Su Weizhong, Ye Gaobin
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, 73 East Beijing Road, Nanjing 210008, China.
Int J Environ Res Public Health. 2014 May 26;11(6):5598-612. doi: 10.3390/ijerph110605598.
Since the 1980s a series of farmland policies have been implemented in China to stabilize the balance of farmland quantity and quality against accelerating urbanization and industrialization processes. This paper aims to reveal differences of soil fertility in the farmland occupation area (FOA) and farmland supplement area (FSA). In 1985-2000 the decline of the FOA area was 181,000 ha, but the FSA rarely increased. In 2000-2010 the decline of the FOA area was 824,800 ha, but the FSA increased dramatically. The accelerating loss process is closely related to urbanization and industrialization of the locations. Most occupied farmland was still located in the areas with higher soil fertility. The FOA in 1985-2000 had higher soil fertility than the FSA, but the FSA in 2000-2010 significantly raised its soil fertility to close to the FOAs' level. The rate of excellent-good levels of the FOA in 2000-2010 decreased from 46.13% to 37.61%; The development model shifts and farmland policies implementation are the chief driving factors behind AFOS changes. The TDBF policy and the main function zoning project should continue to play an effective role in balancing the farmland system.
自20世纪80年代以来,中国实施了一系列农田政策,以稳定农田数量和质量的平衡,应对城市化和工业化进程的加速。本文旨在揭示农田占用区(FOA)和农田补充区(FSA)土壤肥力的差异。1985 - 2000年,农田占用区面积减少了18.1万公顷,但农田补充区面积几乎没有增加。2000 - 2010年,农田占用区面积减少了82.48万公顷,但农田补充区面积大幅增加。这种加速流失的过程与当地的城市化和工业化密切相关。大部分被占用的农田仍位于土壤肥力较高的地区。1985 - 2000年的农田占用区土壤肥力高于农田补充区,但2000 - 2010年的农田补充区土壤肥力显著提高,接近农田占用区的水平。2000 - 2010年农田占用区优良等级比例从46.13%降至37.61%;发展模式转变和农田政策实施是农用地土壤质量变化的主要驱动因素。耕地占补平衡政策和主体功能区规划应继续在平衡农田系统中发挥有效作用。