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A weighted soil heath index approach for refined assessment of soil health in cropping systems 一种用于精细评价种植系统土壤健康的加权土壤健康指数方法
Pub Date : 2023-08-11 DOI: 10.3389/fsoil.2023.1118526
Surendra Singh, S. Jagadamma, D. Yoder, X. Yin, F. Walker
Promoting sustainable crop production is enhanced by an effective method to assess soil health. However, soil health assessment is challenging due to multiple interactions among dynamic soil properties (i.e., soil health indicators) across management practices and agroecological regions. We tested several currently popular soil health assessment methods for cropping systems in Tennessee in the southeastern US and found that these methods failed to differentiate Tennessee soil health under long-term conservation and conventional management.This study developed a Tennessee weighted soil health index (WSHI) by: 1) selecting a set of management-sensitive soil health indicators, 2) assigning meaningful weights to indicators, and 3) normalizing the scores based on regionally relevant undisturbed natural reference sites. The tested cropping systems treatments were moldboard plow (MP) in continuous soybean (SS), no tillage (NT) in SS, NT with wheat cover (NTW) in SS, no cover and chisel plow (NCCT) in continuous cotton (CC), no cover and no tillage (NCNT) in CC, and hairy vetch cover and no tillage (VCNT) in CC. In addition, two woodlots and one grassland sites in the vicinity of the cropping systems were selected to represent undisturbed natural systems.Out of 22 indicators that proved to be management-sensitive, six were selected as a minimum dataset (MDS). These were particulate organic matter C (POM-C), soil respiration from 4-day incubation (4d CO2), small macroaggregate (0.250-2mm)-associated C (SMA-C), surface hardness (PR15), microbial biomass N (MBN), and bulk density (BD). Measured values of the MDS indicators were transformed into unitless normalized scores (based on the regional range of the indicator), and finally integrated into WSHI scores using a weighted-addition approach. Additionally, the soil health gap (SHG) between the soil health of the regional reference system and different cropping systems was calculated. Results revealed that WSHI strongly differentiated soil health between long-term conservation and conventional managements practices. The WSHI scores for southeastern cropland soils varied as follows: VCNT = NTW > NT > NCNT ≥ NCCT ≥ MP. The SHGs under MP, NCCT, NCNT, NT, NTW, and VCNT were 85.5, 79.9, 68, 45.1, 25.2, and 24.3, respectively, relative to the average WSHI of three undisturbed systems. Results showed that the WSHI approach is effective in more meaningful regional assessment of soil health and SHG can be a potential metric for comparing soil health across agroecological regions.
通过一种有效的土壤健康评估方法,促进可持续的作物生产。然而,由于管理实践和农业生态区域的动态土壤特性(即土壤健康指标)之间的多重相互作用,土壤健康评估具有挑战性。我们在美国东南部的田纳西州测试了几种目前流行的种植系统土壤健康评估方法,发现这些方法未能区分长期保护和传统管理下的田纳西州土壤健康。本研究开发了田纳西州加权土壤健康指数(WSHI),方法是:1)选择一组管理敏感的土壤健康指标,2)为指标分配有意义的权重,3)基于区域相关的未受干扰自然参考点对得分进行归一化。试验种植系统处理为连续大豆(SS)的犁板犁(MP)、SS的免耕(NT)、SS中的小麦覆盖NT(NTW)、连续棉花(CC)的无覆盖凿犁(NCCT)、CC中的无覆盖免耕(NCNT)和CC中的毛豆覆盖免耕(VCNT),选择了种植系统附近的两个林地和一个草地,以代表未受干扰的自然系统。在被证明对管理敏感的22个指标中,有6个被选为最小数据集(MDS)。这些是颗粒有机物C(POM-C)、4天培养的土壤呼吸(4d CO2)、小团聚体(0.250-2mm)相关的C(SMA-C)、表面硬度(PR15)、微生物生物量N(MBN)和堆积密度(BD)。MDS指标的测量值被转换为无单位归一化分数(基于指标的区域范围),并最终使用加权加法方法整合为WSHI分数。此外,还计算了区域参考系统和不同种植系统的土壤健康之间的土壤健康差距。结果表明,WSHI强烈区分了长期保护和传统管理做法之间的土壤健康。东南农田土壤的WSHI得分变化如下:VCNT=NTW>NT>NCNT≥NCCT≥MP。相对于三个未扰动系统的平均WSHI,MP、NCCT、NCNT、NT、NTW和VCNT下的SHG分别为85.5、79.9、68、45.1、25.2和24.3。结果表明,WSHI方法在更有意义的土壤健康区域评估中是有效的,SHG可以作为比较农业生态区域土壤健康的潜在指标。
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引用次数: 0
Pore scale modeling of the mutual influence of roots and soil aggregation in the rhizosphere 根与根际土壤团聚相互影响的孔隙尺度模拟
Pub Date : 2023-08-01 DOI: 10.3389/fsoil.2023.1155889
Maximilian Rötzer, A. Prechtel, N. Ray
Investigating plant/root-soil interactions at different scales is crucial to advance the understanding of soil structure formation in the rhizosphere. To better comprehend the underlying interwoven processes an explicit, fully dynamic spatial and image-based modeling at the pore scale is a promising tool especially taking into account experimental limitations. We develop a modeling tool to investigate how soil aggregation, root growth and root exudates mutually interact with each other at the micro-scale. This allows the simultaneous simulation of the dynamic rearrangement of soil particles, the input and turnover of particulate organic matter, root growth and decay as well as the deposition, redistribution and decomposition of mucilage in the rhizosphere. The interactions are realized within a cellular automaton framework. The most stable configuration is determined by the amount and attractiveness of surface contacts between the particles, where organo-mineral associations preferably lead to the formation of soil aggregates. Their break-up can be induced by root growth or the degradation of gluing agents previously created after the decomposition of particulate organic matter and mucilage. We illustrate the capability of our model by simulating a full life cycle of a fine root in a two-dimensional, horizontal cross section through the soil. We evaluate various scenarios to identify the role of different drivers such as soil texture and mucilage. We quantify the displacement intensity of individual particles and the variations in local porosity due to the change in available pore space as influenced by the root growth and observe compaction, gap formation and a biopore evolution. The simulation results support that the deposition of mucilage is an important driver for structure formation in the rhizosphere. Although mucilage is degraded within a few days after exudation, it leads to a persistent stabilization of the aggregated structures for both textures in the vicinity of the root within a time frame of 1000 days. Local porosity changes are quantified for exudation periods of 1, 10 and 100 days and are already pronounced for short-term exudation of mucilage. This stabilization is significantly different from the structures encountered when only POM could trigger the evolution of gluing spots, and is still present after complete degradation of the root.
在不同尺度上研究植物/根-土相互作用对于促进对根际土壤结构形成的认识至关重要。为了更好地理解潜在的交织过程,在孔隙尺度上进行明确的、完全动态的空间和基于图像的建模是一种很有前途的工具,特别是考虑到实验的局限性。我们开发了一个模型工具来研究土壤团聚、根系生长和根系分泌物在微观尺度上是如何相互作用的。这样就可以同时模拟土壤颗粒的动态重排、颗粒有机质的输入和周转、根的生长和腐烂以及根际粘液的沉积、再分配和分解。相互作用是在元胞自动机框架内实现的。最稳定的结构是由颗粒之间表面接触的数量和吸引力决定的,其中有机矿物结合最好导致土壤团聚体的形成。它们的破裂可以由根系生长或先前在颗粒有机物和粘液分解后产生的粘接剂的降解引起。我们通过在土壤的二维水平横截面中模拟细根的完整生命周期来说明我们的模型的能力。我们评估了不同的情况,以确定不同的驱动因素,如土壤质地和粘液的作用。我们量化了单个颗粒的位移强度和局部孔隙度的变化,这是由于可用孔隙空间的变化受到根系生长的影响,并观察了压实、空隙形成和生物孔演化。模拟结果支持了黏液沉积是根际结构形成的重要驱动因素。虽然粘液在渗出后几天内就会降解,但在1000天的时间框架内,它会导致根部附近两种纹理的聚集结构持续稳定。局部孔隙度变化在1、10和100天的渗出期被量化,并且在粘液的短期渗出中已经很明显。这种稳定性与仅POM可以引发胶斑演变时所遇到的结构明显不同,并且在根完全降解后仍然存在。
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引用次数: 0
Women representation in soil science: gender indicators in the University Program of Interdisciplinary Soil Studies 妇女在土壤科学中的代表性:跨学科土壤研究大学方案中的性别指标
Pub Date : 2023-07-21 DOI: 10.3389/fsoil.2023.1194828
Jhoana Hernández, Laura Rodríguez-Bustos, Aylin Barreras, Lizeth Caballero, Ilce Lara, M. Guevara, A. Lopera, A. Vázquez‐Lule, Mariano Torres-Gómez, Blanca Prado
In the world, 33% of soils are degraded, and 2.9 million people are affected by land degradation, with problems associated with food security, conflicts over natural resources, and migration with different impacts on men or women. To support sustainable soil management, it is necessary to include women’s contributions to soil Sciences; their achievements and academic performance still need to be represented. Women in Science represent 30% worldwide. In Mexico, only 24% of top academic positions are women. For commitment to soil Sciences for Sustainable Development Goals (SDGs), UNAM created the University Program for Interdisciplinary Soil Studies (PUEIS).This research evaluates women’s representation through gender indicators in the PUEIS and SNI datasets and discusses their implications for the gender gap in the soil Science community from Mexico. The data was collected with an online semi-structured survey and the gender indicators selected were related to participation, gender gap, sexism, equal opportunities, exclusion, and academic performance.The results show that in the PUEIS, 54% of members identify themselves as women and 46% as men. The gender gap shows equality in the total number of members. However, low-rank jobs, such as lecturers and lab technicians are women dominated, and the top-ranked positions as a full professor, associate professor, and research scientist are equal. One result to consider for the PUEIS members is that the younger generation, as is the older generation, is dominated by men. This could indicate a setback in intermediate generations’ progress toward achieving gender equality. In the case of SNI members, there is a gender gap problem; of members with a Ph.D. degree, only 38% are women, and the elite group of scientists with a Ph.D. at the top position is represented only by 24% of females.This work constitutes the first gender exercise for analyzing women’s participation in the soil Sciences in Mexico. From our perspective, it is not about competition in scientific careers between women and men; however, it is essential to recognize that gender inequalities are related to income, professional development, and science funding inequalities, and these disparities impact women more than men.
在世界范围内,33%的土壤退化,290万人受到土地退化的影响,其问题与粮食安全、自然资源冲突和移徙有关,对男女的影响各不相同。为了支持可持续土壤管理,必须包括妇女对土壤科学的贡献;他们的成就和学业成绩仍然需要得到体现。科学界的女性占全球的30%。在墨西哥,只有24%的高级学术职位是女性。为了致力于土壤科学促进可持续发展目标(SDGs),墨西哥国立自治大学创建了跨学科土壤研究大学项目(PUEIS)。本研究通过PUEIS和SNI数据集中的性别指标评估了女性的代表性,并讨论了它们对墨西哥土壤科学界性别差距的影响。数据是通过在线半结构化调查收集的,所选择的性别指标与参与、性别差距、性别歧视、平等机会、排斥和学习成绩有关。结果显示,在PUEIS中,54%的成员认为自己是女性,46%的成员认为自己是男性。性别差距显示了成员总数的平等。但是,讲师、实验室技术人员等低层职位是女性的天下,教授、副教授、研究科学家等高层职位男女平等。PUEIS成员需要考虑的一个结果是,年轻一代和老一代一样,都由男性主导。这可能表明,中间世代在实现性别平等方面的进展遇到了挫折。在SNI成员的情况下,存在性别差距问题;在拥有博士学位的成员中,只有38%是女性,而在拥有博士学位的科学家精英群体中,女性只占24%。这项工作是分析墨西哥妇女参与土壤科学的第一次性别活动。从我们的角度来看,这不是男女在科学事业上的竞争;然而,必须认识到,性别不平等与收入、专业发展和科学资助不平等有关,这些不平等对女性的影响大于男性。
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引用次数: 0
Editorial: Microbiome-based technologies: use of inoculants for improving agricultural productivity and sustainability 社论:基于微生物组的技术:利用接种剂提高农业生产力和可持续性
Pub Date : 2023-07-12 DOI: 10.3389/fsoil.2023.1241590
S. R. Cotta, A. Pereira, J. Verma
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引用次数: 0
Editorial: Greenhouse gas measurements in underrepresented areas of the world 社论:世界上代表性不足地区的温室气体测量
Pub Date : 2023-07-11 DOI: 10.3389/fsoil.2023.1240930
Jorge F. Pérez-Quezada, A. Meijide, S. Leitner
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引用次数: 0
Predicting changes in soil organic carbon after a low dosage and one-time addition of biochar blended with manure and nitrogen fertilizer 预测低剂量和一次性添加生物炭与粪肥和氮肥混合后土壤有机碳的变化
Pub Date : 2023-06-20 DOI: 10.3389/fsoil.2023.1209530
M. Oelbermann, R. Jiang, M. Mechler
Modeling plays an important role in predicting the long-term effects of biochar on soil organic carbon dynamics. The objective of our study was to apply the Century model to assess changes in temporal soil organic carbon in soil amended with manure and nitrogen fertilizer (MN), with manure and biochar (MB) or with manure, nitrogen fertilizer and biochar (MNB). We determined that, after 115 years, soil organic carbon stocks could not reach a steady state (equilibrium) or pre-cultivation levels, regardless of amendment type. Our results showed that a biennial input of manure and nitrogen fertilizer (MN) led to a 84% increase in soil organic carbon compared to a 79% (MNB) and 70% (MB) increase when amendments contained biochar. However, the quantity of organic matter input from crop residues and amendments was sufficient to increase the active fraction, with a turnover time of months to years, by 86%. In fact, carbon associated with the slow fraction, with a turnover time of 20 to 50 years, was the key driver for soil organic carbon accumulation in all amendment types. Although the passive fraction is the most stable form of carbon in the soil, with a turnover time of 400 to 100 years, once manure and biochar were added to the soil, this fraction increased up to 32%. Our results provided further insight into the ability of Century to accurately predict changes in soil organic carbon stocks when a combination of manure, nitrogen fertilizer or biochar were added to soil. Century predicted soil organic carbon stocks within -1% to +9% of measured values. However, further fine-tuning of the model is required since biochar undergoes chemical transformations (e.g., ageing) and changes soil physical parameters (e.g., bulk density) that can not be currently accounted for in the Century model. Addressing these limitations of Century will also help to increase the relationship between measured and predicted values.
建模在预测生物炭对土壤有机碳动态的长期影响方面起着重要作用。本研究旨在应用Century模型评估有机肥+氮肥(MN)、有机肥+生物炭(MB)和有机肥+氮肥+生物炭(MNB)土壤有机碳的时间变化。结果表明,无论何种改良方式,115年后土壤有机碳储量都无法达到稳定状态(平衡)或耕作前水平。结果表明,两年一次施用有机肥和氮肥(MN)导致土壤有机碳增加84%,而添加生物炭的土壤有机碳增加79%和70%。然而,从作物残茬和改良剂中输入的有机质量足以使活性组分增加86%,周转时间为数月至数年。事实上,在所有修正类型中,周转时间为20 ~ 50年的慢组分碳是土壤有机碳积累的关键驱动力。虽然被动组分是土壤中最稳定的碳形式,其周转时间为400至100年,但一旦向土壤中添加粪肥和生物炭,这一组分增加了32%。我们的研究结果为Century准确预测土壤有机碳储量变化的能力提供了进一步的见解,当粪肥、氮肥或生物炭混合添加到土壤中时。世纪预测土壤有机碳储量在测量值的-1%到+9%之间。然而,由于生物炭经历化学转化(例如,老化)并改变土壤物理参数(例如,体积密度),因此需要对模型进行进一步的微调,而这些目前无法在Century模型中得到解释。解决Century的这些局限性也将有助于增加实测值和预测值之间的关系。
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引用次数: 0
Editorial: Digital soil mapping - advancing the knowledge frontiers 社论:数字土壤测绘-推进知识前沿
Pub Date : 2023-06-06 DOI: 10.3389/fsoil.2023.1225672
V. L. Mulder, P. Roudier, D. Arrouays
COPYRIGHT © 2023 Mulder, Roudier and Arrouays. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms. TYPE Editorial PUBLISHED 06 June 2023 DOI 10.3389/fsoil.2023.1225672
版权所有©2023 Mulder, Roudier and Arrouays。这是一篇基于知识共享署名许可(CC BY)的开放获取文章。允许在其他论坛上使用、分发或复制,前提是要注明原作者和版权所有者,并根据公认的学术惯例引用本期刊的原始出版物。不遵守这些条款的使用、分发或复制是不被允许的。类型社论发表于2023年6月6日DOI 10.3389/fsoil.2023.1225672
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引用次数: 0
Pedological characterization and soil fertility assessment of the selected rice irrigation schemes, Tanzania 坦桑尼亚选定水稻灌溉方案的土壤特征和土壤肥力评价
Pub Date : 2023-05-24 DOI: 10.3389/fsoil.2023.1171849
Said H. Marzouk, H. Tindwa, B. Massawe, N. Amuri, J. Semoka
Rice (Oryza sativa L.) is the second cereal food crop grown in Tanzania after maize (Zea mays L.) and covers approximately 18% of the agricultural land. Soil degradation due to intensive cultivation along with low organic matter input and nutrient imbalance has led to a decline in rice crop yields. This study was conducted to characterize, classify, and assess the fertility status of soils in two rice irrigation schemes of Morogoro region in Tanzania. The data obtained through this study will contribute significantly to land use planning and will facilitate the transfer of agro-technology and other development of the regions with similar ecological conditions. The studied pedons were named MKU-P1 and MKD-P1 for Mkula and Mkindo irrigation schemes, respectively. A total of seven composite soil samples (0–20 cm) were collected for soil fertility assessments. Landform, soil morphological features, parent material, natural vegetation, drainage, erosion, and laboratory data were used to classify the soils in their respective order as per the United States Department of Agriculture (USDA) Soil Taxonomy and the World Reference Base (WRB) soil classification systems. Results showed that the pedons were sandy clay loam in the topsoil and sandy clay to clay in the subsoil; soil reaction ranged from medium acid (pH 5.7) to strongly alkaline (pH 8.6). The topsoil and subsoil nutrients of the studied pedons including available K+, total N, soil organic matter, and organic carbon are low. Based on the USDA Soil Taxonomy, MKU-P1 is classified as Inceptisols cumulic humaquepts and MKD-P1 as Vertisols Fluvaquentic endoaquerts corresponding to Subaquatic fluvisols (loamic, oxyaquic) and Irragric vertisols (gleyic) in the WRB, respectively. The pedons were ranked as suitable for rice production. However, the chemical fertility of the soil is ranked as low fertile associated with deficient in total N; available P, K+, and Ca2+ with excessive iron and manganese; and likely to pose toxicity to crops. The application of organic and mineral amendments in recommended rates and timing for N and P is therefore essential to increase the nutrient content of these soils and minimize losses. Salinity in the subsurface pedon MKD-P1 needs to be taken into future consideration.
水稻(Oryza sativa L.)是坦桑尼亚种植的第二大谷类粮食作物,仅次于玉米(Zea mays L.),约占农业用地的18%。精耕细作导致土壤退化,有机质投入不足,养分失衡,导致水稻产量下降。本研究对坦桑尼亚莫罗戈罗地区两种水稻灌溉方案的土壤肥力状况进行了表征、分类和评估。通过这项研究获得的数据将对土地利用规划作出重大贡献,并将促进具有类似生态条件的地区的农业技术转让和其他发展。在Mkula和Mkindo灌溉方案下,所研究的土壤分别命名为MKU-P1和MKD-P1。共收集7个复合土壤样品(0 ~ 20 cm)进行土壤肥力评价。根据美国农业部(USDA)土壤分类系统和世界参考基地(WRB)土壤分类系统,利用地形、土壤形态特征、母质、自然植被、排水、侵蚀和实验室数据对土壤进行了分类。结果表明:土壤表层为砂质粘土壤土,底土为砂质粘土对粘土;土壤反应范围从中酸性(pH 5.7)到强碱性(pH 8.6)。研究区表层土壤和底土养分(速效钾+、全氮、土壤有机质和有机碳)均较低。根据美国农业部土壤分类,MKU-P1被归类为ineptisols cumulic humaquepts, MKD-P1被归类为veridsols fluvaquic,分别对应于WRB中的水下河流(loic, oxyaquic)和非农业河流(gleyic)。结果表明,这些水稻适于种植。然而,土壤的化学肥力被列为低肥力,与全氮缺乏有关;含有过量的铁和锰的磷、钾和钙;并且可能对作物造成毒性。因此,在建议的氮磷施用速率和施用时间内施用有机和矿物改良剂对于增加这些土壤的养分含量和尽量减少损失至关重要。MKD-P1地下地层的盐度需要进一步考虑。
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引用次数: 0
Recycling wastes to mitigate trace elements contamination in plants: a new horizon for urban agriculture in polluted soils 回收废物以减轻植物中的微量元素污染:污染土壤中城市农业的新前景
Pub Date : 2023-05-19 DOI: 10.3389/fsoil.2023.1163356
Anne Barbillon, T. Lerch, J. Araujo, N. Manouchehri, H. Robain, A. Pando-Bahuon, P. Cambier, François Nold, S. Besançon, C. Aubry
Urban agriculture development often faces the problem of soil pollution. Soil engineering consisting in the addition over polluted soils of a top layer made of recycled wastes is a promising solution. This study was co-constructed with urban farmers and aimed at testing in situ the feasibility of growing vegetables safe for consumption in substrates consisting of organic and inorganic waste, directly overlaying soil polluted by trace elements (TE). Two plants were tested: radishes and tomatoes. Three substrates were tested: 1) sheep manure mixed with composted ramial chipped wood (SHW); 2) biowaste compost mixed with mushroom compost and ramial chipped wood (BMW); and 3) deep excavated subsoils mixed with green waste compost (EXC). Only radishes grown in EXC presented levels of TE below the threshold values. For all the other cases, cadmium levels were above the threshold values. This result concerning plant contamination by TE is consistent with a contamination of SHW and BMW substrates by the polluted soil underneath. EXC contained lower TE content, suggesting that mineral materials limited the transfer from the polluted soil towards the substrate overlay. We concluded that adding a combination of mineral and organic waste on top of polluted soils may better mitigate vegetables contamination than adding only organic waste. However, this result was not observed for all tested vegetables. More research is needed to evaluate the best substrate candidate and its adequate thickness, to study its physico-chemical evolution over a longer period of time and to test a larger panel of vegetables.
城市农业发展往往面临土壤污染问题。土壤工程是一种很有前途的解决方案,它包括在被污染的土壤上添加一层由回收废物制成的表层。本研究与城市农民共同构建,旨在实地测试在有机和无机废弃物组成的基质上种植安全食用蔬菜的可行性,直接覆盖受微量元素(TE)污染的土壤。研究人员测试了两种植物:萝卜和西红柿。试验了3种基质:1)羊粪混合堆肥碎木(SHW);2)生物垃圾堆肥与蘑菇堆肥和苎麻碎木(BMW)混合;3)深挖底土混合绿色废弃物堆肥(EXC)。只有在EXC中生长的萝卜的TE水平低于阈值。在所有其他案例中,镉含量都高于阈值。这一关于TE污染植物的结果与下面污染土壤对SHW和BMW基质的污染是一致的。EXC含有较低的TE含量,表明矿物材料限制了污染土壤向基材覆盖层的转移。我们的结论是,在受污染的土壤上混合添加矿物和有机废物比只添加有机废物更能减轻蔬菜污染。然而,这一结果并不适用于所有的蔬菜。需要更多的研究来评估最佳的候选基质及其适当的厚度,研究其在较长时间内的物理化学演变,并测试更大的蔬菜面板。
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引用次数: 0
Revisiting the past to understand the present and future of soil health in Brazil 回顾过去,了解巴西土壤健康的现状和未来
Pub Date : 2023-05-17 DOI: 10.3389/fsoil.2023.1172436
A. M. M. Silva, V. L. V. P. Araujo, E. Cardoso
As Soil Scientists, we are gathering important and valuable knowledge about the chemical, physical and biological processes in soil, and with the increasing effects of climate change, this knowledge may play a pivotal role in the future of our planet. However, we must revisit crucial points in our past to understand how humanity’s evolution has shaped the current state of soil health. Furthermore, we must also consider that we are funded and supported by the society in which we live, and therefore social and political factors will inevitably play a part in the future of soil health. In this review, we address important historical aspects of crop development and soil microbiome combined with the provision of key ecosystem services to ensure soil sustainability. In addition, we provide a brief overview of key concepts related to soil health, including the criteria of the selection of indicators for soil health assessment, whilst focusing on the role of soil biology. Moreover, we provide an overview of research conducted across diverse biomes in Brazil, highlighting approaches to assess soil health in both agroecosystems and natural ecosystems. We also emphasize the significance of harnessing beneficial plant-microorganism interactions as an ecologically sustainable strategy for enhancing soil health. Finally, we conclude the review by discussing potential advancements in soil health assessment in Brazil, and their potential application in broader agricultural and forestry contexts.
作为土壤科学家,我们正在收集有关土壤中化学、物理和生物过程的重要而有价值的知识,随着气候变化的影响越来越大,这些知识可能会在我们星球的未来发挥关键作用。然而,我们必须重新审视我们过去的关键点,以了解人类的进化如何塑造了当前的土壤健康状况。此外,我们还必须考虑到,我们所生活的社会为我们提供了资金和支持,因此,社会和政治因素将不可避免地在土壤健康的未来发挥作用。在这篇综述中,我们讨论了作物发展和土壤微生物组的重要历史方面,并结合提供关键的生态系统服务,以确保土壤的可持续性。此外,我们简要概述了与土壤健康相关的关键概念,包括土壤健康评估指标的选择标准,同时重点介绍了土壤生物学的作用。此外,我们概述了在巴西不同生物群落中进行的研究,强调了评估农业生态系统和自然生态系统土壤健康的方法。我们还强调了利用有益的植物-微生物相互作用作为增强土壤健康的生态可持续战略的重要性。最后,我们通过讨论巴西土壤健康评估的潜在进展及其在更广泛的农业和林业背景下的潜在应用来结束审查。
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引用次数: 0
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Frontiers in soil science
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