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  • 1
    Online Resource
    Online Resource
    Frontiers Media SA ; 2022
    In:  Spanish Journal of Soil Science Vol. 12 ( 2022-7-19)
    In: Spanish Journal of Soil Science, Frontiers Media SA, Vol. 12 ( 2022-7-19)
    Abstract: Soils have many ecological functions and provide various ecosystem services including support for global food and fuel production. However, FAO reports indicate that approximately one-third of the planet’s arable lands show levels of degradation from processes including soil erosion, low levels of nutrients, acidification, salinization, compaction, sealing, and contamination. These conditions are also found in Brazil where soil degradation is largely caused by inadequate land management. Worldwide, strategic policies have been presented to mitigate this problem, with emphasis on sustainable agriculture. Among them, agroforestry has been identified as a viable system for mitigating and recovering degraded areas. Agroforestry techniques have been developed and tested but are still not understood by farmers, due to their complexity. This study aimed to analyze experiences and studies with agroforestry reported from Australia, some countries in Africa, and Brazil to search for similarities in these complex systems and identify possible correlations to support the hypothesis that land recovery can be enhanced through soil management using agroforestry. A Sankey diagram was developed to illustrate relationships among problems, the adoption of agroforestry and improvements, and the most important contributions. Data analysis shows that the main problems related to soil degradation are soil erosion and decreased soil fertility, while the adoption of agroforestry systems proved to improve different aspects of soil quality and to be a safe path to sustainable agricultural production. To obtain more information on the adoption of these systems in different locations, soils, and climates, it is important to implement policies for reducing land degradation. Furthermore, the assessment of the economic, environmental and social benefits of improving soil fertility and decreasing erosion in agroforestry systems is necessary to validate the use of agroforestry as a sustainable agricultural practice.
    Type of Medium: Online Resource
    ISSN: 2253-6574
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2022
    detail.hit.zdb_id: 2700695-5
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  • 2
    In: Spanish Journal of Soil Science, Frontiers Media SA, Vol. 6 ( 2016-03-09)
    Abstract: There is a critical need to incorporate concerns on soil and water use and protection into land use planning policies and practices, not exclusively in protected areas, especially taking into account the widespread power transfer to local authorities regarding land-use decision making. Accordingly, it is extremely useful what Decision Support Systems (DSS) do on land use. AndaLAND is a prototype DSS which has been developed as a web-based application. It helps to define the vulnerability and the efficiency of the use and protection of soils in the selected target region: Andalusia (Southern Spain). AndaLAND integrates a complete catalogue of information on climate, soil and soil management, to make land vulnerability evaluation. By using Web Map Services (WMS), AndaLAND is fed with available databases from public mapping services (the Geographic Information System for the Common Agricultural Policy-SIGPAC) and other external sources (Microcomputed-based Land Evaluation Information System, MicroLEIS). Climate change scenarios are considered jointly with other relevant global change elements, such as land use change. Soil evaluation is based on decision rules that follow a decision tree. This method was established from Drools (a powerful hybrid reasoning system), using agrological rules for determining soil capacity in plots. The tool is capable of evaluating individually more than 6 million plots currently existing in the Andalusian region. AndaLAND’s final output is a report on the particular vulnerability of a user-specified plot. The report includes information on the plot’s geographical location, its environmental status regarding to (current and potential) impacts, degradation and/or pollution in the water-soil-crop system and eventual affections due to climate change-induced events. The report also provides practical recommendations for sustainable use and management of plots (in particular, for irrigated crops, these recommendations are linked to available irrigation technologies and water consumption).
    Type of Medium: Online Resource
    ISSN: 2253-6574
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2016
    detail.hit.zdb_id: 2700695-5
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  • 3
    Online Resource
    Online Resource
    Frontiers Media SA ; 2014
    In:  Spanish Journal of Soil Science Vol. 2 ( 2014-9-05)
    In: Spanish Journal of Soil Science, Frontiers Media SA, Vol. 2 ( 2014-9-05)
    Abstract: Estimating the spatial variability of soil properties is significant for evaluating environmental impacts. For example, many soil properties are directly used in the modelling of environmental processes such as global climate change. These aspects have not previously been studied at this level in La Rioja (a region of Spain with a humid Mediterranean environment). The intention of this study was to provide quantitative information on soil assessment and mapping methods for natural soils in a humid Mediterranean environment. The properties considered included: pH and organic matter, calcium carbonate and clay contents. For testing, samples were selected from several different soil types which, in theory, were only affected by pedogenetic processes and had developed on different parent materials. More than half of the samples did not contain any CaCO 〈 sub 〉 3 〈 /sub 〉 , while the rest of the samples presented a variety of CaCO 〈 sub 〉 3 〈 /sub 〉 , forms, with high percentages being present in certain cases (up to 65% on the surface). It was possible to establish two different areas: one predominantly acidic and the other principally basic. The predominately basic samples were due to the high percentage of carbonate in the parent materials. The clay content on the surface was similar to that in the subsurface layers. Finally, the organic matter contents in the uppermost layers presented average values of 3.9%,with a range of from 0.3 to 17.5%. The major variations in soils were determined by soil type (therefore by soil forming processes), parent material composition, and vegetation type. This study reveals that these methods are useful to determine the spatial distribution of some soil properties in undisturbed soils. The contour maps of soil property variability could be used to improve future sampling designs and management decisions.
    Type of Medium: Online Resource
    ISSN: 2253-6574
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2014
    detail.hit.zdb_id: 2700695-5
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  • 4
    In: Spanish Journal of Soil Science, Frontiers Media SA, Vol. 2 ( 2014-9-05)
    Abstract: Estimating the spatial variability of soil properties is significant for evaluating environmental impacts. For example, many soil properties are directly used in the modelling of environmental processes such as global climate change. These aspects have not previously been studied at this level in La Rioja (a region of Spain with a humid Mediterranean environment). The intention of this study was to provide quantitative information on soil assessment and mapping methods for natural soils in a humid Mediterranean environment. The properties considered included: pH and organic matter, calcium carbonate and clay contents. For testing, samples were selected from several different soil types which, in theory, were only affected by pedogenetic processes and had developed on different parent materials. More than half of the samples did not contain any CaCO 〈 sub 〉 3 〈 /sub 〉 , while the rest of the samples presented a variety of CaCO 〈 sub 〉 3 〈 /sub 〉 , forms, with high percentages being present in certain cases (up to 65% on the surface). It was possible to establish two different areas: one predominantly acidic and the other principally basic. The predominately basic samples were due to the high percentage of carbonate in the parent materials. The clay content on the surface was similar to that in the subsurface layers. Finally, the organic matter contents in the uppermost layers presented average values of 3.9%,with a range of from 0.3 to 17.5%. The major variations in soils were determined by soil type (therefore by soil forming processes), parent material composition, and vegetation type. This study reveals that these methods are useful to determine the spatial distribution of some soil properties in undisturbed soils. The contour maps of soil property variability could be used to improve future sampling designs and management decisions.
    Type of Medium: Online Resource
    ISSN: 2253-6574
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2014
    detail.hit.zdb_id: 2700695-5
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  • 5
    Online Resource
    Online Resource
    Frontiers Media SA ; 2014
    In:  Spanish Journal of Soil Science Vol. 4 ( 2014-12-3)
    In: Spanish Journal of Soil Science, Frontiers Media SA, Vol. 4 ( 2014-12-3)
    Abstract: Increased human influences on soils frequently result in widespread land and soil degradation. The processes of soil and water degradation are closely linked, as unfavourable changes in the hydrological processes affect soil water regimes. In the last 15-20 years there has been increased interest in human-induced climate change, associated with increased atmospheric concentrations of greenhouse gases. Most of the present and future problems of land and soil degradation, water supply and natural disasters are mainly attributed to these climate changes. At the same time, and probably related to it, there has been a change in the focus of research on soil and water conservation. From the late 1960s there was an increasing interest in stimulating studies related to soil and water conservation. This was a great change from the previous emphasis on more static studies of the characteristics of the soil resource, mainly for soil classification and mapping, and for land evaluation related to agricultural and other uses. This situation was due to the increasing evidence of the global problems of land, soil and water degradation, and their effects on food production and the environment. Particular attention was paid to the processes of soil and water degradation in relation to their use and management for agricultural purposes. These efforts led to the development of models and evaluation systems mainly using empirical approaches. Later studies demonstrated the limitations of the generalized universal use of these empirical approaches. Concurrently there was an increase in related organizations, conventions, congresses and conferences associated with the renewed interest on soil and water conservation. A global assessment of human-induced soil degradation (GLASOD) demonstrated the paucity, difficult accessibility and poor quality of basic information. This information, however, is essential for adequate planning and effective application of practices to prevent soil and water degradation. The most recent conventions and programs at international and regional levels are generally based on re-interpretations, and a different processing method or representation of old information using “new” terminology. In other cases, new information has been mostly generated through indirect or remote sensing deductions, usually without adequate ground-truthing. The decreasing public or private support for more integrated interdisciplinary studies and the compulsion to quickly publish papers has resulted in a very specialized and isolated consideration of different aspects related to the degradation of soil functions. This frequently results in over-simplifications, failures and even contradictions in the proposed strategies to control soil degradation. Currently we have reached quasi-stagnation in soil conservation research and a new series of soil conservation terms (soil quality, desertification, tillage erosion) and clichés (“C sequestration”, “no-tillage”) have been introduced. These are derived from different interests, but generally they are very empirical approaches without a strong scientific basis. However, they attract increased attention from organizations setting policies and providing funds for research in soil and water conservation, and as a consequence many research activities in the last 20 years have been concentrated in such topics. Regretfully, these approaches have very limited accuracy and are insufficient for developing adequate policies for land use and management. Climate, soil and socio-economic conditions differ greatly from one location to another and are changing continuously. There cannot therefore be simple universal prescriptions regarding practices of sustainable soil management for crop production and environmental protection or for mitigation of the greenhouse effect by “C sequestration” in soils. The adequate selection of those sustainable practices must be based on research with a broader vision of soil conservation, where all the system components and their interactions are considered and understood with a far-sighted approach, to ensure that short term gains in one aspect or location do not induce long-term losses in other aspects or elsewhere. Research needs to be directed to better the understanding of the processes and reactions in soils related to chemical recycling and water balance over a range of spatial and temporal scales, with the common objective of improving crop production and environmental protection. Lasting solutions will only be found if adequately trained researchers in soil science and hydrology, who recognize the complexity of the problems, develop appropriate strategies.
    Type of Medium: Online Resource
    ISSN: 2253-6574
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2014
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  • 6
    In: Spanish Journal of Soil Science, Frontiers Media SA, Vol. 10 ( 2020-07-02)
    Abstract: Since soil CO 〈 sub 〉 2 〈 /sub 〉 flux is a key component of ecosystem carbon balance, quantifying its contribution to the ecosystem carbon flux and understanding the factors that underlie its temporal variation is crucial for a better comprehension of ecosystem carbon dynamics under climate change and for optimal ecosystem use and management. Our objectives were to quantify the contributions of total soil CO 〈 sub 〉 2 〈 /sub 〉 efflux ( 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 ) to ecosystem respiration ( 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 ) and heterotrophic soil CO 〈 sub 〉 2 〈 /sub 〉 efflux ( 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 ) to 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 in two 〈 em 〉 chinampa 〈 /em 〉 ecosystems with different natural grass covers. We also aimed to identify the main environmental drivers of seasonal variability of these contributions. The CO 〈 sub 〉 2 〈 /sub 〉 fluxes were measured on each site about every 14 days from September 2008 to August 2009 in the Xochimilco Ecological Park in Mexico City using dark chamber techniques. For two studied sites, 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 , 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 and 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 were estimated on average as 94.1 ± 8.5, 34.7 ± 3.5 and 16.5 ± 1.7 (± S.E.) mg C-CO 〈 sub 〉 2 〈 /sub 〉 m 〈 sup 〉 -2 〈 /sup 〉 h 〈 sup 〉 -1 〈 /sup 〉 , respectively. & nbsp;On average over the study period and sites, the annual cumulative 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 , 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 and 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 fluxes were 824 ± 74, 304 ± 31 and 145 ± 15 g C m 〈 sup 〉 -2 〈 /sup 〉 year, respectively. The 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 , 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 and 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 varied between the winter and summer seasons; this variation was explained mostly by seasonal variations of soil temperature, soil water content and shoot plant biomass. Temperature sensitivity of CO 〈 sub 〉 2 〈 /sub 〉 fluxes depended on vegetation type and plant growth differences among the sites and decreased in the following order: 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 & gt; 〈 em 〉 R 〈 /em 〉 〈 sub 〉 s 〈 /sub 〉 & gt; 〈 em 〉 R 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 . The contribution of 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 to 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 and 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 to 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 for the two studied sites and period averaged about 38% and 50%, respectively regardless of the site vegetation type, but the degree of 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 / 〈 em 〉 R 〈 /em 〉 〈 sub 〉 E 〈 /sub 〉 and 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 / 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 variability depended on the differences in seasonal dynamics of plant cover. The contribution of 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 to 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 varied from 37% in summer to 73% in winter at the site without a seasonal shift in dominant plant species, but 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 / 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 was close to constant during the year at the site with a seasonal change in dominant plant species. During the cold period, the contribution of 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 to 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 increased following plant growth decrease. The linear regression analysis showed that plant biomass was the dominant factor controlling the seasonal variation of 〈 em 〉 F 〈 /em 〉 〈 sub 〉 H 〈 /sub 〉 / 〈 em 〉 F 〈 /em 〉 〈 sub 〉 S 〈 /sub 〉 ratios, whereas the plant biomass dynamic followed the dynamics of soil water content, water table depth, and soil temperature. Our results suggest that seasonal variation of soil contribution to total fluxes from the 〈 em 〉 chinampa 〈 /em 〉 ecosystem is locally differentiated. These differences were related to differences in seasonal dynamics of cover productivity which has been associated with localization of soil water content. This finding has important implications for assessing the contribution of the chinampa ecosystem to the global carbon budget.
    Type of Medium: Online Resource
    ISSN: 2253-6574
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2020
    detail.hit.zdb_id: 2700695-5
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