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Soil quality index under different land-use types: the case of Choke Mountain agroecosystems, upper Blue Nile Basin, Ethiopia 不同土地利用类型下的土壤质量指数——以埃塞俄比亚青尼罗上游呛山农业生态系统为例
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2023-01-09 DOI: 10.1139/cjss-2022-0053
D. Mesfin, E. Assefa, B. Simane
Abstract In an agroecosystem (AES), land-use types affect soil quality. As a result, determining soil quality in various land uses is critical. This study was carried out to evaluate the soil quality index (SQI) of the different land-use types in AESs of the Choke Mountain watershed, upper Blue Nile Basin. Forty-seven soil samples were taken from cultivated land (CL), grazing land (GL), plantation forest land (PFL), and natural forest land (NFL) of the five AESs. The minimum data set (MDS) was chosen using principal component analysis. To calculate SQI, five soil quality indicators were selected as an MDS: silt, pH, cation exchange capacity, exchangeable potassium, and soil organic matter. SQIs for the overall land uses were ordered as GL > NFL > PFL > CL. Compared with NFL, the SQIs of PFL and CL were reduced by 10% and 19.7%, respectively, whereas the SQI of GL was increased by 1.8%. Among AESs of Choke, SQI of GL was higher in the midland plain, dominated by Vertisol (AES 2), followed by the midland plain with Nitosols (AES 3). SQI of CL was intermediate, and SQIs of GL, NFL, and PFL were good. AES 2 of the watershed recorded the highest total SQI value, whereas hilly and mountainous highlands (AES 5) recorded the lowest SQIs compared to other AESs. Thus, site-specific land use and management practices across the various AESs should be recommended to policymakers and farmers for a sustainable ecosystem and environment.
在农业生态系统(AES)中,土地利用类型影响土壤质量。因此,确定不同土地用途的土壤质量至关重要。以青尼罗上游呛山流域AESs不同土地利用类型的土壤质量指数(SQI)为研究对象。从5个农业生态系统的耕地(CL)、放牧地(GL)、人工林(PFL)和天然林(NFL)采集土壤样品47份。采用主成分分析法选取最小数据集。为了计算SQI,选取淤泥、pH、阳离子交换容量、交换性钾和土壤有机质5个土壤质量指标作为MDS。整体土地用途的sqi排序为GL > NFL > PFL > CL。与NFL相比,PFL和CL的SQI分别降低了10%和19.7%,而GL的SQI增加了1.8%。在窒息的AESs中,中部平原地区GL的SQI较高,以Vertisol (AES 2)为主,其次是中部平原地区的Nitosols (AES 3)。CL的SQI为中等,GL、NFL和PFL的SQIs较好。流域的空气质量指数(AES 2)最高,而丘陵和山地高原(AES 5)的空气质量指数最低。因此,应向决策者和农民推荐不同农业生态系统的具体土地利用和管理实践,以实现可持续的生态系统和环境。
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引用次数: 1
Biochar applications to boreal podzol improve soil hydraulic properties and control nitrogen dynamics 生物炭在北方恶唑中的应用改善了土壤水力特性并控制了氮动力学
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-12-22 DOI: 10.1139/cjss-2022-0086
R. Saha, RaymondH. Thomas, K. Hawboldt, M. Nadeem, M. Cheema, L. Galagedara
Abstract The study aimed to investigate the effects of biochar (BC) application on hydraulic properties and nitrogen (N) transport in a podzolic soil profile. Soil samples were collected from an agricultural research field in Pasadena, Newfoundland, Canada. The following three types of leaching columns were prepared: (i) topsoil, (ii) top and E-horizon soil, and (iii) mixed soil (2:1 ratio of topsoil and E-horizon soil). Granular biochar (GBC) and powder biochar (PBC) were mixed with soils at the rate of 0%, 1% and 2% (w/w). BC’s morphological structure and pore size distribution were examined using a scanning electron microscope, and the specific surface area was assessed by the Brunauer−Emmett−Teller method. Soil physical and hydraulic properties (bulk density, porosity, field capacity (FC), permanent wilting point, plant available water (PAW)), leaching concentration of nitrate (NO3−) and ammonium (NH4+), and volume of leachate were measured through a total of 378 experiments under laboratory conditions. GBC and PBC showed hydrophobic and hydrophilic characteristics, respectively. With the 2% PBC amendment, porosity increased by 3%, FC by 10%, and PAW by 13% in the mixed soil and reduced NO3− leaching by 36% in top and E-horizon soil and NH4+ leaching by 72% in mixed soil. On the other hand, NO3− and NH4+ leaching was reduced by 26% and 33% in mixed soil when treated with 2% GBC. A 2% application rate for both BC (GBC and PBC) showed the best performance to enhance soil hydraulic properties and retain significant amounts of NO3− and NH4+ in the boreal podzol.
摘要本研究旨在探讨生物炭(BC)施用对灰化土水力学特性和氮(N)运移的影响。土壤样本采集自加拿大纽芬兰帕萨迪纳的一个农业研究领域。制备了三种类型的淋滤柱:(i)表层土,(ii)表层土和e层土,(iii)混合土(表层土和e层土的比例为2:1)。颗粒型生物炭(GBC)和粉状生物炭(PBC)分别以0%、1%和2% (w/w)的比例与土壤混合。采用扫描电镜观察BC的形态结构和孔径分布,采用Brunauer - Emmett - Teller法测定比表面积。在实验室条件下,通过378次试验,测量了土壤的物理和水力特性(容重、孔隙度、田间容量(FC)、永久萎蔫点(permanent蔫点)、植物有效水分(PAW))、硝态氮(NO3−)和铵态氮(NH4+)的浸出浓度和渗滤液体积。GBC和PBC分别表现为疏水性和亲水性。添加2% PBC后,混合土孔隙度增加3%,FC增加10%,PAW增加13%,表层和e层土壤NO3−淋溶减少36%,NH4+淋溶减少72%。另一方面,2% GBC处理的混合土壤NO3−和NH4+淋失分别减少26%和33%。施用2%的BC (GBC和PBC)对改善土壤水力特性和保留大量NO3−和NH4+的效果最好。
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引用次数: 0
Rationalizing mottling and gleying in the characterization and classification of Canadian soils 加拿大土壤表征和分类中斑点和潜育的合理化
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-12-15 DOI: 10.1139/cjss-2022-0036
R. Heck, D. Saurette, C. J. Warren
Abstract Mottling and gleying remain important characteristics for the classification of soils in Canada. The development of criteria for the morphological description of these redoximorphic soil features, for soil horizon nomenclature, for the taxonomy of gleysolic and gleyed soils, as well as for soil drainage classification, began in the mid-1940s and continued for the next four decades. Despite advancements elsewhere, notably with Soil Taxonomy and the World Reference Base, there have been minimal refinements made in Canada, during the past quarter century. Various issues are identified, including the need for more succinct and clearer definitions, a revision of standards for the field characterization of redoximorphic features, as well as more consistency in the application of concepts across existing taxa and systems. A taxonomic framework to more effectively reflect redoximorphic features, such as a new “Redoximorphic Phase” is also discussed. Ultimately, it is recommended that a special committee to be established to conduct a thorough study and present recommendations.
斑点和潜育仍然是加拿大土壤分类的重要特征。从20世纪40年代中期开始,制定了对这些重样土壤特征的形态描述、土壤层命名、潜育土和潜育土的分类以及土壤排水分类的标准,并持续了40年。尽管在其他地方取得了进步,特别是在土壤分类学和世界参考基地方面,但在过去的四分之一个世纪里,加拿大的改进程度很低。确定了各种问题,包括需要更简洁、更清晰的定义,修订重做形态特征的现场表征标准,以及在现有分类群和系统中应用概念的一致性。还讨论了一个更有效地反映再氧化态特征的分类框架,如一个新的“再氧化态阶段”。最后,建议成立一个特别委员会,进行彻底研究并提出建议。
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引用次数: 1
Ratio of non-growing season to growing season N2O emissions in Canadian croplands: an update to national inventory methodology 加拿大农田非生长季节与生长季节N2O排放量的比率:国家清单方法的更新
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-12-08 DOI: 10.1139/cjss-2022-0101
D. Pelster, A. Thiagarajan, C. Liang, M. Chantigny, C. Wagner-Riddle, K. Congreves, R. Lemke, A. Glenn, M. Tenuta, G. Hernandez‐Ramirez, S. Bittman, D. Hunt, J. Owens, D. MacDonald
Abstract National inventory reporting of agricultural nitrous oxide (N2O) emissions in Canada is based primarily on measurements obtained using static chambers. In regions with cold winters and an accumulated snowpack (including Canada), these measurements tend to focus on the growing season (typically May–October). However, research has shown that emissions continue throughout the non-growing season (NGS) and that these account for a significant proportion of annual emissions. In the Canadian National Inventory NGS emissions currently are assumed to be adequately captured in western Canada, while they are accounted for in eastern Canada by multiplying the growing season emissions by a correction factor of 1.4, a value that was derived based on a limited number of measurements. Here we use recent Canadian studies to validate this correction factor. We collected data from available Canadian studies that measured soil N2O emissions from agricultural systems for the entire year and determined the proportion of these emissions that occurred during the NGS. The proportion of annual N2O emissions that occurred during the NGS varied widely, ranging from −4% to 119% with a mean of 35.5%, compared to the previous estimate of 30%. Due to high variability, few differences were observed between means associated with climatic, soil, and management variables. To correct for NGS N2O emissions from Canadian agricultural soils, we suggest that the current correction factor for converting growing season to total annual emissions be changed from 1.4 to 1.55 and that this be used for all agricultural soils in Canada rather than just eastern Canada.
摘要加拿大农业一氧化二氮(N2O)排放的国家清单报告主要基于使用静态室获得的测量结果。在冬季寒冷、积雪堆积的地区(包括加拿大),这些测量往往集中在生长季节(通常为5月至10月)。然而,研究表明,在整个非生长季节(NGS),排放量仍在继续,这些排放量在年排放量中占很大比例。在加拿大国家清单中,目前假设加拿大西部充分捕获了NGS排放量,而加拿大东部则通过将生长季节的排放量乘以1.4的修正系数来计算,该修正系数是基于有限数量的测量得出的。在这里,我们使用加拿大最近的研究来验证这个校正因子。我们从加拿大现有的研究中收集了数据,这些研究测量了农业系统全年的土壤N2O排放量,并确定了NGS期间这些排放量的比例。NGS期间发生的年N2O排放比例变化很大,从−4%到119%不等,平均为35.5%,而之前的估计为30%。由于高度可变性,在与气候、土壤和管理变量相关的平均值之间几乎没有观察到差异。为了校正加拿大农业土壤的NGS N2O排放量,我们建议将当前将生长季节转换为年总排放量的校正系数从1.4改为1.55,并将其用于加拿大的所有农业土壤,而不仅仅是加拿大东部。
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引用次数: 2
Earthworm distribution around tile drainage in agricultural fields of southwest Quebec, Canada 加拿大魁北克西南部农田瓷砖排水沟周围的蚯蚓分布
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-11-25 DOI: 10.1139/cjss-2022-0059
H. Diop, Leanne Ejack, A. Elmi, J. Whalen
Abstract Tile drainage is installed in agricultural fields to remove excess soil moisture to allow earlier planting of spring crops. Water moving from soil into tile drainage lines will potentially create a moist environment for earthworms. This study investigated how earthworms were distributed around tile lines, and how their abundance was affected by moisture in field crops on sandy and clayey soils. Earthworm abundance and soil moisture were similar above and between tile lines. Earthworm biomass was low in dry soils, peaked at 41 g moisture 100 g−1, and declined in wetter soils, which affects the earthworm activity in agricultural fields.
在农田中安装瓦片排水系统是为了去除多余的土壤水分,以便提前种植春季作物。水从土壤流入瓷砖排水管道,可能会为蚯蚓创造一个潮湿的环境。本研究考察了蚯蚓是如何分布在瓦线周围的,以及它们的丰度如何受到沙质和粘性土壤上大田作物水分的影响。蚯蚓数量和土壤湿度在瓦线以上和瓦线之间相似。蚯蚓生物量在干燥土壤中较低,在水分100 g−1时达到最大值41 g,在湿润土壤中下降,这影响了农田蚯蚓的活动。
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引用次数: 0
Establishment and experiment of a pressure-bearing subsidence model of layered soil in forest region 林区层状土承压沉降模型的建立与试验
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-11-25 DOI: 10.1139/cjss-2022-0067
Yuan Zhou, Shufa Sun, Jingkai Wang, Miao Yu, Haoyu Yin, Fei Yang, Hao Luo
Abstract Forest vehicle operation causes different degrees of compaction damage to the soil, which is related to the pressure-bearing characteristics of the soil. However, scholars have not profoundly investigated the pressure-bearing factors of forest soil. In this paper, disturbed brown coniferous forest soil was collected layer by layer, dried, screened, and tested with indoor pressing-plate tests with different pressing-plate shapes and diameters (side lengths). A kind of pressure–subsidence (P–Z) curve of hard soil, which is different from those of farmland soil and homogeneous remolded soil, was obtained and drawn as the P–Z curve. The results show that in the process of pressure subsidence, the forest soil gradually changed from loose to compact. Furthermore, the change of pressure-bearing subsidence of layered soil from this forest region was characterized first by the rapid increase of soil subsidence with the increase of pressure. Then, the subsidence speed became slower with the increase of pressure; finally, subsidence speed was much less affected by the increase in pressure. According to the pressure-bearing subsidence curve of forest soil, a new subsidence model is put forward in this paper. The new model has a good prediction effect on the subsidence curve of forest soil. This paper aims to provide a theoretical basis for studying soil pressure-bearing characteristics and the development of vehicles in high-passing forest areas.
摘要森林车辆作业对土壤造成不同程度的压实破坏,这与土壤的承压特性有关。然而,学者们对森林土壤承压因素的研究还不够深入。本文逐层采集受扰动的棕针叶林土壤,进行干燥、筛选,并采用不同压板形状和直径(边长)的室内压板试验。得到了一种不同于农田土和均质重塑土的硬土压力沉降(P-Z)曲线,并将其绘制为P-Z曲线。结果表明:在压力沉降过程中,森林土壤逐渐由疏松向密实转变;此外,该林区层状土的承压沉降变化首先表现为随压力的增加而迅速增加。随着压力的增大,沉降速度逐渐变缓;最后,沉降速度受压力增加的影响较小。根据森林土壤的承压沉降曲线,提出了一种新的沉降模型。该模型对森林土壤沉降曲线具有较好的预测效果。本文旨在为公路林区土壤承压特性研究和车辆发展提供理论依据。
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引用次数: 0
Do cover crops on the Canadian prairies affect soil nitrogen cycling? 加拿大大草原上的覆盖作物会影响土壤氮循环吗?
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-11-25 DOI: 10.1139/cjss-2022-0079
O. Otchere, Y. Lawley, K. Congreves
Abstract For one of Canada’s most important regions of crop production—the prairies—it’s uncertain if cover crops can be successfully integrated into rotations; if so, will soil nitrogen (N) cycling be influenced to benefit main crops? To address these gaps, we compared a crop rotation with cover crops (CC) vs. without cover crops (LR) from 2018 to 2021 in Saskatoon, SK. The main crops were grown in sequence of wheat–canola–potato–pea; the cover crops included red clover, berseem clover/oat mix, fall rye, and a brassica cover. Yield and aboveground biomass were collected each year and analyzed to determine crop yield and N use efficiency (NUE). Soil N availability was monitored in various ways, that is, by assessing pre-plant soil nitrate, soil inorganic N (SIN) supply rate, and potentially mineralizable N (PMN). We found that the influence on soil N dynamics was restricted to the non-growing season where cover crops reduced SIN supply rate and nitrate content compared to the conventional practice without cover crops. Yet, rotations with vs. without cover crop did not differ in crop NUEs, yields, or in-season N dynamics. We found some evidence that diversifying rotations with cover crops may help the system to function more like perennial systems in terms of regulating N in the long run; but had limited impact during the three years studied. To ensure that cover crops are effective and functional on the prairies, innovative design approaches are needed to adapt cover crops to reach soil health goals under prairie conditions.
摘要对于加拿大最重要的作物生产地区之一——大草原来说,覆盖作物能否成功融入轮作还不确定;如果是这样,土壤氮循环是否会受到影响,使主要作物受益?为了解决这些差距,我们比较了2018年至2021年SK萨斯卡通有覆盖作物(CC)和无覆盖作物(LR)的轮作情况。主要作物按小麦-油菜-土豆-豌豆的顺序种植;覆盖作物包括红三叶草、三叶草/燕麦混合物、秋黑麦和芸苔。每年收集产量和地上生物量并进行分析,以确定作物产量和氮利用效率(NUE)。通过评估植物前期土壤硝酸盐、土壤无机氮(SIN)供应速率和潜在矿化氮(PMN),以多种方式监测土壤氮的有效性。我们发现,与没有覆盖作物的传统做法相比,覆盖作物降低了SIN供应率和硝酸盐含量,对土壤氮动态的影响仅限于非生长季节。然而,有覆盖作物与无覆盖作物的轮作在作物NUE、产量或季节氮动态方面没有差异。我们发现一些证据表明,从长远来看,覆盖作物的多样化轮作可能有助于该系统在调节氮方面更像多年生系统;但在研究的三年中影响有限。为了确保覆盖作物在草原上的有效性和功能性,需要创新的设计方法来调整覆盖作物,以实现草原条件下的土壤健康目标。
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引用次数: 1
Crop rotational diversity alters the composition of stabilized soil organic matter compounds in soil physical fractions 轮作多样性改变了土壤物理组分中稳定土壤有机质化合物的组成
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-11-23 DOI: 10.1139/cjss-2022-0058
Huan Tong, Meiling Man, C. Wagner-Riddle, K. Dunfield, B. Deen, M. Simpson
Abstract Crop rotational diversity is an important part of sustainable agricultural and soil management to improve crop yield and soil fertility including enhancing soil organic matter (SOM) stabilization. Because of the physical protection via interactions with soil minerals, SOM in mineral-associated fractions is believed to be longer-lived and more stable relative to SOM in particulate (light) fractions. However, it is still unclear how crop rotational diversity alters soil carbon distribution, composition and stabilization in soil physical fractions. To address this, we studied a 37 years’ agricultural site with different crop rotational diversity (from continuous corn or alfalfa up to four species (corn, soybean, winter wheat, and red clover)). Soil carbon analysis, targeted compound analysis and nuclear magnetic resonance spectroscopy methods were used to obtain the distribution and degradation of SOM components in light and mineral-associated (F53–2000 µm, F2–53 µm, and F<2 µm) fractions. Higher soil organic carbon (SOC) concentrations were observed in F<2 µm with relatively high diversified crop rotations (three and four types of crops) compared to monoculture or two crops in the rotations, which suggests that carbon storage is enhanced in mineral-stabilized pools. Higher concentrations of long-chain aliphatic compounds as well as increased accumulation and preservation of lignin-derived compounds in fine aggregates (<53 µm) were also observed with relatively high diversified crop rotations. Overall, the increased concentration and preservation of specific SOM compounds as well as increased SOC in finer mineral-associated fractions (<53 µm) suggests that crop rotational diversity may enhance the long-term stability of SOM in agroecosystems.
摘要作物轮作多样性是可持续农业和土壤管理的重要组成部分,旨在提高作物产量和土壤肥力,包括提高土壤有机质(SOM)的稳定性。由于与土壤矿物相互作用的物理保护作用,与颗粒(轻)组分中的SOM相比,矿物相关组分中SOM的寿命更长、更稳定。然而,目前尚不清楚作物轮作多样性如何改变土壤碳分布、组成和土壤物理组分的稳定性。为了解决这一问题,我们研究了一个37年的农业场地,该场地具有不同的作物轮作多样性(从连续的玉米或苜蓿到四个物种(玉米、大豆、冬小麦和红三叶草))。土壤碳分析、靶向化合物分析和核磁共振波谱方法用于获得SOM组分在光和矿物相关(F53–2000µm、F2–53µm和F<2µm)组分中的分布和降解。在F<2µm的土壤有机碳(SOC)浓度较高,与轮作中的单一种植或两种作物相比,多样化作物轮作(三种和四种作物)相对较高,这表明矿物稳定库中的碳储存增强。在相对较高的多样化作物轮作中,还观察到长链脂族化合物浓度较高,木质素衍生化合物在细聚集体(<53µm)中的积累和保存增加。总体而言,特定SOM化合物的浓度和保存增加,以及较细矿物相关组分(<53µm)的SOC增加,表明作物轮作多样性可能增强农业生态系统中SOM的长期稳定性。
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引用次数: 1
Predictive mapping of wetland soil types in the Canadian Prairie Pothole Region using high-resolution digital elevation model terrain derivatives 利用高分辨率数字高程模型地形衍生物预测加拿大草原坑区湿地土壤类型
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-11-23 DOI: 10.1139/cjss-2022-0034
J. Kiss, A. Bedard-Haughn, P. Sorenson
Abstract Wetland soil types, which can be distinguished based on calcium carbonate content, vary in their effect on ecosystem functions like phosphorus retention, salinity contributions, and greenhouse gas forcing. These soil types may be predictively mapped with machine learning models that use terrain derivatives calculated from high-resolution digital elevation models. Soil profiles from three Saskatchewan study sites were classified into three functional categories—upland, calcareous wetland, or noncalcareous wetland—and used to train random forest models for predictive soil mapping. Multiple terrain derivatives were included as predictor variables to capture local- and landscape-scale morphometry and hydrology influences, including five derivatives developed for this study. Models were developed at three spatial resolutions: 2, 5, and 10 m, and tested via internal cross-validation and independent validation with datasets from previous studies. Predictive accuracies were highest when mapping at 2 m resolution (independent validation accuracy range = 64%–100%) but also successful when mapping at 5 and 10 m resolutions (independent validation accuracy range = 63%–100%); however, visual inspection determined that the maps generated at 10 m resolution were less detailed and occasionally featured questionable discontinuous soil distributions. Three of the five terrain derivatives developed for this study were among the most important predictor variables (first, second, and 10th most important). Models trained using only data from a specific site had slightly better performance than models trained using data from all sites, except in regions where training data were lacking.
湿地土壤类型对磷保持、盐度贡献和温室气体强迫等生态系统功能的影响各不相同,可根据碳酸钙含量进行区分。这些土壤类型可以通过机器学习模型进行预测映射,该模型使用高分辨率数字高程模型计算的地形导数。萨斯喀彻温省三个研究地点的土壤剖面被划分为三个功能类别——高地、钙质湿地和非钙质湿地,并用于训练用于预测土壤制图的随机森林模型。多种地形衍生物被纳入预测变量,以捕获局部和景观尺度的形态计量学和水文影响,其中包括为本研究开发的五个衍生物。在3种空间分辨率下开发模型:2、5和10 m,并通过内部交叉验证和与先前研究数据集的独立验证进行测试。预测精度在2米分辨率下最高(独立验证精度范围= 64%-100%),但在5米和10米分辨率下也成功(独立验证精度范围= 63%-100%);然而,目视检查确定,以10米分辨率生成的地图不太详细,偶尔也有可疑的不连续土壤分布。为本研究开发的五个地形导数中有三个是最重要的预测变量(第一、第二和第十重要)。除了缺乏训练数据的地区外,仅使用来自特定地点的数据训练的模型比使用来自所有地点的数据训练的模型性能稍好。
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引用次数: 1
Biochar application stabilized the heavy metals in coal mined soil 生物炭的应用稳定了煤矿土壤中的重金属
IF 1.7 4区 农林科学 Q3 Agricultural and Biological Sciences Pub Date : 2022-11-03 DOI: 10.1139/cjss-2022-0073
Myra Nazeer, M. J. Khan, D. Muhammad, Ahmad Masood Khan
Abstract The waste of coal mining activities causes accumulation of hazardous elements in soil for plants. Biochar is considered an important soil remediation strategy to stabilize the heavy metals. The aim of this study was to quantify the effect of biochar sources and rate on the heavy metal stabilization in coal-contaminated soil. Biochars of three feedstocks (maize straw (MBC), rice straw (RBC), and sugarcane bagasse (SBC)) with four levels (0%, 0.5%, 1%, and 2%, i.e., 0, 10, 20, and 40 ton ha−1) were applied to two types of soils (naturally contaminated soil (NCS) versus artificially contaminated soil (ACS) spiked with Cd, Cu, Cr, and Pb). Plastic pots were incubated at 30% field capacity for 90 days at 25 °C, and soil pH, electrical conductivity (EC), and heavy metals concentration were measured after 1, 4, 8, and 12 weeks. Among the biochars, RBC showed maximum immobilization of Cd, Pb, Cu, and Cr as compared with MBC and SBC. Similarly, biochar application increased heavy immobilization, being maximum at 2% (40 ton ha−1) rate compared with control. The pH of both soils with biochar addition increased as compared with control. The remediation effect of biochar on heavy metal stabilization was positive over time. The higher rate (40 ton ha−1) of RBC for ACS and MBC for NCS could be used effectively for heavy metal stabilization.
摘要:煤矿开采废弃物对植物有害元素在土壤中积累。生物炭被认为是稳定重金属的重要土壤修复策略。本研究的目的是量化生物炭来源和速率对煤污染土壤重金属稳定化的影响。将玉米秸秆(MBC)、水稻秸秆(RBC)和甘蔗渣(SBC)三种原料(0%、0.5%、1%和2%,即0、10、20和40 ton ha - 1)的生物炭分别施用于两种土壤(自然污染土壤(NCS)和添加Cd、Cu、Cr和Pb的人工污染土壤(ACS))。在25℃条件下,以30%田间容量培养90 d,分别于1、4、8、12周后测定土壤pH、电导率(EC)和重金属浓度。在生物炭中,与MBC和SBC相比,RBC对Cd、Pb、Cu和Cr的固定化效果最好。同样,施用生物炭增加了重度固定化,与对照相比,最大固定化率为2%(40吨公顷- 1)。与对照相比,添加生物炭的土壤pH值均有所增加。随着时间的推移,生物炭对重金属稳定的修复效果是积极的。较高的速率(40吨ha - 1) RBC用于ACS和MBC用于NCS可以有效地用于重金属稳定。
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引用次数: 1
期刊
Canadian Journal of Soil Science
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