Distributions of soil phosphorus in China’s densely populated village landscapes
- 168 Downloads
Village landscapes, which integrate small-scale agriculture with housing, forestry and a host of other land use practices, cover more than 2 × 106 km2 across China. Village lands tend to be managed at very fine spatial scales (≤30 m), with managers altering soil fertility and even terrain by terracing, irrigation, fertilizing, and other land use practices. Under these conditions, accumulation of excess phosphorous in soils has become important contributor to eutrophication of surface waters across China’s densely populated village landscapes. The aim of this study was to investigate relationships between fine-scale patterns of agricultural management and soil total phosphorus (STP) within China’s village landscapes.
Materials and methods
First, China’s village landscapes were divided into five environmentally distinct regions across China. Within each region, a single 100 km2 research site was then selected, and 12 500 × 500 m square landscape sample cells were selected for fine-scale mapping. Soils were sampled within fine-scale landscape features using a regionally weighted landscape sampling design.
Results and discussion
STP stock across the 0.9 × 106 km2 area of our five village regions was approximately 0.14 Pg (1 Pg = 1015 g), with STP densities ranging from 0.08 kg m−2 in Tropical Hilly Region to 0.22 kg m−2 in North China Plain and Yangtze Plain, with village landscape STP density varying significantly with precipitation and temperature. Outside the Tropical Hilly Region, STP densities also varied significantly with land form, use, and cover. As expected, the highest STP densities were found in agricultural lands and in areas near buildings, while the lowest were in nonproductive lands and forestry lands. As a combined result of these high STP densities and the predominance of agricultural land use, most village STP stock was found in agricultural lands. A surprisingly large portion of village STP stock was associated with built structures and disturbed lands surrounding them (15.0% in North China Plain, 19.3% in Yangtze Plain, 5.9% in Sichuan Hilly Region, 7.8% in Subtropical Hilly Region, 2.7% in Tropical Hilly Region), which had a significant relationship with population density.
Our results demonstrated that local patterns of land management and human residence were associated with substantial differences in STP both within and across China’s village landscapes which have increased their potential contribution to P pollution. With the rapid change in land use/land cover in China’s densely populated landscapes, such information is essential for rational planning of future management to reach agricultural sustainability.
KeywordsChina Land cover Land form Land use Pollution Soil phosphorus Village landscapes
Funding support came from the US National Science Foundation (DEB-0075617) awarded to Erle C. Ellis in 2000. Work in China was conducted in collaboration with Prof. Lin Zhang Yang of the Institute of Soil Science, Chinese Academy of Sciences (CAS), Nanjing, China, Prof. Hua Ouyang of the Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, China and Prof. Xu Cheng of China Agricultural University, Beijing, China. We are grateful to our local collaborators for field assistance and anonymous reviewers for helpful comments on the manuscript. Any opinions, findings, conclusions, or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation.
- Burgess RL, Sharper DM (1981) Forest island dynamics in man-dominated landscape. Springer, New YorkGoogle Scholar
- China Agricultural University (1998) Agricultural chemistry. Agricultural Press, Beijing, pp 115–123 in ChineseGoogle Scholar
- Ellis EC (2004) Long-term ecological changes in the densely populated rural landscapes of China. In: DeFries RS, Asner GP, Houghton RA (eds) Ecosystems and land use change. American Geophysical Union, Washington, DC, pp 303–320Google Scholar
- Forman RTT, Gordorn M (1986) Landscape ecology. Wiley, New YorkGoogle Scholar
- Jiang Y, Zhang YG, Liang WJ, Men FX, Liu YJ (2005) Effects of land use on the profile distribution of phosphorus in Aquic Brown soil. J Agro-Enviro Sci 24(3):512–516 in ChineseGoogle Scholar
- Jiao JG, Wu JX, Yang LZ, Li HX, Ellis EC (2006) Effects of land use on soil total nitrogen and phosphorus in different densely populated village landscapes. J Soil Water Conserv 20(3):97–101 in ChineseGoogle Scholar
- Lu P, Peng PQ, Song BL, Tang GY, Zou Y, Huang DY, Xiao HA, Su YR (2005) Geostatistical and GIS analyses on soil total P in the typical area of Dongting lake plain. Scientia Agricultura Sinica 38(6):1204–1212 in ChineseGoogle Scholar
- Olsen SR, Sommers LE (1982) Phosphorus. In: Page AL, Miller RH, Keeney DR (eds) Methods of soil analysis part 2. Chemical and microbiological properties. American Society of Agronomy: Soil Science Society of America, Madison, Wisconsin, pp 406–407Google Scholar
- Onthong J, Osaki M, Nilnond C, Tadano T (1999) Phosphorus status of some highly weathered soils in peninsular Thailand and availability in relation to citrate and oxalate application. Soil Sci Plant Nutr 45(3):627–637Google Scholar
- Sharpley AN, Rekolainen S (1997) Phosphorus in agriculture and its environmental implications. In: Tunney H, Carton OT, Brookes PC, Johnston AE (eds) Phosphorus loss from soil to water. C.A.B. International, Wallingford, pp 1–54Google Scholar
- Shen SM, Yu WT, Zhang L, Lian HZ (1993) Internal and external nutrient cycling of poplar tree II. Transferring and cycling of nutrients in and out of the tree before and after leaf fallen. Chinese J Appl Ecol 4(1):27–31 in ChineseGoogle Scholar
- Tang JD, Ye XY, Rao GL, Lin BS (2003) Effect of human activities on quality of cultivated land in Guangdong province. Soil 1:8–12 (in Chinese)Google Scholar
- Wollast R (1993) Interactions of C, N, P and S biogeochemical cycles global change. Springer, BerlinGoogle Scholar
- Xiao PF, Zhang SR, Huang LQ, Gan WZ, Wu DY (2005) Temporal–spatial variability of soil available phosphorus in Chengdu plain. J Soil Water Conserv 19(4):89–93 in ChineseGoogle Scholar
- Zhang Y, Zhang H, Peng BZ, Yang H (2003) Soil erosion and nutrient loss of various land use patterns. Bull Soil Water Conserv 23(1):23–27 in ChineseGoogle Scholar