Du Guo-ming, Pan Tao, Yin Zhe-rui, Dong Jin-wei
Ying Yong Sheng Tai Xue Bao. 2015 Jan;26(1):207-14.
On the background of global climate change, agriculture in North China has been experiencing substantial modifications to adapt to the ongoing regional warming. One of the most significant land use change is the conversation from upland cropland to paddy cropland, which is characterized by the dramatic changes of agricultural landscape pattern. In this study, we generated land use maps in Fujin City in 2000 and 2013 by using Landsat TM imagery, and analyzed the landscape pattern changes (cropland composite, special distribution, and patch characteristics, etc.) of croplands by using landscape indices and empirical approach. The results indicated a rapid cropland increase from 512400 hm2(reclamation ratio 60.4%) in 2000 to 699300 hm2(reclamation 82.4%) in 2013, especially, the paddy cropland proportion in the total cropland increased from 6.7% to more than half (54.1%) , that is, the agricultural land use mode had changed from the initial stage of paddy agriculture to the intermediate stage. The reclamation area and common agricultural area showed different paddy agriculture development characteristics: in 2000, the paddy field ratios in the common agricultural area and reclamation area were similar (5.5% and 8.3% respectively); however, in 2013, the paddy field ratio in the common agricultural area (33.6%) was significantly lower than that in reclamation area (83.4%). In 2000, the total number of cropland patches was 2311 in the study, including 1010 patches from the common agricultural area and 1301 patches from the reclamation area. The coefficient of variation (CV) , and shape index (SI) of cropland patches in upland cropland were always higher than in paddy cropland. Upland cropland had larger mean patch size with the plaque area index above 60% and higher connectivity. The patch density of upland cropland was lower than that of paddy cropland. In the conversions to the intermediate and later stages of paddy agriculture, the patch number of cropland increased rapidly with different rates in upland and paddy croplands. The CV of paddy cropland patches increased while fluctuated in upland cropland. The SI of paddy cropland increased first and then decreased, while that of upland cropland decreased continuously. The mean patch sizes of paddy and upland croplands increased and decreased respectively. The patch density increased in upland cropland while decreased in paddy cropland. The connectivity of upland cropland decreased while that of paddy cropland increased. The staggered degree of both cropland types was enhanced from 2000 to 2013. In general, the paddy agriculture was becoming the dominated agricultural land use mode in the study area while the convesions had different rates in two administrative regions (reclamation and common agricultural areas).
在全球气候变化的背景下,中国北方的农业一直在经历重大变革以适应区域气候持续变暖。最显著的土地利用变化之一是从旱地农田向水田农田的转变,其特点是农业景观格局发生了巨大变化。在本研究中,我们利用Landsat TM影像生成了2000年和2013年抚远市的土地利用图,并采用景观指数和实证方法分析了农田的景观格局变化(农田综合情况、空间分布和斑块特征等)。结果表明,农田面积从2000年的512400公顷(开垦率60.4%)迅速增加到2013年的699300公顷(开垦率82.4%),特别是水田在总农田中的比例从6.7%增加到一半以上(54.1%),即农业土地利用模式已从水田农业的初始阶段转变为中期阶段。开垦区和普通农业区呈现出不同的水田农业发展特征:2000年,普通农业区和开垦区的水田比例相似(分别为5.5%和8.3%);然而,2013年,普通农业区的水田比例(33.6%)显著低于开垦区(83.4%)。2000年,研究区农田斑块总数为2311个,其中普通农业区1010个斑块,开垦区1301个斑块。旱地农田斑块的变异系数(CV)和形状指数(SI)始终高于水田。旱地平均斑块面积较大,斑块面积指数高于60%,连通性较高。旱地的斑块密度低于水田。在向水田农业的中期和后期转变过程中,旱地和水田的农田斑块数量以不同速率迅速增加。水田斑块的CV增加,而旱地则波动。水田的SI先增加后减少,而旱地则持续下降。水田和旱地的平均斑块面积分别增加和减少。旱地的斑块密度增加,而水田的斑块密度减少。旱地的连通性降低,而水田的连通性增加。从2000年到2013年,两种农田类型的交错程度都有所增强。总体而言,水田农业正成为研究区主要的农业土地利用模式,而两个行政区(开垦区和普通农业区)的转变速率不同。