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Changes in some soil properties induced by re-conversion of cropland into grassland in the semiarid steppe zone of Inner Mongolia, China

AIMS: “Grain for Green Program” (GGP), i.e., re-conversion of cropland into forest or grassland, initiated by Chinese government has a profound impact on mitigating environmental degradation. The objectives of this study were to assess the changes of some soil properties during the processes of re-c...

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Published in:Plant and soil 2013-12, Vol.373 (1-2), p.89-106
Main Authors: Zhang, Zhi-Hua, Li, Xiao-Yan, Jiang, Zhi-Yun, Peng, Hai-Ying, Li, Liu, Zhao, Guo-Qin
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container_title Plant and soil
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Jiang, Zhi-Yun
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description AIMS: “Grain for Green Program” (GGP), i.e., re-conversion of cropland into forest or grassland, initiated by Chinese government has a profound impact on mitigating environmental degradation. The objectives of this study were to assess the changes of some soil properties during the processes of re-conversion from cropland to grassland over time in the semiarid steppe region of north China. METHODS: Two sites with different ages of re-conversion were selected for measurements of organic matter (SOM), total nitrogen (TN) and phosphorus (TP), bulk density (BD) and grain size distribution. Saturated hydraulic conductivity was determined by the constant hydraulic head method and unsaturated hydraulic conductivity by disc infiltrometer at tensions of 30, 60 and 150 mm. Soil water content was measured using the gravimetric method. Wetting front depths in the soil after rainfall were also recorded at the study sites. RESULTS: Natural grasslands had higher belowground biomass than re-converted grasslands. Re-converted grasslands had lower SOM and TN at depths of 0–20 cm and higher saturated hydraulic conductivity at depths of 0–10 cm than natural grassland. The natural grassland soils had higher soil water contents in the surface soil (0–20 cm) and lower soil water contents at deeper depths than re-converted grassland soils. Soil aggregate stability reached the natural steppe level 12 years after re-conversion. CONCLUSIONS: The recovery of soil properties after GGP appeared to be slow, and these properties did not return to natural grassland status before cultivation after 12 years of re-conversion.
doi_str_mv 10.1007/s11104-013-1772-3
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The objectives of this study were to assess the changes of some soil properties during the processes of re-conversion from cropland to grassland over time in the semiarid steppe region of north China. METHODS: Two sites with different ages of re-conversion were selected for measurements of organic matter (SOM), total nitrogen (TN) and phosphorus (TP), bulk density (BD) and grain size distribution. Saturated hydraulic conductivity was determined by the constant hydraulic head method and unsaturated hydraulic conductivity by disc infiltrometer at tensions of 30, 60 and 150 mm. Soil water content was measured using the gravimetric method. Wetting front depths in the soil after rainfall were also recorded at the study sites. RESULTS: Natural grasslands had higher belowground biomass than re-converted grasslands. Re-converted grasslands had lower SOM and TN at depths of 0–20 cm and higher saturated hydraulic conductivity at depths of 0–10 cm than natural grassland. The natural grassland soils had higher soil water contents in the surface soil (0–20 cm) and lower soil water contents at deeper depths than re-converted grassland soils. Soil aggregate stability reached the natural steppe level 12 years after re-conversion. CONCLUSIONS: The recovery of soil properties after GGP appeared to be slow, and these properties did not return to natural grassland status before cultivation after 12 years of re-conversion.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-013-1772-3</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Springer-Verlag</publisher><subject>aggregate stability ; Agricultural land ; Agricultural soils ; Agronomy. Soil science and plant productions ; Animal, plant and microbial ecology ; belowground biomass ; Biological and medical sciences ; Biomedical and Life Sciences ; bulk density ; ecological restoration ; Ecology ; Environmental aspects ; Environmental degradation ; Environmental restoration ; Farmlands ; forests ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Grassland soils ; Grasslands ; infiltrometers ; Land use ; land use change ; Life Sciences ; Moisture content ; Natural grasslands ; nitrogen content ; Organic matter ; Organic phosphorus ; particle size distribution ; phosphorus ; Physical properties ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; piezometers ; Piezometric head ; Plant Physiology ; Plant Sciences ; rain ; reforestation ; Regular Article ; saturated hydraulic conductivity ; semiarid soils ; semiarid zones ; Soil aggregates ; Soil depth ; Soil hydraulic properties ; Soil infiltration ; Soil management ; soil organic matter ; Soil properties ; Soil research ; Soil science ; Soil Science &amp; Conservation ; Soil sciences ; Soil stability ; Soil surfaces ; soil texture ; Soil water ; Soil water content ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. 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The objectives of this study were to assess the changes of some soil properties during the processes of re-conversion from cropland to grassland over time in the semiarid steppe region of north China. METHODS: Two sites with different ages of re-conversion were selected for measurements of organic matter (SOM), total nitrogen (TN) and phosphorus (TP), bulk density (BD) and grain size distribution. Saturated hydraulic conductivity was determined by the constant hydraulic head method and unsaturated hydraulic conductivity by disc infiltrometer at tensions of 30, 60 and 150 mm. Soil water content was measured using the gravimetric method. Wetting front depths in the soil after rainfall were also recorded at the study sites. RESULTS: Natural grasslands had higher belowground biomass than re-converted grasslands. Re-converted grasslands had lower SOM and TN at depths of 0–20 cm and higher saturated hydraulic conductivity at depths of 0–10 cm than natural grassland. The natural grassland soils had higher soil water contents in the surface soil (0–20 cm) and lower soil water contents at deeper depths than re-converted grassland soils. Soil aggregate stability reached the natural steppe level 12 years after re-conversion. CONCLUSIONS: The recovery of soil properties after GGP appeared to be slow, and these properties did not return to natural grassland status before cultivation after 12 years of re-conversion.</description><subject>aggregate stability</subject><subject>Agricultural land</subject><subject>Agricultural soils</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Animal, plant and microbial ecology</subject><subject>belowground biomass</subject><subject>Biological and medical sciences</subject><subject>Biomedical and Life Sciences</subject><subject>bulk density</subject><subject>ecological restoration</subject><subject>Ecology</subject><subject>Environmental aspects</subject><subject>Environmental degradation</subject><subject>Environmental restoration</subject><subject>Farmlands</subject><subject>forests</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Grassland soils</subject><subject>Grasslands</subject><subject>infiltrometers</subject><subject>Land use</subject><subject>land use change</subject><subject>Life Sciences</subject><subject>Moisture content</subject><subject>Natural grasslands</subject><subject>nitrogen content</subject><subject>Organic matter</subject><subject>Organic phosphorus</subject><subject>particle size distribution</subject><subject>phosphorus</subject><subject>Physical properties</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>piezometers</subject><subject>Piezometric head</subject><subject>Plant Physiology</subject><subject>Plant Sciences</subject><subject>rain</subject><subject>reforestation</subject><subject>Regular Article</subject><subject>saturated hydraulic conductivity</subject><subject>semiarid soils</subject><subject>semiarid zones</subject><subject>Soil aggregates</subject><subject>Soil depth</subject><subject>Soil hydraulic properties</subject><subject>Soil infiltration</subject><subject>Soil management</subject><subject>soil organic matter</subject><subject>Soil properties</subject><subject>Soil research</subject><subject>Soil science</subject><subject>Soil Science &amp; Conservation</subject><subject>Soil sciences</subject><subject>Soil stability</subject><subject>Soil surfaces</subject><subject>soil texture</subject><subject>Soil water</subject><subject>Soil water content</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. 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Soil science and plant productions</topic><topic>Animal, plant and microbial ecology</topic><topic>belowground biomass</topic><topic>Biological and medical sciences</topic><topic>Biomedical and Life Sciences</topic><topic>bulk density</topic><topic>ecological restoration</topic><topic>Ecology</topic><topic>Environmental aspects</topic><topic>Environmental degradation</topic><topic>Environmental restoration</topic><topic>Farmlands</topic><topic>forests</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. 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Soil fertility</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>Steppe soils</topic><topic>Steppes</topic><topic>unsaturated hydraulic conductivity</topic><topic>Water and solute dynamics</topic><topic>Water content</topic><topic>wetting front</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhang, Zhi-Hua</creatorcontrib><creatorcontrib>Li, Xiao-Yan</creatorcontrib><creatorcontrib>Jiang, Zhi-Yun</creatorcontrib><creatorcontrib>Peng, Hai-Ying</creatorcontrib><creatorcontrib>Li, Liu</creatorcontrib><creatorcontrib>Zhao, Guo-Qin</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection (Proquest) (PQ_SDU_P3)</collection><collection>ProQuest Biological Science Collection</collection><collection>Agriculture Science Database</collection><collection>ProQuest Biological Science Journals</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhang, Zhi-Hua</au><au>Li, Xiao-Yan</au><au>Jiang, Zhi-Yun</au><au>Peng, Hai-Ying</au><au>Li, Liu</au><au>Zhao, Guo-Qin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in some soil properties induced by re-conversion of cropland into grassland in the semiarid steppe zone of Inner Mongolia, China</atitle><jtitle>Plant and soil</jtitle><stitle>Plant Soil</stitle><date>2013-12-01</date><risdate>2013</risdate><volume>373</volume><issue>1-2</issue><spage>89</spage><epage>106</epage><pages>89-106</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>AIMS: “Grain for Green Program” (GGP), i.e., re-conversion of cropland into forest or grassland, initiated by Chinese government has a profound impact on mitigating environmental degradation. The objectives of this study were to assess the changes of some soil properties during the processes of re-conversion from cropland to grassland over time in the semiarid steppe region of north China. METHODS: Two sites with different ages of re-conversion were selected for measurements of organic matter (SOM), total nitrogen (TN) and phosphorus (TP), bulk density (BD) and grain size distribution. Saturated hydraulic conductivity was determined by the constant hydraulic head method and unsaturated hydraulic conductivity by disc infiltrometer at tensions of 30, 60 and 150 mm. Soil water content was measured using the gravimetric method. Wetting front depths in the soil after rainfall were also recorded at the study sites. RESULTS: Natural grasslands had higher belowground biomass than re-converted grasslands. Re-converted grasslands had lower SOM and TN at depths of 0–20 cm and higher saturated hydraulic conductivity at depths of 0–10 cm than natural grassland. The natural grassland soils had higher soil water contents in the surface soil (0–20 cm) and lower soil water contents at deeper depths than re-converted grassland soils. Soil aggregate stability reached the natural steppe level 12 years after re-conversion. CONCLUSIONS: The recovery of soil properties after GGP appeared to be slow, and these properties did not return to natural grassland status before cultivation after 12 years of re-conversion.</abstract><cop>Dordrecht</cop><pub>Springer-Verlag</pub><doi>10.1007/s11104-013-1772-3</doi><tpages>18</tpages></addata></record>
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ispartof Plant and soil, 2013-12, Vol.373 (1-2), p.89-106
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subjects aggregate stability
Agricultural land
Agricultural soils
Agronomy. Soil science and plant productions
Animal, plant and microbial ecology
belowground biomass
Biological and medical sciences
Biomedical and Life Sciences
bulk density
ecological restoration
Ecology
Environmental aspects
Environmental degradation
Environmental restoration
Farmlands
forests
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
Grassland soils
Grasslands
infiltrometers
Land use
land use change
Life Sciences
Moisture content
Natural grasslands
nitrogen content
Organic matter
Organic phosphorus
particle size distribution
phosphorus
Physical properties
Physics, chemistry, biochemistry and biology of agricultural and forest soils
piezometers
Piezometric head
Plant Physiology
Plant Sciences
rain
reforestation
Regular Article
saturated hydraulic conductivity
semiarid soils
semiarid zones
Soil aggregates
Soil depth
Soil hydraulic properties
Soil infiltration
Soil management
soil organic matter
Soil properties
Soil research
Soil science
Soil Science & Conservation
Soil sciences
Soil stability
Soil surfaces
soil texture
Soil water
Soil water content
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Steppe soils
Steppes
unsaturated hydraulic conductivity
Water and solute dynamics
Water content
wetting front
title Changes in some soil properties induced by re-conversion of cropland into grassland in the semiarid steppe zone of Inner Mongolia, China
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