sequester soil organic carbon (SOC). To date, no studies have quantified SOC under Kernza on working farms. We sampled three sites with paired fields under annual grains and converted to Kernza 5–17 years ago to 100 cm and compared their SOC stocks as distributed between mineral-associated organic matter (MAOM) and particulate organic matter (POM). POM-C was higher under Kernza cultivation but total and MAOM-C were similar. Our findings suggest that Kernza increases SOC at depth as POM. Further study is needed to assess whether this will result in long-term SOC sequestration. Résumé Passer des céréales annuelles à des céréales vivaces comme l’agropyre intermédiaire Kernza® permettrait de séquestrer le carbone organique du sol (COS). Jusqu’à présent, aucune étude n’a quantifié le COS dans les exploitations agricoles qui cultivent Kernza. Les auteurs ont prélevé des échantillons jusqu’à une profondeur de 100 cm à trois endroits où des champs servant à la culture de céréales annuelles avaient été convertis à la culture du Kernza 5–17 années plus tôt. Ensuite, ils ont comparé les réserves de COS sous forme de matière organique liée aux minéraux (MOAM) et de particules de matière organique (PMO). La concentration de C-PMO était plus importante dans les parcelles de Kernza, mais la teneur totale et la concentration de C-MOAM étaient similaires. Ces résultats laissent croire que Kernza augmente la quantité de COS en profondeur sous forme de PMO. Des études plus poussées seraient nécessaires pour déterminer s’il y a subséquemment séquestration à long terme du COS. [Traduit par la Rédaction]","PeriodicalId":9384,"journal":{"name":"Canadian Journal of Soil Science","volume":"102 1","pages":"1005 - 1009"},"PeriodicalIF":1.7,"publicationDate":"2022-09-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45184069","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: 4
Revised proposed classification for human modified soils in Canada: Anthroposolic order 加拿大人类改良土壤的修订拟议分类:人工土壤目
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-09-15 DOI: 10.1139/cjss-2022-0033
M. Naeth, L. Leskiw, J. A. Brierley, C. J. Warren, Kevin Keys, Konstantin G. Dlusskiy, Ronggui Wu, G. Spiers, J. Laskosky, M. Krzic, G. Patterson, A. Bedard-Haughn
Abstract As the global human population and associated anthropogenic activities rapidly increase, so does the areal extent of disturbed soils. Regulatory frameworks must incorporate reclamation criteria and management options for these disturbed soils, requiring consistent descriptions and interpretations. Many human-altered soils cannot be classified using the current Canadian System of Soil Classification (CSSC), thus an Anthroposolic order is proposed. Anthroposols are soils that are highly modified or constructed by human activity, with one or more natural horizons removed and replaced, added to, or significantly modified. Disturbed horizons are anthropic in origin and contain materials significantly modified physically and/or chemically by human activities. Three great groups are defined by the presence of anthropogenic artefacts and organic carbon content. Eight subgroups are based on the amount of organic material, thickness of horizons, material composition, hydrologic regime, and presence of permafrost. Traditional phases and modifiers are used as in the CSSC. The proposed classification has been revised from the original publication in 2012 after field testing and discussion among soil scientists across Canada. This revised classification is proposed for inclusion in the revised CSSC, to account for the very large and expanding aerial extent of disturbed soils in Canada, and to remain current with other global soil taxonomy systems.
随着全球人口和相关人为活动的迅速增加,受干扰土壤的面积也在增加。管理框架必须纳入这些受干扰土壤的复垦标准和管理方案,需要一致的描述和解释。许多人为改变的土壤不能用现行的加拿大土壤分类系统(CSSC)进行分类,因此提出了一个人类时代的分类顺序。人溶土壤是由人类活动高度改变或构成的土壤,其中一个或多个自然层被移除、替换、添加或显著改变。扰动层是由人类活动引起的,其中含有经人类活动在物理上和/或化学上显著改变的物质。根据人为人工制品的存在和有机碳含量划分了三大类。根据有机物质的数量、地层厚度、物质组成、水文状况和永久冻土层的存在,划分出八个亚组。与CSSC一样,采用了传统的相位和修饰符。在经过加拿大各地土壤科学家的实地测试和讨论后,拟议的分类已经从2012年的原始出版物中进行了修订。这一修订后的分类被提议纳入修订后的CSSC,以说明加拿大非常大的和不断扩大的受干扰土壤的空中范围,并与其他全球土壤分类系统保持同步。
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引用次数: 2
Proposed classification for human modified soils in Canada: Anthroposolic order 加拿大人类改良土壤的拟议分类:人类类人学顺序
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-09-15 DOI: 10.1139/CJSS2011-028
M. Naeth, H. A. Archibald, Candace L. Nemirsky, L. Leskiw, J. A. Brierley, Michael D. Bock, A. VandenBygaart, D. Chanasyk
Naeth, M. A., Archibald, H. A., Nemirsky, C. L., Leskiw, L. A., Brierley, J. A., Bock, M. D., VandenBygaart, A. J. and Chanasyk, D. S. 2012. Proposed classification for human modified soils in Canada: Anthroposolic order. Can. J. Soil Sci. 92: 7-18. With increasing anthropogenic activity, the areal extent of disturbed soils is becoming larger and disturbances more intense. Regulatory frameworks must incorporate reclamation criteria for these disturbed soils, requiring consistent descriptions and interpretations. Many human altered soils cannot be classified using the Canadian System of Soil Classification (CSSC), thus an Anthroposolic Order is proposed. Anthroposols are azonal soils, highly modified or constructed by human activity, with one or more natural horizons removed, removed and replaced, added to, or significantly modified. Defining features are severe disruption of soil forming factors and introduction of potentially new pedogenic trajectories. Disturbed layers are anthropic in origin and contain materials significantly modified physically and/or chemically by human activities. Three great groups are defined by presence of anthropogenic artefacts and organic carbon content. Six subgroups are based on a cover soil layer with higher organic carbon content than the profile below it, on depth of disturbance, on drainage characteristics and water regime at the site. Some new phases and modifiers, in addition to traditional ones used in the CSSC, are based on chemical and physical properties and origins of anthropogenic artefacts. The proposed classification has been successfully applied to reclaimed profiles and is ready for widespread field testing.
Naeth, m.a., Archibald, h.a., Nemirsky, c.l., Leskiw, l.a., Brierley, j.a., Bock, m.d., VandenBygaart, a.j.和Chanasyk, d.s. 2012。加拿大人类改良土壤的拟议分类:人类类人学顺序。可以。土壤学报,32(2):718 - 718。随着人类活动的增加,受干扰土壤的面积越来越大,干扰也越来越强烈。管理框架必须纳入这些受干扰土壤的复垦标准,要求一致的描述和解释。加拿大土壤分类系统(Canadian System of Soil Classification, CSSC)无法对许多人类改变的土壤进行分类,因此提出了一个人类类群目。人壤是由人类活动高度改变或构建的地域性土壤,其中一个或多个自然层被移除、移除和替换、添加或显著改变。定义特征是土壤形成因素的严重破坏和潜在的新成土轨迹的引入。扰动层是由人类活动引起的,其中含有经人类活动在物理和/或化学上显著改变的物质。根据人为人工制品的存在和有机碳含量划分了三大类。六个亚组是基于有机碳含量高于其下方剖面的覆盖土层、扰动深度、排水特征和场地的水状况。除了CSSC中使用的传统相和改性剂外,还有一些新的相和改性剂是基于人为人工制品的化学和物理性质以及来源。提出的分类方法已成功应用于回收剖面,并准备进行广泛的现场测试。
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引用次数: 3
Identifying rotation and tillage practices that maintain or enhance soil carbon and its relation to soil health 确定维持或增加土壤碳的轮作和耕作方法及其与土壤健康的关系
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-09-15 DOI: 10.1139/cjss-2021-0161
Erin Wepruk, A. Diochon, L. V. Van Eerd, E. Gregorich, B. Deen, D. Hooker
Abstract Physical fractions of soil organic matter (SOM) are established indicators of management-induced change and have been used to estimate the soil carbon storage capacity and storage potential. Here, we use SOM physical fractions and soil textures to identify management practices that maintain or enhance soil health and carbon storage in agricultural soils in Ontario. Metadata from the National Soil Database were used to estimate carbon storage potentials and calculate carbon deficits. A map was created showing carbon deficits in Ontario's agricultural soils and indicates that these soils have the potential to store an additional 0 to 2kgm−2 in the top 20cm of the soil. Tillage system generally had no effect on the size of the carbon deficit at four long-term agricultural experiments (Delhi, Elora, Ottawa, and Ridgetown). There was only a significant tillage effect at Ridgetown and only in the maize–soybean crop rotation, where the carbon deficit was 2.95gCkgsoil−1 under conventional tillage compared to 8.97gCkgsoil−1 with no tillage. A statistically significant effect of crop rotation was detected in Elora and Ridgetown. In Elora, continuous alfalfa had the smallest carbon deficit (7.25gCkgsoil−1) and maize–soybean rotation had the largest deficit (12.07gCkgsoil−1). In Ridgetown, the maize–soybean rotation had the smallest carbon deficit (2.95gCkgsoil−1). Regression analysis showed a weak negative relationship (R2=0.11; P<0.001) between carbon storage deficits and soil health scores. This suggests that increasing SOM levels alone may not improve soil health.
土壤有机质物理组分(SOM)是公认的管理变化指标,可用于评价土壤碳储量和储存潜力。在这里,我们使用SOM物理组分和土壤质地来确定维持或增强安大略省农业土壤土壤健康和碳储存的管理实践。利用国家土壤数据库的元数据估算碳储存潜力并计算碳亏缺。绘制的地图显示了安大略省农业土壤的碳赤字,并表明这些土壤有可能在土壤的顶部20厘米处储存额外的0至2kgm - 2。在四个长期农业试验(德里、埃罗拉、渥太华和里奇敦)中,耕作制度一般对碳赤字的大小没有影响。仅在Ridgetown和玉米-大豆轮作中存在显著的耕作效应,常规耕作的碳亏缺为2.95gCkgsoil - 1,而不耕作的碳亏缺为8.97gCkgsoil - 1。在Elora和Ridgetown发现了统计上显著的作物轮作效果。在Elora地区,连续苜蓿的碳亏缺最小(7.25gCkgsoil - 1),玉米-大豆轮作的碳亏缺最大(12.07gCkgsoil - 1)。在Ridgetown,玉米-大豆轮作的碳亏缺最小(2.95gCkgsoil−1)。回归分析显示两者呈弱负相关(R2=0.11;P<0.001)。这表明仅增加SOM水平可能不会改善土壤健康。
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引用次数: 0
Spatial dependency and independency of nitrogen in lowbush blueberry commercial fields 低灌丛蓝莓商品田氮素的空间依赖性和独立性
IF 1.7 4区 农林科学 Q4 SOIL SCIENCE Pub Date : 2022-09-15 DOI: 10.1139/cjss-2022-0063
Anthony J. Pelletier, J. Lafond, M. Paré
Abstract Rhizomes of wild lowbush blueberry (Vaccinium angustifolium Aiton) extend horizontally, creating spatial dependency when fertilization trials are performed. Knowing this spatial dependency would help researchers to better design field studies. Here, we used labelled nitrogen (N) fertilizer (15N-(NH4)2SO4) to measure N translocation among blueberry stems for one old (56year) and one younger (15year) commercial field. Leaf 15N concentrations at the tip-dieback stage were used to monitor N acquisition. No difference between sites suggests no field age effect on N translocation. Spatial dependency and independency were reached for distances of ≤0.75 and ≥1.75m from the fertilizer application point, respectively.
摘要野生低灌木蓝莓(越橘)的根状茎水平延伸,在进行施肥试验时产生空间依赖性。了解这种空间依赖性将有助于研究人员更好地设计实地研究。在这里,我们使用标记的氮(N)肥料(15N-(NH4)2SO4)来测量一个老的(56岁)和一个年轻的(15岁)商业田地的蓝莓茎之间的N迁移。利用顶端枯死期的叶片15N浓度来监测氮的获取。位点之间没有差异表明田间年龄对N易位没有影响。距施肥点≤0.75和≥1.75m的距离分别达到空间依赖性和独立性。
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引用次数: 0
期刊
Canadian Journal of Soil Science
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