Articles | Volume 8, issue 4
https://doi.org/10.5194/se-8-737-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-8-737-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
04 Jul 2017
Research article |
| 04 Jul 2017
Land use change affects biogenic silica pool distribution in a subtropical soil toposequence
Dácil Unzué-Belmonte
CORRESPONDING AUTHOR
EcosystemManagement Research Group, Department of Biology, University
of Antwerp, Universiteitsplein 1C, 2610 Wilrijk, Belgium
Invited contribution by Dácil Unzué-Belmonte, recipient of the EGU Soil System Sciences Outstanding Student Poster Award 2014.
Yolanda Ameijeiras-Mariño
Earth and Life Institute, Environmental Sciences, Université
catholique de Louvain, Croix du Sud 2 bte L7.05.10, 1348 Louvain-la-Neuve,
Belgium
Sophie Opfergelt
Earth and Life Institute, Environmental Sciences, Université
catholique de Louvain, Croix du Sud 2 bte L7.05.10, 1348 Louvain-la-Neuve,
Belgium
Jean-Thomas Cornelis
Department Biosystem Engineering (BIOSE), Gembloux Agro-Bio Tech
(GxABT), University of Liège (ULg), Avenue Maréchal Juin, 27, 5030
Gembloux, Belgium
Lúcia Barão
ICAAM, Instituto de Ciências Agrárias e Ambientais
Mediterrânicas, University of Évora, Apartado 94, 7002-554
Évora, Portugal
Jean Minella
Universidade Federal de Santa Maria (UFSM), Department of Soil
Science, 1000 Avenue Roraima, Camobi, CEP 97105-900 Santa Maria, RS, Brazil
Patrick Meire
EcosystemManagement Research Group, Department of Biology, University
of Antwerp, Universiteitsplein 1C, 2610 Wilrijk, Belgium
Eric Struyf
EcosystemManagement Research Group, Department of Biology, University
of Antwerp, Universiteitsplein 1C, 2610 Wilrijk, Belgium
Related authors
No articles found.
Bennet Juhls, Anne Morgenstern, Jens Hölemann, Antje Eulenburg, Birgit Heim, Frederieke Miesner, Hendrik Grotheer, Gesine Mollenhauer, Hanno Meyer, Ephraim Erkens, Felica Yara Gehde, Sofia Antonova, Sergey Chalov, Maria Tereshina, Oxana Erina, Evgeniya Fingert, Ekaterina Abramova, Tina Sanders, Liudmila Lebedeva, Nikolai Torgovkin, Georgii Maksimov, Vasily Povazhnyi, Rafael Gonçalves-Araujo, Urban Wünsch, Antonina Chetverova, Sophie Opfergelt, and Pier Paul Overduin
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-290, https://doi.org/10.5194/essd-2024-290, 2024
Revised manuscript accepted for ESSD
Short summary
Short summary
The Siberian Arctic is warming fast: permafrost is thawing, river chemistry is changing, and coastal ecosystems are affected. We want to understand changes to the Lena River, a major Arctic river flowing to the Arctic Ocean, by collecting 4.5 years of detailed water data, including temperature and carbon and nutrient contents. This dataset records current conditions and helps us to detect future changes. Explore it at https://doi.org/10.1594/PANGAEA.913197 and https://lena-monitoring.awi.de/.
Elisabeth Mauclet, Maëlle Villani, Arthur Monhonval, Catherine Hirst, Edward A. G. Schuur, and Sophie Opfergelt
Earth Syst. Sci. Data, 15, 3891–3904, https://doi.org/10.5194/essd-15-3891-2023, https://doi.org/10.5194/essd-15-3891-2023, 2023
Short summary
Short summary
Permafrost ecosystems are limited in nutrients for vegetation development and constrain the biological activity to the active layer. Upon Arctic warming, permafrost degradation exposes organic and mineral soil material that may directly influence the capacity of the soil to retain key nutrients for vegetation growth and development. Here, we demonstrate that the average total exchangeable nutrient density (Ca, K, Mg, and Na) is more than 2 times higher in the permafrost than in the active layer.
Elisabeth Mauclet, Yannick Agnan, Catherine Hirst, Arthur Monhonval, Benoît Pereira, Aubry Vandeuren, Maëlle Villani, Justin Ledman, Meghan Taylor, Briana L. Jasinski, Edward A. G. Schuur, and Sophie Opfergelt
Biogeosciences, 19, 2333–2351, https://doi.org/10.5194/bg-19-2333-2022, https://doi.org/10.5194/bg-19-2333-2022, 2022
Short summary
Short summary
Arctic warming and permafrost degradation largely affect tundra vegetation. Wetter lowlands show an increase in sedges, whereas drier uplands favor shrub expansion. Here, we demonstrate that the difference in the foliar elemental composition of typical tundra vegetation species controls the change in local foliar elemental stock and potential mineral element cycling through litter production upon a shift in tundra vegetation.
Petra Zahajská, Carolina Olid, Johanna Stadmark, Sherilyn C. Fritz, Sophie Opfergelt, and Daniel J. Conley
Biogeosciences, 18, 2325–2345, https://doi.org/10.5194/bg-18-2325-2021, https://doi.org/10.5194/bg-18-2325-2021, 2021
Short summary
Short summary
The drivers of high accumulation of single-cell siliceous algae (diatoms) in a high-latitude lake have not been fully characterized before. We studied silicon cycling of the lake through water, radon, silicon, and stable silicon isotope balances. Results showed that groundwater brings 3 times more water and dissolved silica than the stream inlet. We demonstrate that groundwater discharge and low sediment deposition have driven the high diatom accumulation in the studied lake in the past century.
Dante M. L. Horemans, Yoeri M. Dijkstra, Michèle Tackx, Patrick Meire, and Tom J. S. Cox
Biogeosciences Discuss., https://doi.org/10.5194/bg-2021-59, https://doi.org/10.5194/bg-2021-59, 2021
Manuscript not accepted for further review
Short summary
Short summary
We study the appearance in 2008–2014 and disappearance after 2015 of a phytoplankton spring-bloom in the brackish region in the Scheldt estuary. To this end, we analyze long-term in situ observations covering the full estuary and apply a model approach to determine which of the changed conditions may explain the observed change in phytoplankton. Our results suggest that insight into the zooplankton dynamics is essential to understand the phytoplankton dynamics in the Scheldt estuary.
Arthur Monhonval, Sophie Opfergelt, Elisabeth Mauclet, Benoît Pereira, Aubry Vandeuren, Guido Grosse, Lutz Schirrmeister, Matthias Fuchs, Peter Kuhry, and Jens Strauss
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2020-359, https://doi.org/10.5194/essd-2020-359, 2020
Preprint withdrawn
Short summary
Short summary
With global warming, ice-rich permafrost soils expose organic carbon to microbial degradation and unlock mineral elements as well. Interactions between mineral elements and organic carbon may enhance or mitigate microbial degradation. Here, we provide a large scale ice-rich permafrost mineral concentrations assessment and estimates of mineral element stocks in those deposits. Si is the most abundant mineral element and Fe and Al are present in the same order of magnitude as organic carbon.
Thorben Amann, Jens Hartmann, Eric Struyf, Wagner de Oliveira Garcia, Elke K. Fischer, Ivan Janssens, Patrick Meire, and Jonas Schoelynck
Biogeosciences, 17, 103–119, https://doi.org/10.5194/bg-17-103-2020, https://doi.org/10.5194/bg-17-103-2020, 2020
Short summary
Short summary
Weathering is a major control on atmospheric CO2 at geologic timescales. Enhancement of this process can be used to actively remove CO2 from the atmosphere. Field results are still scarce and with this experiment we try to add some near-natural insights into dissolution processes. Results show CO2 sequestration potentials but also highlight the strong variability of outcomes that can be expected in natural environments. Such experiments are of the utmost importance to identify key processes.
S. Smolders, Y. Plancke, S. Ides, P. Meire, and S. Temmerman
Nat. Hazards Earth Syst. Sci., 15, 1659–1675, https://doi.org/10.5194/nhess-15-1659-2015, https://doi.org/10.5194/nhess-15-1659-2015, 2015
Short summary
Short summary
Within a confined estuary, a large wetland can play an important role in storm surge mitigation. By use of a numerical model the effects of different wetland sizes, wetland elevations and wetland locations along the estuary on storm surge attenuation along the estuary were investigated. With this paper we aim to contribute towards a better understanding and wider implementation of ecosystem-based adaptation to increasing estuarine flood risks associated with storms.
W. Clymans, L. Barão, N. Van der Putten, S. Wastegård, G. Gísladóttir, S. Björck, B. Moine, E. Struyf, and D. J. Conley
Biogeosciences, 12, 3789–3804, https://doi.org/10.5194/bg-12-3789-2015, https://doi.org/10.5194/bg-12-3789-2015, 2015
Short summary
Short summary
Biogenic silica (BSi) is used as a proxy by soil scientists to identify biological effects on the Si cycle and by palaeoecologists to study environmental changes. We show the presence of tephra constituents can make measurements erroneous at low BSi concentrations, with repercussions for soil and palaeoecological studies. However, we also show that glass shards do not produce an identical dissolution signal to that of BSi, meaning they can be distinguished with appropriate experimental setups.
S. Doetterl, J.-T. Cornelis, J. Six, S. Bodé, S. Opfergelt, P. Boeckx, and K. Van Oost
Biogeosciences, 12, 1357–1371, https://doi.org/10.5194/bg-12-1357-2015, https://doi.org/10.5194/bg-12-1357-2015, 2015
Short summary
Short summary
We link the mineralogy of soils affected by erosion and deposition to the distribution of soil carbon fractions, their turnover and microbial activity. We show that the weathering status of soils and their history are controlling the stabilization of carbon with minerals. After burial, aggregated C is preserved more efficiently while non-aggregated C can be released and younger C re-sequestered more easily. Weathering changes the effectiveness of stabilization mechanism limiting this C sink.
Related subject area
Soil science
Soil erodibility and its influencing factors on the Loess Plateau of China: a case study in the Ansai watershed
Stability of soil organic matter in Cryosols of the maritime Antarctic: insights from 13C NMR and electron spin resonance spectroscopy
Influence of slope aspect on the microbial properties of rhizospheric and non-rhizospheric soils on the Loess Plateau, China
Assessment of soil erosion vulnerability in the heavily populated and ecologically fragile communities in Motozintla de Mendoza, Chiapas, Mexico
Simulating carbon sequestration using cellular automata and land use assessment for Karaj, Iran
Polycyclic aromatic hydrocarbon in urban soils of an Eastern European megalopolis: distribution, source identification and cancer risk evaluation
On soil textural classifications and soil-texture-based estimations
Assessment and monitoring of land degradation using geospatial technology in Bathinda district, Punjab, India
The hidden ecological resource of andic soils in mountain ecosystems: evidence from Italy
Revegetation in abandoned quarries with landfill stabilized waste and gravels: water dynamics and plant growth – a case study
Land-use changes influence soil bacterial communities in a meadow grassland in Northeast China
Physical soil quality indicators for monitoring British soils
Mineral-leaching chemical transport with runoff and sediment from severely eroded rare-earth tailings in southern China
Development of a composite soil degradation assessment index for cocoa agroecosystems in southwestern Nigeria
Soil erosion evolution and spatial correlation analysis in a typical karst geomorphology using RUSLE with GIS
Assessing and analysing the impact of land take pressures on arable land
Evaluating of the spatial heterogeneity of soil loss tolerance and its effects on erosion risk in the carbonate areas of southern China
Identification of regional soil quality factors and indicators: a case study on an alluvial plain (central Turkey)
Micromorphological characteristics of sandy forest soils recently impacted by wildfires in Russia
Application of a new model using productivity coupled with hydrothermal factors (PCH) for evaluating net primary productivity of grassland in southern China
Soil Atterberg limits of different weathering profiles of the collapsing gullies in the hilly granitic region of southern China
The response of Opalinus Clay when exposed to cyclic relative humidity variations
Effects of wheat stubble on runoff, infiltration, and erosion of farmland on the Loess Plateau, China, subjected to simulated rainfall
Reversing land degradation through grasses: a systematic meta-analysis in the Indian tropics
Cooperative effects of field traffic and organic matter treatments on some compaction-related soil properties
Determination of critical pH and Al concentration of acidic Ultisols for wheat and canola crops
Community-weighted mean traits but not functional diversity determine the changes in soil properties during wetland drying on the Tibetan Plateau
Leguminous species sequester more carbon than gramineous species in cultivated grasslands of a semi-arid area
Estimating soil erosion risk and evaluating erosion control measures for soil conservation planning at Koga watershed in the highlands of Ethiopia
Factors of soil diversity in the Batumi delta (Georgia)
Application of a modified distributed-dynamic erosion and sediment yield model in a typical watershed of a hilly and gully region, Chinese Loess Plateau
Nitrogen addition alters elemental stoichiometry within soil aggregates in a temperate steppe
Effects of topsoil treatments on afforestation in a dry Mediterranean climate (southern Spain)
Geochemical mass-balance, weathering and evolution of soils formed on a Quaternaryage basaltic toposequences
Soil wind erosion in ecological olive trees in the Tabernas desert (southeastern Spain): a wind tunnel experiment
Wenwu Zhao, Hui Wei, Lizhi Jia, Stefani Daryanto, Xiao Zhang, and Yanxu Liu
Solid Earth, 9, 1507–1516, https://doi.org/10.5194/se-9-1507-2018, https://doi.org/10.5194/se-9-1507-2018, 2018
Short summary
Short summary
Soil erodibility (K) is one of the key factors of soil erosion. Selecting the optimal estimation method of soil erodibility is critical to estimate the amount of soil erosion, and provide the base for sustainable land management. This research took the Loess Plateau of China as a case study, estimated soil erodibility factor with different methods, selected the best texture-based method to estimate K, and aimed to understand the indirect environmental factors of soil erodibility.
Evgeny Abakumov and Ivan Alekseev
Solid Earth, 9, 1329–1339, https://doi.org/10.5194/se-9-1329-2018, https://doi.org/10.5194/se-9-1329-2018, 2018
Ze Min Ai, Jiao Yang Zhang, Hong Fei Liu, Sha Xue, and Guo Bin Liu
Solid Earth, 9, 1157–1168, https://doi.org/10.5194/se-9-1157-2018, https://doi.org/10.5194/se-9-1157-2018, 2018
Short summary
Short summary
Slope aspect significantly but differently affected the soil microbial biomass carbon and phospholipid fatty acid contents.
Soil carbon and nitrogen have the largest effect on the soil microbial properties.
The rhizospheric effect caused significant difference between rhizospheric and non-rhizospheric soil microbial properties.
Slope aspect affected the mechanisms driving the structure of microbial communities in a micro-ecosystem environment.
Selene B. González-Morales, Alex Mayer, and Neptalí Ramírez-Marcial
Solid Earth, 9, 745–757, https://doi.org/10.5194/se-9-745-2018, https://doi.org/10.5194/se-9-745-2018, 2018
Short summary
Short summary
Physical aspects and knowledge of soil erosion in six rural communities in Chiapas, Mexico, were assessed. Average erosion rates estimated using the RUSLE model ranged from 200 to 1200 ha−1 yr−1. Most erosion rates were relatively high due to steep slopes, sandy soils, and bare land cover. The results of a knowledge, attitudes, and practices (KAP) survey showed that some communities with high erosion rates also had less knowledge of and more negative attitudes towards soil erosion management.
Ali Khatibi, Sharareh Pourebrahim, and Mazlin Bin Mokhtar
Solid Earth, 9, 735–744, https://doi.org/10.5194/se-9-735-2018, https://doi.org/10.5194/se-9-735-2018, 2018
Short summary
Short summary
The speed of land use changes is much higher than in the past, which led to many changes in the environment and ecological processes. These changes cause some changes in the climate, the amount of pollution and biodiversity. Monitoring and modeling historical situation of the region can be used to anticipate the negative effects of these changes in order to protect resources. Agriculture class will be faced with a huge reduction of carbon sequestration because of expansion of residential areas.
George Shamilishvily, Evgeny Abakumov, and Dmitriy Gabov
Solid Earth, 9, 669–682, https://doi.org/10.5194/se-9-669-2018, https://doi.org/10.5194/se-9-669-2018, 2018
Miguel Ángel Martín, Yakov A. Pachepsky, Carlos García-Gutiérrez, and Miguel Reyes
Solid Earth, 9, 159–165, https://doi.org/10.5194/se-9-159-2018, https://doi.org/10.5194/se-9-159-2018, 2018
Short summary
Short summary
The soil texture representation with the standard textural fraction triplet sand–silt–clay is commonly used to estimate soil properties. The objective of this work was to test the hypothesis that other fraction sizes in the triplets may provide a better representation of soil texture for the reconstruction of the particle size distribution and for estimating some soil properties with soil texture as a predictor. The results supported the hypothesis.
Naseer Ahmad and Puneeta Pandey
Solid Earth, 9, 75–90, https://doi.org/10.5194/se-9-75-2018, https://doi.org/10.5194/se-9-75-2018, 2018
Short summary
Short summary
The severity of land degradation was assessed by analysing the physico-chemical parameters and correlating with satellite data in the Bathinda district, Punjab. Most of the soil samples were slightly or moderately saline, while a few were calcareous and alkaline. Comparing the satellite datasets of 2000 and 2014 revealed an increase in settlements and a decrease in barren area. The study can be useful for soil and environmental scientists and planning agencies for restoration of degraded lands.
Fabio Terribile, Michela Iamarino, Giuliano Langella, Piero Manna, Florindo Antonio Mileti, Simona Vingiani, and Angelo Basile
Solid Earth, 9, 63–74, https://doi.org/10.5194/se-9-63-2018, https://doi.org/10.5194/se-9-63-2018, 2018
Short summary
Short summary
Andic soils have unique morphological, physical and chemical properties that induce both considerable soil fertility and great vulnerability to land degradation. Here we attempt to show that soils rich in poorly crystalline clay minerals have an utmost ecological importance.
Our results are hoped to be a starting point for better understanding the ecological importance of andic soils and also possibly to better consider pedological information in carbon balance calculations.
Cheng-liang Zhang, Jing-jing Feng, Li-ming Rong, and Ting-ning Zhao
Solid Earth, 8, 1131–1139, https://doi.org/10.5194/se-8-1131-2017, https://doi.org/10.5194/se-8-1131-2017, 2017
Short summary
Short summary
A mixture of landfill stabilized waste and rock fragments (LGM) can be used as topsoil substitute during ecological restoration in abandoned quarries. Target species grew best when the volume fraction of landfill stabilized waste was 50 %. Moderate compaction enhanced plant growth in LGM when the volume fraction of landfill stabilized waste was lower than 20 %.
Chengyou Cao, Ying Zhang, Wei Qian, Caiping Liang, Congmin Wang, and Shuang Tao
Solid Earth, 8, 1119–1129, https://doi.org/10.5194/se-8-1119-2017, https://doi.org/10.5194/se-8-1119-2017, 2017
Short summary
Short summary
The influences of land-use conversion on soil properties and bacterial communities were assessed. Diversity was detected in four distinct land-use systems through high-throughput sequencing. Land-use changes affected soil properties and bacterial community structures. The microbial dominant taxa were unchanged, but their relative abundances were significantly different, indicating that the effects of land-use conversion on bacterial communities were more quantitative than qualitative.
Ron Corstanje, Theresa G. Mercer, Jane R. Rickson, Lynda K. Deeks, Paul Newell-Price, Ian Holman, Cedric Kechavarsi, and Toby W. Waine
Solid Earth, 8, 1003–1016, https://doi.org/10.5194/se-8-1003-2017, https://doi.org/10.5194/se-8-1003-2017, 2017
Short summary
Short summary
This research assessed whether physical soil properties can be used to indicate the quality of British soils in terms of their delivery of ecosystem goods and services. A prioritised list of physical
soil quality indicators(SQIs) were tested for robustness, spatial and temporal variability, and expected rate of change. Seven SQIs were selected: soil packing density, water retention characteristics, aggregate stability, rate of soil erosion, soil depth, soil structure and soil sealing.
Huizhong Lu, Longxi Cao, Yin Liang, Jiuqin Yuan, Yayun Zhu, Yi Wang, Yalan Gu, and Qiguo Zhao
Solid Earth, 8, 845–855, https://doi.org/10.5194/se-8-845-2017, https://doi.org/10.5194/se-8-845-2017, 2017
Sunday Adenrele Adeniyi, Willem Petrus de Clercq, and Adriaan van Niekerk
Solid Earth, 8, 827–843, https://doi.org/10.5194/se-8-827-2017, https://doi.org/10.5194/se-8-827-2017, 2017
Short summary
Short summary
Cocoa agroecosystems are a major land use type in West Africa, reportedly associated with the problem of soil degradation. This study developed a composite soil degradation assessment index (CSDI) for determining the degradation status of cocoa soils under smallholder farming systems in southwestern Nigeria. The newly developed index can show early warning signs of soil degradation, which can help farmers and extension officers to implement rehabilitation practices on degraded cocoa soils.
Cheng Zeng, Shijie Wang, Xiaoyong Bai, Yangbing Li, Yichao Tian, Yue Li, Luhua Wu, and Guangjie Luo
Solid Earth, 8, 721–736, https://doi.org/10.5194/se-8-721-2017, https://doi.org/10.5194/se-8-721-2017, 2017
Short summary
Short summary
This paper describes methodological experience and provides data references for international counterparts to study soil erosion in karst landform areas. The lithological and desertification factors introduced in the soil erosion model accurately reflect and predict soil erosion conditions and spatial distribution characteristics in karst areas. Future studies on soil erosion in karst areas should include underground loss in the calculation scope.
Ece Aksoy, Mirko Gregor, Christoph Schröder, Manuel Löhnertz, and Geertrui Louwagie
Solid Earth, 8, 683–695, https://doi.org/10.5194/se-8-683-2017, https://doi.org/10.5194/se-8-683-2017, 2017
Short summary
Short summary
The aim of this study is to relate the potential of land for a particular use in a given region with the actual land use. To this aim, the impact of several land cover flows related to urban development on soils with good, average, and poor production potentials were assessed and mapped. Thus, the amount and quality (potential for agricultural production) of agricultural land lost between the years 2000 and 2006 and the regions with major impact (hot spots) in Europe were identified.
Yue Li, Xiao Yong Bai, Shi Jie Wang, Luo Yi Qin, Yi Chao Tian, and Guang Jie Luo
Solid Earth, 8, 661–669, https://doi.org/10.5194/se-8-661-2017, https://doi.org/10.5194/se-8-661-2017, 2017
Short summary
Short summary
First, we report the following discovery: T values are spatially heterogeneous, and a minimum of three criteria should be considered instead of only a single criterion in karst areas. In fact, our findings disprove the old “one region, one T value” concept.
Second, we proposed a new viewpoint: in karst regions, a large soil erosion modulus does not correspond to severe soil erosion. Although T value can reflect soil sensitivity, this value cannot indicate soil erosion risk.
Cevdet Şeker, Hasan Hüseyin Özaytekin, Hamza Negiş, İlknur Gümüş, Mert Dedeoğlu, Emel Atmaca, and Ümmühan Karaca
Solid Earth, 8, 583–595, https://doi.org/10.5194/se-8-583-2017, https://doi.org/10.5194/se-8-583-2017, 2017
Ekaterina Maksimova and Evgeny Abakumov
Solid Earth, 8, 553–560, https://doi.org/10.5194/se-8-553-2017, https://doi.org/10.5194/se-8-553-2017, 2017
Short summary
Short summary
Two fire-affected soils have been studied using micromorphological methods. The objective of the paper is to assess and compare fire effects on the micropedological organisation of soils in a forest-steppe zone of central Russia. The burnt soils differ from the control on a macromorphological level only in the upper part of the profile where the litter is transformed to ash identified as a dim grey organomineral mixture. Processes of soil erosion are clearly manifested 1 year after the fire.
Zheng-Guo Sun, Jie Liu, and Hai-Yang Tang
Solid Earth, 8, 545–552, https://doi.org/10.5194/se-8-545-2017, https://doi.org/10.5194/se-8-545-2017, 2017
Short summary
Short summary
To simulate grassland NPP in Southern China, a new model was built and validated based on data recorded from 2003 to 2014. There was a highly significant correlation between simulated and measured NPP. The NPP values had a decreasing trend from east to west and south to north. Mean NPP was 471.62 g C m−2 from 2003 to 2014. Additionally, the mean annual NPP presented a rising trend, increasing 3.49 g C m−2 yr−1.
Yusong Deng, Chongfa Cai, Dong Xia, Shuwen Ding, Jiazhou Chen, and Tianwei Wang
Solid Earth, 8, 499–513, https://doi.org/10.5194/se-8-499-2017, https://doi.org/10.5194/se-8-499-2017, 2017
Short summary
Short summary
Soil is a sphere of the earth system with a special structure and function. From the point of view of the earth system, soil science should not only study the soil material but also change towards the relationship between the soil and the
earth system, which has a profound impact on the human living environment and global change research. The results show the relationship between soil Atterberg limits and the occurrence mechanism of collapsing gullies, which can be used as a reference.
Katrin M. Wild, Patric Walter, and Florian Amann
Solid Earth, 8, 351–360, https://doi.org/10.5194/se-8-351-2017, https://doi.org/10.5194/se-8-351-2017, 2017
Linhua Wang, Bo Ma, and Faqi Wu
Solid Earth, 8, 281–290, https://doi.org/10.5194/se-8-281-2017, https://doi.org/10.5194/se-8-281-2017, 2017
Short summary
Short summary
Soil and water losses in agriculture are a major environmental problem on the Loess Plateau, China. This study investigated the effects of wheat stubble on soil erosion in laboratory plots under simulated rainfall. These results show that the traditional plow may induce more serious soil and water losses compared to wheat stubble cover. Wheat stubble cover delayed runoff generation time, decreased the runoff and sediment loss, and increased rainwater infiltration into the soil.
Debashis Mandal, Pankaj Srivastava, Nishita Giri, Rajesh Kaushal, Artemi Cerda, and Nurnabi Meherul Alam
Solid Earth, 8, 217–233, https://doi.org/10.5194/se-8-217-2017, https://doi.org/10.5194/se-8-217-2017, 2017
Metin Mujdeci, Ahmet Ali Isildar, Veli Uygur, Pelin Alaboz, Husnu Unlu, and Huseyin Senol
Solid Earth, 8, 189–198, https://doi.org/10.5194/se-8-189-2017, https://doi.org/10.5194/se-8-189-2017, 2017
Short summary
Short summary
Organic matter addition is an efficient way of reducing the effects of field traffic. The depth-dependent (0–10 and 10–20 cm) changes in some physical soil traits such as penetration resistance, bulk density, and porosity as a function of tractor passes and organic matter addition to clay soil.
The enhancing effects of treatments on the investigated parameters were C>GM>FYM. The increase in tillage lines made the soil properties worse and corresponded with the type of organic matter.
M. Abdulaha-Al Baquy, Jiu-Yu Li, Chen-Yang Xu, Khalid Mehmood, and Ren-Kou Xu
Solid Earth, 8, 149–159, https://doi.org/10.5194/se-8-149-2017, https://doi.org/10.5194/se-8-149-2017, 2017
Short summary
Short summary
Al toxicity to plants and soil infertility in acidic soils are the main limiting factors for crop growth. To establish which acid soils need to be ameliorated for plant growth, the parameters of critical soil pH and soil Al concentration must be determined. The critical soil pH and exchangeable aluminium of two Ultisols for wheat and canola production were determined in this study. The results obtained will provide useful references for the utilization and management of acid soils.
Wei Li, Howard E. Epstein, Zhongming Wen, Jie Zhao, Jingwei Jin, Guanghua Jing, Jimin Cheng, and Guozhen Du
Solid Earth, 8, 137–147, https://doi.org/10.5194/se-8-137-2017, https://doi.org/10.5194/se-8-137-2017, 2017
Short summary
Short summary
This is an interesting piece of work and makes a nice contribution to the knowledge on how aboveground vegetation can control belowground soil properties through functional traits and functional diversity. Functional traits are the center of recent attempts to unify key ecological theories on species coexistence and assembly in communities. The results presented are valuable for understanding the relationship between species traits, functional diversity, and soil properties.
Yu Liu, Fuping Tian, Pengyan Jia, Jingge Zhang, Fujiang Hou, and Gaolin Wu
Solid Earth, 8, 83–91, https://doi.org/10.5194/se-8-83-2017, https://doi.org/10.5194/se-8-83-2017, 2017
Tegegne Molla and Biniam Sisheber
Solid Earth, 8, 13–25, https://doi.org/10.5194/se-8-13-2017, https://doi.org/10.5194/se-8-13-2017, 2017
Short summary
Short summary
This study was conducted to estimate the rate of soil erosion and to evaluate the existing SWC strategies in the Koga watershed. A mixed approach of field investigation and an integrated RUSLE model modified for Ethiopian highlands is being adopted for soil erosion assessment. Most of the existing SWC structures fail to meet the standard due to deficient construction and management of SWC structures. The soil erosion rate is by far higher than the tolerable soil loss rate.
Bülent Turgut and Merve Ateş
Solid Earth, 8, 1–12, https://doi.org/10.5194/se-8-1-2017, https://doi.org/10.5194/se-8-1-2017, 2017
Short summary
Short summary
The soil properties of Batumi delta, an important area for agricultural production and biodiversity in the southwest of Georgia, have not been studied yet. In order to provide scientific data, soil samples were taken from different points of delta and their basic characteristics were determined. At the end of the study, the results indicated that the soil properties were affected by the formation time and land use, and the relations between the soil properties varied depending on these factors.
Lei Wu, Xia Liu, and Xiaoyi Ma
Solid Earth, 7, 1577–1590, https://doi.org/10.5194/se-7-1577-2016, https://doi.org/10.5194/se-7-1577-2016, 2016
Short summary
Short summary
1. A distributed and dynamic sediment yield model for loess hilly area was modified. 2. Spatiotemporal evolution of sediment in an easily eroded watershed was estimated. 3. Effects of returning farmland on erosion and sediment yield were evaluated.
Jinfei Yin, Ruzhen Wang, Heyong Liu, Xue Feng, Zhuwen Xu, and Yong Jiang
Solid Earth, 7, 1565–1575, https://doi.org/10.5194/se-7-1565-2016, https://doi.org/10.5194/se-7-1565-2016, 2016
Short summary
Short summary
In this paper we report on changes in elemental stoichiometry as affected by the nitrogen addition effect within three soil aggregate fractions of large macroaggregates (> 2000 μm), small macroaggregates (250–2000 μm), and microaggregates (< 250 μm) in a temperate steppe.
Paloma Hueso-González, Juan Francisco Martínez-Murillo, and Jose Damian Ruiz-Sinoga
Solid Earth, 7, 1479–1489, https://doi.org/10.5194/se-7-1479-2016, https://doi.org/10.5194/se-7-1479-2016, 2016
Short summary
Short summary
The development of alternative low-cost and low-environmental-impact revegetation methods is necessary for the effective management of Mediterranean forest environments. This research assessed the effects of five types of soil amendment on the success of afforestation processes. In terms of land management, the study shows that the addition of mulch or hydroabsorbent polymer can reduce transplanting stress and improve the success of afforestation programs.
Hüseyin Şenol, Tülay Tunçay, and Orhan Dengiz
Solid Earth Discuss., https://doi.org/10.5194/se-2016-105, https://doi.org/10.5194/se-2016-105, 2016
Preprint withdrawn
Short summary
Short summary
In this study the features of pedogenic evolution of four soil profiles formed in topographically different positions of the southwestern–northeastern direction were investigated. The results of the study showed a strong relationship between the topography and some of the soil’s morphological, mineralogical, physical and chemical characteristics. Soil depth and physical soil features such as texture, structure and bulk density were found to improve downwards within the toposequence.
Carlos Asensio, Francisco Javier Lozano, Pedro Gallardo, and Antonio Giménez
Solid Earth, 7, 1233–1242, https://doi.org/10.5194/se-7-1233-2016, https://doi.org/10.5194/se-7-1233-2016, 2016
Short summary
Short summary
Climate and soil surface conditions influence the erosive capacity of the wind, causing loss of soil productivity. Wind erosion leads soil drying and its loss of nutrients, and this in turn is conditioned by soil surface compaction. The impact of management on most of soil properties and on its wind erodibility determines agricultural productivity and sustainability. We used a new wind tunnel to evaluate all these acts.
Cited articles
Alexandre, A., Meunier, J.-D., Colin, F., and Koud, J.-M.: Plant impact on the biogeochemical cycle of silicon and related weathering processes, Geochim. Cosmochim. Ac., 61, 677–682, https://doi.org/10.1016/S0016-7037(97)00001-X, 1997.
Ameijeiras-Mariño, Y.: Changes in soil chemical weathering intensity after forest conversion to cropland: importance of slope geomorphology, in: The response of soil chemical weathering to physical erosion: integrating the impact of forest conversion, edited by: Université catholique de Louvain (UCL), PhD thesis, Belgium, 2017.
Barão, L., Clymans, W., Vandevenne, F., Meire, P., Conley, D. J., and Struyf, E.: Pedogenic and biogenic alkaline-extracted silicon distributions along a temperate land-use gradient, Eur. J. Soil Sci., 65, 693–705, https://doi.org/10.1111/ejss.12161, 2014.
Barão, L., Vandevenne, F., Clymans, W., Frings, P., Ragueneau, O., Meire, P., Conley, D. J., and Struyf, E.: Alkaline-extractable silicon from land to ocean: A challenge for biogenic silicon determination, Limnol. Oceanogr. Methods, 13, 329–344, https://doi.org/10.1002/lom3.10028, 2015.
Bartoli, F.: Crystallochemistry and surface properties of biogenic opal, J. Soil Sci., 36, 335–350, https://doi.org/10.1111/j.1365-2389.1985.tb00340.x, 1985.
Blecker, S. W., Mcculley, R. L., Chadwick, O. A., and Kelly, E. F.: Biologic cycling of silica across a grassland bioclimosequence, Global Biogeochem. Cy., 20, 1–11, https://doi.org/10.1029/2006GB002690, 2006.
Campforts, B., Van de Broek, M., Trigalet, S., Schoonejans, J., Robinet, J., Unzué-Belmonte, D., Ameijeiras-Mariño, Y., Vermeire, M. L., and Minella, J.: Soil texture data Brazilian SOGLO field sites, available at: https://doi.org/10.17632/pcbpbx5x7n.1 (last access: 27 June 2017), 2016.
Chadwick, O. A., Hendricks, D. M., and Nettleton, W. D.: Silica in Duric Soils: II. Mineralogy1, Soil Sci. Soc. Am. J., 51, 982–985, https://doi.org/10.2136/sssaj1987.03615995005100040029x, 1987.
Chao, T. T. and Sanzolone, R. F.: Decomposition techniques, J. Geochemical Explor., 44, 65–106, 1992.
Clymans, W., Struyf, E., Govers, G., Vandevenne, F., and Conley, D. J.: Anthropogenic impact on amorphous silica pools in temperate soils, Biogeosciences, 8, 2281–2293, https://doi.org/10.5194/bg-8-2281-2011, 2011.
Clymans, W., Struyf, E., Van den Putte, A., Langhans, C., Wang, Z., and Govers, G.: Amorphous silica mobilization by inter-rill erosion: Insights from rainfall experiments, Earth Surf. Proc. Land., 40, 1171–1181, https://doi.org/10.1002/esp.3707, 2015.
Conley, D. J., Likens, G. E., Buso, D. C., Saccone, L., Bailey, S. W., and Johnson, C. E.: Deforestation causes increased dissolved silicate losses in the Hubbard Brook Experimental Forest, Glob. Chang. Biol., 14, 2548–2554, https://doi.org/10.1111/j.1365-2486.2008.01667.x, 2008.
Cornelis, J. and Delvaux, B.: Soil processes drive the biological silicon feedback loop, Funct. Ecol., 1, 1298–1310, https://doi.org/10.1111/1365-2435.12704, 2016.
Cornelis, J.-T., Delvaux, B., Georg, R. B., Lucas, Y., Ranger, J., and Opfergelt, S.: Tracing the origin of dissolved silicon transferred from various soil-plant systems towards rivers: a review, Biogeosciences, 8, 89–112, https://doi.org/10.5194/bg-8-89-2011, 2011.
Currie, H. A. and Perry, C. C.: Silica in Plants: Biological, Biochemical and Chemical Studies, Ann. Bot., 100, 1383–1389, https://doi.org/10.1093/aob/mcm247, 2007.
Delvaux, B., Herbillon, A. J., and Vielvoye, L.: Characterization of a weathering sequence of soils derived from volcanic ash in Cameroon. Taxonomic, mineralogical and agronomic implications, Geoderma, 45, 375–388, https://doi.org/10.1016/0016-7061(89)90017-7, 1989.
DeMaster, D. J.: The supply and accumulation of silica in the marine environment, Geochim. Cosmochim. Ac., 45, 1715–1732, https://doi.org/10.1016/0016-7037(81)90006-5, 1981.
Derry, L. A., Kurtz, A. C., Ziegler, K., and Chadwick, O. A.: Biological control of terrestrial silica cycling and export fluxes to watersheds, Nature, 433, 728–31, https://doi.org/10.1038/nature03299, 2005.
Doetterl, S., Cornelis, J.-T., Six, J., Bodé, S., Opfergelt, S., Boeckx, P., and Van Oost, K.: Soil redistribution and weathering controlling the fate of geochemical and physical carbon stabilization mechanisms in soils of an eroding landscape, Biogeosciences, 12, 1357–1371, https://doi.org/10.5194/bg-12-1357-2015, 2015.
Drees, L. R., Wilding, L. P., Smeck, N. E., and Senkayi, A. L.: Silica in soils: quartz and disorders polymorphs, in Minerals in soil environments, 914–974, Soil Science Society of America, Madison, 1989.
Drever, J. I.: The effect of land plants on weathering rates of silicate minerals, Geochim. Cosmochim. Ac., 58, 2325–2332, https://doi.org/10.1016/0016-7037(94)90013-2, 1994.
Fraysse, F., Pokrovsky, O. S., Schott, J., and Meunier, J.: Surface properties, solubility and dissolution kinetics of bamboo phytoliths, 70, 1939–1951, https://doi.org/10.1016/j.gca.2005.12.025, 2006.
Fraysse, F., Pokrovsky, O. S., Schott, J., and Meunier, J.-D.: Surface chemistry and reactivity of plant phytoliths in aqueous solutions, Chem. Geol., 258, 197–206, https://doi.org/10.1016/j.chemgeo.2008.10.003, 2009.
Govers, G., Quine, T. A., Desmet, P. J. J., and Walling, D. E.: The relative contribution of soil tillage and overland flow erosion to soil redistribution on agricultural land, Earth Surf. Proc. Land., 21, 929–946, https://doi.org/10.1002/(SICI)1096-9837(199610)21:10<929::AID-ESP631>3.0.CO;2-C, 1996.
Guntzer, F., Keller, C., Poulton, P. R., McGrath, S. P., and Meunier, J. D.: Long-term removal of wheat straw decreases soil amorphous silica at Broadbalk, Rothamsted, Plant Soil, 352, 173–184, https://doi.org/10.1007/s11104-011-0987-4, 2012.
Hall, T. B., Rosillo-Calle, F., Williams, R. H., and Woods, J.: Biomass for energy: supply prospects, in: Renewable Energy: Sources for Fuels and Electricity, edited by: Hall, R. H., Kelly, T. B., Reddy, H., Williams, A. K. N., 593–651, Island Press, Washington DC, 1993.
Herbillon, A. J.: Chemical estimation of weatherable minerals present in the diagnostic horizons of low activity clay soils, in: Proceedings of the 8th International Soil Classification Work-shop: Classification, Characterization and Utilization of Oxisols, Part 1, edited by: EMBRAPA, 39–48, Rio de Janeiro, 1986.
Ibrahim, M. A. and Lal, R.: Catena Soil carbon and silicon pools across an un-drained toposequence in central Ohio, Catena, 120, 57–63, https://doi.org/10.1016/j.catena.2014.04.006, 2014.
IUSS Working Group WRB: World Reference Base for Soil Resources 2014, update 2015, International soil classification system for naming soils and creating legends for soil maps, World Soil Resources Reports No. 106, FAO, Rome, 2015.
Jones, L. H. P. and Handreck, K. A.: Effects of Iron and Aluminium Oxides on Silica in Solution in Soils, Nature, 198, 852–853, https://doi.org/10.1038/198852a0, 1963.
Keller, C., Guntzer, F., Barboni, D., Labreuche, J., and Meunier, J. D.: Impact of agriculture on the Si biogeochemical cycle: Input from phytolith studies, C. R. Geosci., 344, 739–746, https://doi.org/10.1016/j.crte.2012.10.004, 2012.
Kelly, E. F., Chadwick, O. A., and Hilinski, T. E.: The effect of plants on mineral weathering, Biogeochemistry, 42, 21–53, https://doi.org/10.1007/978-94-017-2691-7_2, 1998.
Kendrick, K. J. and Graham, R. C.: Pedogenic silica accumulation in chronosequence soils, southern California, Soil Sci. Soc. Am. J., 68, 1295–1303, 2004.
Kirchholtes, R. P. J., van Mourik, J. M., and Johnson, B. R.: Phytoliths as indicators of plant community change: A case study of the reconstruction of the historical extent of the oak savanna in the Willamette Valley Oregon, USA, Catena, 132, 89–96, https://doi.org/10.1016/j.catena.2014.11.004, 2015.
Koning, E., Epping, E., and Van Raaphorst, W.: Determining Biogenic Silica in Marine Samples by Tracking Silicate and Aluminium Concentrations in Alkaline Leaching Solutions, Aquat. Geochem., 8, 37–67, https://doi.org/10.1023/A:1020318610178, 2002.
Kottek, M., Grieser, J., Beck, C., Rudolf, B., and Rubel, F.: World Map of the Köppen-Geiger climate classification updated, Meteorol. Z., 15, 259–263, https://doi.org/10.1127/0941-2948/2006/0130, 2006.
Li, Z., Song, Z., Parr, J. F., and Wang, H.: Occluded C in rice phytoliths: implications to biogeochemical carbon sequestration, Plant Soil, 370, 615–623, https://doi.org/10.1007/s11104-013-1661-9, 2013.
Lindsay, W. L.: Chemical equilibria in soils, Wiley, New York, available at: http://soils.ifas.ufl.edu/lqma/SEED/CWR6252/Handout/Chemical equilibira.pdf (last access: 27 June 2017), 1979.
Meunier, J., Colin, F., and Alarcon, C.: Biogenic silica storage in soils, Geology, 27, 835–838, https://doi.org/10.1130/0091-7613, 1999.
Meunier, J. D., Kirman, S., Strasberg, D., Nicolini, E., Delcher, E., and Keller, C.: The output and bio-cycling of Si in a tropical rain forest developed on young basalt flows (La Reunion Island), Geoderma, 159, 431–439, https://doi.org/10.1016/j.geoderma.2010.09.010, 2010.
Minella, J. P. G., Walling, D. E., and Merten, G. H.: Establishing a sediment budget for a small agricultural catchment in southern Brazil, to support the development of effective sediment management strategies, J. Hydrol., 519, 2189–2201, https://doi.org/10.1016/j.jhydrol.2014.10.013, 2014.
Montgomery, D. R. and Brandon, M. T.: Topographic controls on erosion rates in tectonically active mountain ranges, Earth Planet. Sci. Lett., 201, 481–489, https://doi.org/10.1016/S0012-821X(02)00725-2, 2002.
Opfergelt, S., de Bournonville, G., Cardinal, D., André, L., Delstanche, S., and Delvaux, B.: Impact of soil weathering degree on silicon isotopic fractionation during adsorption onto iron oxides in basaltic ash soils, Cameroon, Geochim. Cosmochim. Ac., 73, 7226–7240, https://doi.org/10.1016/j.gca.2009.09.003, 2009.
Opfergelt, S., Cardinal, D., André, L., Delvigne, C., Bremond, L., and Delvaux, B.: Variations of δ30Si and Ge ∕ Si with weathering and biogenic input in tropical basaltic ash soils under monoculture, Geochim. Cosmochim. Ac., 74, 225–240, https://doi.org/10.1016/j.gca.2009.09.025, 2010.
Parr, J., Sullivan, L., Chen, B., Ye, G., and Zheng, W.: Carbon bio-sequestration within the phytoliths of economic bamboo species, Glob. Chang. Biol., 16, 2661–2667, https://doi.org/10.1111/j.1365-2486.2009.02118.x, 2010.
Piperno, D. R.: Phytoliths: A Comprehensive Guide for Archaeologists and Paleoecologists, Altamira Press, San Diego, 2006.
Robert, M. and Tessier, D.: Méthode de préparation des argiles des sols pour des études minéralogiques, Ann. Agron., 25, 859–882, 1974.
Ronchi, B., Barão, L., Clymans, W., Vandevenne, F., Batelaan, O., Govers, G., Struyf, E., and Dassargues, A.: Factors controlling Si export from soils: A soil column approach, Catena, 133, 85–96, https://doi.org/10.1016/j.catena.2015.05.007, 2015.
Rovner, I.: Potential of opal phytoliths for use in paleoecological reconstruction, Quat. Res., 1, 343–359, https://doi.org/10.1016/0033-5894(71)90070-6, 1971.
Saccone, L., Conley, D. J., Koning, E., Sauer, D., Sommer, M., Kaczorek, D., Blecker, S. W., and Kelly, E. F.: Assessing the extraction and quantification of amorphous silica in soils of forest and grassland ecosystems, Eur. J. Soil Sci., 58, 1446–1459, https://doi.org/10.1111/j.1365-2389.2007.00949.x, 2007.
Santos, G. M. and Alexandre, A.: Earth-Science Reviews The phytolith carbon sequestration concept: Fact or fiction? A comment on “Occurrence, turnover and carbon sequestration potential of phytoliths in terrestrial ecosystems by Song et al. https://doi.org/10.1016/j.earscirev.2016.04.007”, Earth Sci. Rev., 164, 251–255, https://doi.org/10.1016/j.earscirev.2016.11.005, 2017.
Sauer, D., Saccone, L., Conley, D. J., Herrmann, L., and Sommer, M.: Review of methodologies for extracting plant-available and amorphous Si from soils and aquatic sediments, Biogeochemistry, 80, 89–108, https://doi.org/10.1007/s10533-005-5879-3, 2006.
Smis, A., Van Damme, S., Struyf, E., Clymans, W., Van Wesemael, B., Frot, E., Vandevenne, F., Van Hoestenberghe, T., Govers, G., and Meire, P.: A trade-off between dissolved and amorphous silica transport during peak flow events (Scheldt river basin, Belgium): Impacts of precipitation intensity on terrestrial Si dynamics in strongly cultivated catchments, Biogeochemistry, 106, 475–487, https://doi.org/10.1007/s10533-010-9527-1, 2011.
Sommer, M., Kaczorek, D., Kuzyakov, Y., and Breuer, J.: Silicon pools and fluxes in soils and landscapes – a review, J. Plant Nutr. Soil Sci., 169, 310–329, https://doi.org/10.1002/jpln.200521981, 2006.
Sommer, M., Jochheim, H., Höhn, A., Breuer, J., Zagorski, Z., Busse, J., Barkusky, D., Meier, K., Puppe, D., Wanner, M., and Kaczorek, D.: Si cycling in a forest biogeosystem – the importance of transient state biogenic Si pools, Biogeosciences, 10, 4991–5007, https://doi.org/10.5194/bg-10-4991-2013, 2013.
Song, Z., Wang, H., Strong, P. J., Li, Z., and Jiang, P.: Plant impact on the coupled terrestrial biogeochemical cycles of silicon and carbon: Implications for biogeochemical carbon sequestration, Earth-Sci. Rev., 115, 319–331, https://doi.org/10.1016/j.earscirev.2012.09.006, 2012.
Song, Z., Müller, K., and Wang, H.: Biogeochemical silicon cycle and carbon sequestration in agricultural ecosystems, Earth-Sci. Rev., 139, 268–278, https://doi.org/10.1016/j.earscirev.2014.09.009, 2014.
Song, Z., McGrouther, K., and Wang, H.: Occurrence, turnover and carbon sequestration potential of phytoliths in terrestrial ecosystems, Earth-Sci. Rev., 158, 19–30, https://doi.org/10.1016/j.earscirev.2016.04.007, 2016.
Struyf, E. and Conley, D. J.: Emerging understanding of the ecosystem silica filter, Biogeochemistry, 107, 9–18, https://doi.org/10.1007/s10533-011-9590-2, 2012.
Struyf, E., Temmerman, S., and Meire, P.: Dynamics of biogenic Si in freshwater tidal marshes: Si regeneration and retention in marsh sediments (Scheldt estuary), Biogeochemistry, 82, 41–53, https://doi.org/10.1007/s10533-006-9051-5, 2007.
Struyf, E., Smis, A., Van Damme, S., Garnier, J., Govers, G., Van Wesemael, B., Conley, D. J., Batelaan, O., Frot, E., Clymans, W., Vandevenne, F., Lancelot, C., Goos, P., and Meire, P.: Historical land use change has lowered terrestrial silica mobilization, Nat. Commun., 1, 129, https://doi.org/10.1038/ncomms1128, 2010.
Uehara, G. and Gillman, G.: The Mineralogy, Chemistry, and Physics of Tropical Soils With Variable Charge Clays, West View Press, Boulder, CO, USA, 1981.
Unzué-Belmonte, D., Struyf, E., Clymans, W., Tischer, A., Potthast, K., Bremer, M., Meire, P., and Schaller, J.: Fire enhances solubility of biogenic silica, Sci. Total Environ., 572, 1289–1296, https://doi.org/10.1016/j.scitotenv.2015.12.085, 2016.
Unzué-Belmonte, D., Ameijeiras-Mariño, Y., Trigalet, S., Schoonejans, J., Campforts, B., Van de Broek, M., Robinet, J., and Minella, J.: Alkaline Extractable Silica – SOGLO Project, available at: https://doi.org/10.17632/r996jnwhtg.1, last access: 27 June 2017.
Vanacker, V., Bellin, N., Molina, A., and Kubik, P. W.: Erosion regulation as a function of human disturbances to vegetation cover: a conceptual model, Landsc. Ecol, 29, 293–309, https://doi.org/10.1007/s10980-013-9956-z, 2014.
Van Cappellen, P.: Biomineralization and global biogeochemical cycles, Rev. Mineral. Geochemistry, 54, 357–381, https://doi.org/10.2113/0540357, 2003.
Vandevenne, F., Struyf, E., Clymans, W., and Meire, P.: Agricultural silica harvest: have humans created a new loop in the global silica cycle?, Front. Ecol. Environ., 10, 243–248, https://doi.org/10.1890/110046, 2012.
Vandevenne, F. I., Barão, L., Ronchi, B., Govers, G., Meire, P., Kelly, E. F., and Struyf, E.: Silicon pools in human impacted soils of temperate zones, Global Biogeochem. Cy., 29, 1439–1450, https://doi.org/10.1002/2014GB005049, 2015a.
Vandevenne, F. I., Delvaux, C., Hughes, H. J., André, L., Ronchi, B., Clymans, W., Barão, L., Cornelis, J.-T., Govers, G., Meire, P., and Struyf, E.: Landscape cultivation alters δ30Si signature in terrestrial ecosystems, Sci. Rep., 5, 7732, https://doi.org/10.1038/srep07732, 2015b.
Von Braun, J.: The world food situation: new driving forces and required actions, Food Policy Reports 18, International Food Policy Research Institute, Washington DC, 2007.
Watteau, F. and Villemin, G.: Ultrastructural study of the biogeochemical cycle of silicon in the soil and litter of a temperate forest, Eur. J. Soil Sci., 52, 385–396, https://doi.org/10.1046/j.1365-2389.2001.00391.x, 2001.
Wei, X., Shao, M., Gale, W., and Li, L.: Global pattern of soil carbon losses due to the conversion of forests to agricultural land, Sci. Rep., 1, 6–11, https://doi.org/10.1038/srep04062, 2014.
Short summary
We studied the effect of land conversion and erosion intensity on the biogenic silica (BSi) pools in a subtropical soil in the south of Brazil. Our study shows that deforestation will rapidly (< 50 years) deplete (10–53 %) the biogenic alkaline extractable Si (AlkExSi) pool in soils. Higher erosion in steeply sloped sites implies increased deposition of biogenic Si in deposition zones near the bottom of the slope, where rapid burial can cause removal of BSi from biologically active zones.
We studied the effect of land conversion and erosion intensity on the biogenic silica (BSi)...
