Major limitations to achieving "4 per 1000" increases in soil organic carbon stock in temperate regions: Evidence from long-term experiments at Rothamsted Research, United Kingdom

被引:265
作者
Poulton, Paul [1 ]
Johnston, Johnny [1 ]
Macdonald, Andy [1 ]
White, Rodger [2 ]
Powlson, David [1 ]
机构
[1] Rothamsted Res, Dept Sustainable Agr Sci, Harpenden, Herts, England
[2] Rothamsted Res, Dept Computat & Analyt Sci, Harpenden, Herts, England
基金
英国生物技术与生命科学研究理事会;
关键词
4; per; 1000; carbon sequestration; climate change mitigation; long-term experiments; management practices; organic amendments; Rothamsted; soil organic carbon; BROADBALK WHEAT EXPERIMENT; GREENHOUSE-GAS MITIGATION; CLIMATE-CHANGE MITIGATION; CONSERVATION AGRICULTURE; PART; SEQUESTRATION; MANAGEMENT; FERTILIZER; NITROGEN; MATTER;
D O I
10.1111/gcb.14066
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
We evaluated the "4 per 1000" initiative for increasing soil organic carbon (SOC) by analysing rates of SOC increase in treatments in 16 long-term experiments in southeast United Kingdom. The initiative sets a goal for SOC stock to increase by 4 parts per thousand per year in the 0-40 cm soil depth, continued over 20 years. Our experiments, on three soil types, provided 114 treatment comparisons over 7-157 years. Treatments included organic additions (incorporated by inversion ploughing), N fertilizers, introducing pasture leys into continuous arable systems, and converting arable land to woodland. In 65% of cases, SOC increases occurred at > 7 parts per thousand per year in the 0-23 cm depth, approximately equivalent to 4 parts per thousand per year in the 0-40 cm depth. In the two longest running experiments (>150 years), annual farmyard manure (FYM) applications at 35 t fresh material per hectare (equivalent to approx. 3.2 t organic C/ha/year) gave SOC increases of 18 parts per thousand and 43 parts per thousand per year in the 23 cm depth during the first 20 years. Increases exceeding 7 parts per thousand per year continued for 40-60 years. In other experiments, with FYM applied at lower rates or not every year, there were increases of 3 parts per thousand-8 parts per thousand per year over several decades. Other treatments gave increases between zero and 19 parts per thousand per year over various periods. We conclude that there are severe limitations to achieving the "4 per 1000" goal in practical agriculture over large areas. The reasons include (1) farmers not having the necessary resources (e.g. insufficient manure); (2) some, though not all, practices favouring SOC already widely adopted; (3) practices uneconomic for farmers-potentially overcome by changes in regulations or subsidies; (4) practices undesirable for global food security. We suggest it is more realistic to promote practices for increasing SOC based on improving soil quality and functioning as small increases can have disproportionately large beneficial impacts, though not necessarily translating into increased crop yield.
引用
收藏
页码:2563 / 2584
页数:22
相关论文
共 81 条
[21]   The effects of long-term applications of inorganic nitrogen fertilizer on soil nitrogen in the Broadbalk wheat experiment [J].
Glendining, MJ ;
Powlson, DS ;
Poulton, PR ;
Bradbury, NJ ;
Palazzo, D ;
Li, X .
JOURNAL OF AGRICULTURAL SCIENCE, 1996, 127 :347-363
[22]   Predicting Agricultural Management Influence on Long-Term Soil Organic Carbon Dynamics: Implications for Biofuel Production [J].
Gollany, H. T. ;
Rickman, R. W. ;
Liang, Y. ;
Albrecht, S. L. ;
Machado, S. ;
Kang, S. .
AGRONOMY JOURNAL, 2011, 103 (01) :234-246
[23]   Nitrate leaching from the Broadbalk Wheat Experiment, Rothamsted, UK, as influenced by fertilizer and manure inputs and the weather [J].
Goulding, KWT ;
Poulton, PR ;
Webster, CP ;
Howe, MT .
SOIL USE AND MANAGEMENT, 2000, 16 (04) :244-250
[24]   Changes in soil organic carbon in croplands subjected to fertilizer management: a global meta-analysis [J].
Han, Pengfei ;
Zhang, Wen ;
Wang, Guocheng ;
Sun, Wenjuan ;
Huang, Yao .
SCIENTIFIC REPORTS, 2016, 6
[25]   INFLUENCE OF MIXED CROPPING ROTATIONS (PASTURE ARABLE) ON ORGANIC-MATTER CONTENT, WATER STABLE AGGREGATION AND CLOD POROSITY IN A GROUP OF SOILS [J].
HAYNES, RJ ;
SWIFT, RS ;
STEPHEN, RC .
SOIL & TILLAGE RESEARCH, 1991, 19 (01) :77-87
[26]   Development of an indicator for risk of phosphorus leaching [J].
Hesketh, N ;
Brookes, PC .
JOURNAL OF ENVIRONMENTAL QUALITY, 2000, 29 (01) :105-110
[27]   Do organic inputs matter - a meta-analysis of additional yield effects for arable crops in Europe [J].
Hijbeek, R. ;
van Ittersum, M. K. ;
ten Berge, H. F. M. ;
Gort, G. ;
Spiegel, H. ;
Whitmore, A. P. .
PLANT AND SOIL, 2017, 411 (1-2) :293-303
[28]   SIMULATION BY NCSOIL OF NET MINERALIZATION IN SOILS FROM THE DEHERAIN AND 36 PARCELLES FIELDS AT GRIGNON [J].
HOUOT, S ;
MOLINA, JAE ;
CHAUSSOD, R ;
CLAPP, CE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1989, 53 (02) :451-455
[29]   Beyond carbon sequestration: soil as conduit of solar energy [J].
Janzen, H. H. .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2015, 66 (01) :19-32
[30]   The turnover of organic carbon in subsoils. Part 1. Natural and bomb radiocarbon in soil profiles from the Rothamsted long-term field experiments [J].
Jenkinson, D. S. ;
Poulton, P. R. ;
Bryant, C. .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2008, 59 (02) :391-U13