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Wang, J., Chen, Y., Shao, X., Zhang, Y. & Cao, Y. 2012. Land-use changes and policy dimension driving forces in China: Present, trend and future. Land Use Policy, 29: 737-749. Warren, M.W., Kauffman, J.B., Murdiyarso, D., Anshari, G., Hergoualc’h, K., Kurnianto, S., Purbopuspito, J., Gusmayanti, E., Afifudin, M., Rahajoe, J., Alhamd, L., Limin, S. & Iswandi, A. 2012. A cost-efficient method to assess carbon stocks in tropical peat soil. Biogeosciences, 9: 4477–4485. We i, C.Y. & Chen, T.B. 2001. Hyperaccumulators and phytoremediation of heavy metal contaminated soil: a review of studies in China and abroad. Acta Ecologica Sinica, 21: 1196-1203. Widowati, W., De Neve, L.R., Sukristiyonubowo, S., Setyorini, D., Kasno, A., Sihaputar, I.A. & Sukristiyohastomo. 2011. Nitrogen balances and nitrogen uses efficiency of intensive vegetable rotations in South East Asian tropical Andisols. Nutr. Cycling Agroecosys., 91: 131-143. Williams, M., Fordyce, F., Paijitprapapong, P. & Charoenchaisri, P. 1996. Arsenic contamination in surface drainage and groundwater in part of Southeast Asia tin belt, Nakhon Si Thammarat province, Southern Thailand. Environ. Geol., 27: 16-33. Wosten, J.H.M., Clymans, E., Page, S.E., Rieley, J.O. & Limin, S.H. 2008. Peat-water interrelationships in a tropical peatland ecosystem in Southeast Asia. Catena, 73: 212-224. Xie, Z., Liu, G., Bei, Q., Chen, C., Cadisch, G., Liu, Q., Lin, Z., Hasegawa, T. and Zhu, J. 2014. Soil organic carbon stocks, changes and CO 2 mitigation potential by alteration of residue amendment pattern in China. In A. Hartemink & K. McSweeney, eds. Soil Carbon,, pp.457-466. Springer International Publishing. Xie, Z., Zhu, J., Liu, G., Cadisch, G., Hasegawa, T., Chen, C., Sun, H., Tang, H. & Zeng, Q. 2007. Soil organic stocks in China and changes from 1980s to 2000s. Global Change Biol., 13:1989-2007. Yagasaki, Y. & Shirato, Y. 2014. Assessment on the rates and potentials of soil organic carbon sequestration in agricultural lands in Japan using a process-based model and spatially explicit land-use change inventories – Part 1: Historical trend and validation based on nation-wide soil monitoring. Biogeosciences, 11: 4429-4442. Yan, X., Du, L., Shi, S. & Xing, G. 2000. Nitrous oxide emission from wetland rice soil as affected by the application of controlled-availability fertilizers and mid-season aeration. Biol. Fertil. Soils, 32: 60-66. Yan, X.Y., Akimoto, H. & Ohara, T. 2003. Estimation of nitrous oxide, nitric oxide and ammonia emissions from croplands in East, Southeast and South Asia. Global Change Biol., 9,:1080-1096. Yan, X.Y., Akiyama, H., Yagi, K. & Akimoto, H. 2009. Global estimations of the inventory and mitigation potential of methane emissions from rice cultivation conducted using the 2006 Intergovernmental Panel on Climate Change Guidelines. Global Biogeochem. Cycles, 23: GB 2002. doi:10.1029/2008GB 003299. Yan, Z., Liu, P., Li, Y., Ma, L., Alva, A., Dou, Z., Chen, Q. & Zhang, F. 2013. Phosphorus in China’s intensive vegetable production systems: Overfertilization, soil enrichment, and environmental implications. J. Environ. Qual., 42: 982-989. Yokoyama, K. & Taguchi, Y-H. 2013. Microbiology and biodiversity-based modelling of suppression of cottony leak of scarlet runner bean in soils with diverse and uniform ecology. J. Agric. Sci. Appl., 2: 35-44. Yokoyama, K. 1993. Evaluation of biodiversity of soil microbial community. In Symbiosphere: Ecological Complexity for Promoting Biodiversity, p. 74-78. Biology International special issue 29. International Union of Biological Sciences. Yu, Y.Y., Guo, Z.T., Wu, H.B., Kahmann, J.A. & Oldfield, F. 2009. Spatial changes in soil organic carbon density and storage of cultivated soils in China from 1980 to 2000. Global Biogeochem. Cycles, 23: GB 2021, doi: 2010.1029/2008GB 003428. Zhang, X.Y., Cruse, R.M., Sui, Y.Y. & Jhao, Z. 2006. Soil compaction induced by small tractor traffic in northeast China. Soil Sci. Soc. Am. J., 70: 613-619. Status of the World’s Soil Resources | Main Report Regional Assessment of Soil Changes 328 in Asia
Zhao, Y., Duan, L., Xing, J., Larssen, T., Nielsen, C.P. & Hao, J.M. 2009. Soil acidification in China: Is controlling SO 2 emissions enough? Environ. Sci. Tech., 43: 8021-8026. Zhou, G.Y., Liu, S.G., Li, Z.A., Zhang, D.Q., Tang, X.L., Zhou, C.Y., Yan, J.H. & Mo, J.M. 2006. Old-growth forests can accumulate carbon in Soils. Science, 314: 1417. Zhuang, P., Zou, B., Li, N.Y. & Li, Z.A. 2009. Heavy metal contamination in soils and food crops around Dabaoshan mine in Guangdong, China: implication for human health. Environ. Geochem. Health, 31: 707-715. Status of the World’s Soil Resources | Main Report Regional Assessment of Soil Changes 329 in Asia
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Status of the World’s Main Report
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Dick, Warren Dos Santos Baptista, I
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Table of contents Disclaimer and co
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4.1 | Current land cover and land u
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6.5.5 | Responses | 126 6.6 | Soil
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7.7.3 | Soil and drought hazard | 1
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9.5.2 | South Africa | 266 9.6 | Su
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12.3.8 | Soil acidification | 373 1
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14.5.4 | Nutrient imbalance | 464 1
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Foreword This document presents the
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Preface | Scope of The State of the
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Acknowledgments The Status of the W
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CACILM CAMRE CAZRI CBD CBM-CFS CCAF
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FDNPS FFS FIA FSI FSR GAP GDP GEF G
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LU MA MADRPM MAF MAFF MDBA MDGS MEN
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SKM SLAM SLC SLM SMAP SMOS SOC SOE
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List of tables Table 1.1 | Chronolo
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List of figures Figure 2.1 | Overvi
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Figure 6.15 | Factors controlling s
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Figure 11.4 | Soil map and soil deg
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colored diaper associated with micr
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Preface The main objectives of The
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Global soil resources Coordinating
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The balance between the supporting
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1.2 | Basic concepts Prior to the 2
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Soil functions and ecosystem servic
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Climate regulation ∑ Regulation o
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2 | The role of soils in ecosystem
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2.1.2 | Nature and formation of soi
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2.1.4 | Factors influencing soil C
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In coming years, human population a
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Management practices need to be imp
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Another important role of soil wate
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The development of molecular techno
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Fierer, N., Ladau, J., Clemente, J.
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Sato, T., Qadir, M., Yamamoto, S.,
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3 | Global Soil Resources 3.1 | The
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Fridland’s was the first attempt
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Soil management has a considerable
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Accumulation of water soluble salts
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and increases infiltration, which r
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Figure 3.7 Soil suitability for cro
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3.7 | Global assessments of soil ch
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3.7.2 | LADA-GLADIS: the ecosystem
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References AFES. 2008. Réferentiel
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Neustuev, S.S. 1931. Elements of So
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75% crops Mixed >50% artificial 50-
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or increasing forest areas. Between
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Degrading land covers approximately
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70 60 (A) soil carbon 50 Soil
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A meta-analysis of 57 publications
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the nutrient inputs remain in the c
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Livestock density Livestock product
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4.3.3 | Land use change resulting i
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Impact of land take Land take, by i
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Photo by F. Macias Photo by J.C. Fe
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The formation of sulfidic material
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are however strongly dependent on t
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Figure 4.10 Global distribution of
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Bardgett, R.D. & van der Putten, W.
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Dentener, F., Drevet, J., Lamarque,
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Hettelingh, J.P., Sliggers, J., van
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Magnani, F., Mencuccini, M., Borghe
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Pugh, T.A.M., Arneth, A., Olin, S.,
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Van Aardenne, J.A., Dentener, F.J.,
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5 | Drivers of global soil change D
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5.1.2 | Urbanization In tandem with
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Large areas of arable land have bee
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most affected zone with 15 million
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(Brito et al., 2005). This has impl
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MA. 2005. Ecosystems and Human Well
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6.1.2 | Status of Soil Erosion Over
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Figure 6.2 Location of active and f
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High soil erosion rates will also h
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Near-surface soil water content has
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6.2 | Global soil organic carbon st
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where the drainage in the 1960’s
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6.2.4 | Spatial distribution of car
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Vegetation Classes Topsoil Subsoil
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Soil Order Historic Area 10 6 ha Pr
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6.3 | Soil contamination status and
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and Uruguay. The number of exposed
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products increase soil acidity (Bar
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availability and inhibit plant grow
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In several Asian countries, a blend
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underlines the need for global-scal
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Figure 6.10 Urbanisation of the bes
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Figure 6.11 Major components of the
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Within the same continent, large va
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Box 6.2 | Nutrient balances in urba
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is among the top options in the por
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The quality of the soil’s water i
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At continental scales, the only pra
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Figure 6.16 (a) Global distribution
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Engineering in Japan, 5: 157-174. A
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Chadwick, D., Sommer, S., Thorman,
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Drechsel, Pay, Giordano, Mark, Gyie
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Gardner, T., Acosta-Martinez, V., C
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Hue, N.V. & Licudine, D.L. 1999. Am
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Liski, J., Ilvesniemi, H., Mäkelä
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Ng, H. 2010. Regional Assessment: S
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Reheis, M. 1997. Dust deposition do
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Smith, K.A., McTaggart, I.P. & Tsur
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United Nations. 2008. World Urbaniz
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Wood, M.K. & Blackburn, W.H. 1984.
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7 | The impact of soil change on ec
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Rockström et al. (2009) suggest we
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0.0 Response 1.0 Water quality Soil
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One approach to maintaining soil he
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Author Database Used Extent Estimat
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salinization. Safe design and opera
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The second limitation to prediction
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Figure 7.6 Some soil-related feedba
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soils occurs on largely unmanaged a
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extremes several weeks in advance (
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The direct effect of aerosols on th
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capacity declines as N loads increa
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The concept of the critical load of
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as it indicates that management and
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10-year frequency Ten-year frequenc
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phenomena such as the onset of mass
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Although poorly explored, diversity
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affect the health of humans and ani
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Bever, J.D., Westover, K.M. & Anton
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Damoah, R., Spichtinger, N., Servra
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Fenn, M.E., Poth, M.A., Aber, J.D.,
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Heimann, M. & Reichstein, M. 2008.
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Koster, R.D., Dirmeyer, P.A., Guo,
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Naeem, S., Bunker, D.E., Hector, A.
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Raufman, Y.J. & Fraser, R.S. 1997.
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Sheffield, J. & Wood, E.F. 2007. Pr
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UNEP. 2012. Policy Implications of
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8 | Governance and policy responses
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contemporary challenge for policy m
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Year 1982 FAO World Soil Charter 19
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Ensure integrated management of pes
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8.4 | Regional soil policies 8.4.1
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while in areas with fertile soils t
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In New Zealand, there are few regul
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The SEEA Central Framework identifi
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EC. 2013. Decision No 1386/2013/EU
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World Bank. 2011. Rising Global Int
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9.1 | Introduction Land degradation
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Figure 9.1 Agro-ecological zones in
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The soils are strongly weathered an
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It exposes the soil to the erosive
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In many African cultures, harvestin
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Maputo accounts for 83 percent of t
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Poverty: General poverty of the far
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Considering that over 80 percent of
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Extent of SOM decline in the region
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Many farmers do not follow recommen
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9.5 | Case studies 9.5.1 | Senegal
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Figure 9.7 Extent of dominant degra
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management, it is important to note
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From 2006, several further national
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Figure 9.12 Actual water erosion pr
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Figure 9.13 Topsoil pH derived from
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Figure 9.14 Change in land-cover be
Page 319 and 320: Waterlogging Compaction Soil sealin
Page 321 and 322: Birru, T.C. 2002. Organic matter re
Page 323 and 324: Hein, L. & De Ridder, N. 2006. Dese
Page 325 and 326: Meyer, J.H., Harding, R., Rampersad
Page 327 and 328: Smith P. 2008. Soil organic carbon
Page 329 and 330: 10 | Regional Assessment of Soil Ch
Page 331 and 332: Figure 10.1 Length of the available
Page 333 and 334: Figure 10.2 Threats to soils in the
Page 335 and 336: 10.3.4 | Soil acidification There i
Page 337 and 338: In paddy rice cultivation and uplan
Page 339 and 340: 10.3.10 | Sealing and capping Seali
Page 341 and 342: practices. On low slopes, agronomic
Page 343 and 344: (Valentin et al., 2008). For peatla
Page 345 and 346: in Laos (59 kg N ha -1 ). On the ot
Page 347 and 348: Sub-Regions. Inceptisols are the do
Page 349 and 350: 10.5.2 | Case study for Indonesia T
Page 351 and 352: Peat fire is another important proc
Page 353 and 354: An agricultural soil monitoring pro
Page 355 and 356: The Basic Soil-Environmental Monito
Page 357 and 358: Figure 10.8 Estimate CH 4 emission
Page 359 and 360: Threat to soil function Soil erosio
Page 361 and 362: References Aggarwal, G.C., Sidhu, A
Page 363 and 364: FAO. 2012. FAOSTAT. Rome, FAO. (Als
Page 365 and 366: Kukal, S.S. & Aggarwal, G.C. 2003.
Page 367 and 368: Piao, S., Fang, J., Ciais, P., Peyl
Page 369: Taniyama, I. 2003. Study of soil fa
Page 373 and 374: 11.1 | Introduction The majority of
Page 375 and 376: The internal stratification within
Page 377 and 378: Mediterranean zone This zone by def
Page 379 and 380: (5) Salinization and sodification I
Page 381 and 382: The real extent of diffuse soil con
Page 383 and 384: While there is no harmonised exhaus
Page 385 and 386: Prepared by I. Alyabina Figure 11.2
Page 387 and 388: This is due to the country’s geo-
Page 389 and 390: Future changes in climate and land
Page 391 and 392: Considering an increase of industri
Page 393 and 394: Comparison of cultivated soils with
Page 395 and 396: Figure 11.3 Some types and extent o
Page 397 and 398: The plains in the basins of Amu Dar
Page 399 and 400: Threat to soil function Soil sealin
Page 401 and 402: References Acosta, J.A., Faz, A., J
Page 403 and 404: Inisheva, L.I. (ed.). 2005. Concept
Page 405 and 406: van Lynden, G.W.J. 1997. Guidelines
Page 407 and 408: 12.1 | Introduction This chapter di
Page 409 and 410: Figure 12.1 Biomes in Latin America
Page 411 and 412: Temperate Grasslands, Savannahs and
Page 413 and 414: humid. The most common soil groups
Page 415 and 416: 12.3.6 | Compaction In LAC there ar
Page 417 and 418: New regional information has been g
Page 419 and 420: Primary forests have higher carbon
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Prepared by C. Cruz-Gaistardo Figur
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The salinity of soils on the cultiv
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Figure 12.6 Expansion of the agricu
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Figure 12.7 Percentage of areas aff
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Figure 12.8 Predominant types of la
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Threat to soil function Soil erosio
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Boddey, R.M., Alves, B.J.R, Jantali
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Gardi, C., Angelini, M., Barceló,
Page 437 and 438:
Nogueira, M.A., Albino, U.B., Brand
Page 439 and 440:
Spavorek, G., Bemdes, G., Barreto,
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13 | Regional Assessment of Soil Ch
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The Arab Centre for the Study of Ar
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Poverty within this system is exten
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Wind erosion A review conducted by
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13.3.5 | Soil salinization/sodifica
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13.3.9 | Compaction Soil compaction
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13.4 | Major soil threats in the re
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In Sudan, studies showed that in ar
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2002). There are few studies on the
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Consequences of salinization Salini
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Rates of C change are influenced no
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Figure 13.3 Layout of the project s
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13.5 | Case studies 13.5.1 | Case s
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Studies show that both climatic and
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2 - Land degradation assessment map
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Figure 13.9 Type of ecosystem servi
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Threat to soil function Soil erosio
Page 475 and 476:
References Abahussain, A.A., Abdu,
Page 477 and 478:
Badraoui, M. 1998. Effects of inten
Page 479 and 480:
FAO. 2004. Regional Workshop on Pro
Page 481 and 482:
Mamdouh Nasr. 1999. Assessing Deser
Page 483 and 484:
Yaghi, B. & Abdul-Wahab, S.A. 2004.
Page 485 and 486:
14.1 | Introduction Although Canada
Page 487 and 488:
The area of forested land in Canada
Page 489 and 490:
14.3 | Soil threats This section fo
Page 491 and 492:
Figure 14.2 Map of Superfund sites
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Figure 14.3 Areas in United States
Page 495 and 496:
The drivers for soil sealing in Can
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14.4.1 | Soil erosion Soil erosion
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The relationship between soil prope
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14.4.4 | Soil biodiversity Soil bio
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Figure 14.5 Risk of water erosion i
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Figure 14.7 Soil organic carbon cha
Page 507 and 508:
Figure 14.8 Residual soil N in Cana
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14.6 | Conclusions and recommendati
Page 511 and 512:
Compaction Sealing and land take Sa
Page 513 and 514:
Clearwater, R.L., Martin, T., Hoppe
Page 515 and 516:
Kurz, W.A., Dymond, C.C., White, T.
Page 517 and 518:
USDA. 2011. Resource Conservation A
Page 519 and 520:
15.1 | Introduction The Southwest P
Page 521 and 522:
of the country. The undulating and
Page 523 and 524:
The broad area of Near Oceania (inc
Page 525 and 526:
Country and land-use driver Implica
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15.5 | Threats to soils in the regi
Page 529 and 530:
egenerating soils. The South Island
Page 531 and 532:
New Zealand The importance of soil
Page 533 and 534:
Fertilizers Impurities in fertilize
Page 535 and 536:
The main onsite effects of acidific
Page 537 and 538:
Saltwater intrusion Saltwater intru
Page 539 and 540:
Phosphorus is naturally deficient a
Page 541 and 542:
Canterbury region. There has been a
Page 543 and 544:
Figure 15.3 (a) Trends in winter ra
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Figure 15.5 Agricultural lime sales
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The management of water is also fun
Page 549 and 550:
The DustWatch network Australia has
Page 551 and 552:
Soil sealing and capping Contaminat
Page 553 and 554:
Bui, E.N., Hancock, G.J. & Wilkinso
Page 555 and 556:
Hartemink, A.E. 1998b. Acidificatio
Page 557 and 558:
Moorehead, A. (ed.). 2011. Forests
Page 559 and 560:
Robertson, M.J., George, R.J., O’
Page 561 and 562:
Wilson, B.R. & Lonergan, V.E. 2013.
Page 563 and 564:
16.1 | Antarctic soils and environm
Page 565 and 566:
16.3 | Response All activities in A
Page 567 and 568:
IAATO. 2014. Tourism statistics. In
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Annex | Soil groups, characteristic
Page 571 and 572:
a Photo by C. Tarnocai b Photo by S
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Figure A 2 (a) An Anthrosol (Plagge
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a Photo by P. Charzyński Figure A
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a Photo by A. Filaretova b Photo by
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Figure A 5 (a) A Leptosol profile i
Page 581 and 582:
a Photo by L. Wilding b Photo by L.
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Figure A 7 (a) A Solonetz profile a
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a Photo by T. Toth b Photo by S. Kh
Page 587 and 588:
Figure A 9 (a) A Podzol profile and
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FERRALSOLS (OXISOLS) Ferralsols (Fi
Page 591 and 592:
NITISOLS (Alfisols, Ultisols, Incep
Page 593 and 594:
PLINTHOSOLS (Plinthic sub-groups) P
Page 595 and 596:
PLANOSOLS (Albaqualfs, Albaquults a
Page 597 and 598:
GLEYSOLS (Aquic suborder and Endoaq
Page 599 and 600:
STAGNOSOLS (Aquic Suborders and Epi
Page 601 and 602:
ANDOSOLS (ANDISOLS) Andosols (Figur
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5 | Soils with accumulation of orga
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KASTANOZEMS (Ustolls and Xerolls) K
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PHAEOZEMS (Udolls and Albolls) Phae
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UMBRISOLS (Umbric Great Group in Aq
Page 611 and 612:
6 | Soils with accumulation of mode
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CALCISOLS (Calcids, Argids, Cambids
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GYPSISOLS (Gypsids) Gypsisols are c
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7 | Soils with a clay-enriched subs
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ACRISOLS (Kan- great groups of Ulti
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LIXISOLS (Kan - great groups of Alf
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ALISOLS (Ultisols with an argillic
Page 625 and 626:
LUVISOLS (Alfisols with an argillic
Page 627 and 628:
8 | Soils with little or no profile
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REGOSOLS (Orthents) Regisols are th
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ARENOSOLS (Psamments) Arenosols are
Page 633 and 634:
FLUVISOLS (Fluvents, Fluv-Subroups)
Page 635 and 636:
9 | Permanently flooded soils WASSE
Page 637 and 638:
Kastanozems Histosols Gypsisols Gre
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Jones, A., Breuning-Madsen, H., Bro
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Glossary of technical terms Aerobic
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Topsoil: the upper part of a natura
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Broll, Gabrielle Bruulsma, Tom Bunn
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Leys, John Lobb, David Ma, Lin Maci
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Urquiaga Caballero, Segundo Urquiza
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