To analyze the bacterial communities in lime concretion black soil upon the incorporation of crop residues for two years in wheat-maize system, total DNA was directly extracted and PCR-amplified with the F357GC and R5...To analyze the bacterial communities in lime concretion black soil upon the incorporation of crop residues for two years in wheat-maize system, total DNA was directly extracted and PCR-amplified with the F357GC and R518 primers targeting the 16S rRNA genes of V3 region. The amplified fragments were analyzed by perpendicular DGGE. Analyzing of species richness index S and Shannon diversity index H revealed that there was a high diversity of soil bacterial community compositions among all treatments after incorporation of crop residues and fertilizing under field conditions. Eleven DGGE bands recovered were re-amplified, sequenced. Phylogenetic analysis of the representative DGGE fingerprints identified four groups of the prokaryotic communities in the soil by returning wheat residues and fertilizing under field conditions. The bacterial communities belonged to gamma proteobacterium, Cupriavidus sp, halophilic eubacterium, Acidobacterium sp, Sorangium sp, delta proteobacterium, Streptococcus sp and Streptococcus agalactiae were main bacterial communities. Principal Component Analysis (PCA) showed that there were the differences in DNA profiles among the six treatments. It showed that wheat residue returning, maize residue returning and fertilizing all can improve bacterial diversity in varying degrees. As far as improvement of bacterial diversity was concerned, wheat residue returning was higher than fertilizing, and fertilizing higher than maize residue returning.展开更多
When the soil condition and depth to water table stay constant, climate condition will then be the only determinant of evaporation intensity of phreatic water from bare soil. Based on a series of long-term quality-con...When the soil condition and depth to water table stay constant, climate condition will then be the only determinant of evaporation intensity of phreatic water from bare soil. Based on a series of long-term quality-controlled data collected at the Wudaogou Hydrological Experiment Station in the Huaibei Plain, Anhui, China, the variation trends of the evaporation rate of phreatic water from bare soil were studied through the Mann-Kendall trend test and the linear regression trend test, followed by the study on the responses of evaporation to climate change. Results indicated that in the Huaibei Plain during 1991-2008, evaporation of phreatic water from bare soil tended to increase at a rate of 5% on monthly scale in March, June and July while in other months the increase was minor. On the seasonal basis, the evaporation saw significant increase in spring and summer. In addition, annual evaporation tended to grow evidently over time. When air temperature rises by 1 °C, the annual evaporation rate increases by 7.24–14.21%, while when the vapor pressure deficit rises by 10%, it changes from-0.09 to 5.40%. The study also provides references for further understanding of the trends and responses of regional evapotranspiration to climate change.展开更多
通过安徽省蒙城县砂姜黑土上连续4a的冬小麦-夏玉米连作长期定位试验,研究了秸秆还田配合施用不同量氮肥对土壤理化性质及作物产量的影响。结果表明,秸秆还田可降低土壤容重2.5%—9.2%,提高含水量8.2%—28.5%和表层土壤贮水量4.1%—19....通过安徽省蒙城县砂姜黑土上连续4a的冬小麦-夏玉米连作长期定位试验,研究了秸秆还田配合施用不同量氮肥对土壤理化性质及作物产量的影响。结果表明,秸秆还田可降低土壤容重2.5%—9.2%,提高含水量8.2%—28.5%和表层土壤贮水量4.1%—19.9%;增加土壤总孔隙度1.1%—8.9%、毛管孔隙度18.9%—41.0%,非毛管孔隙度降低6.4%—38.8%,土壤毛管孔隙度占土壤总孔隙度的比例增加。秸秆还田所有处理耕层的土壤硝态氮含量高于秸秆移除处理,施氮540、630、720 kg N hm-2a-1时,秸秆还田处理的硝态氮含量显著高于秸秆移除,而铵态氮含量无明显变化规律。无论秸秆还田还是秸秆移除,耕层土壤的硝态氮含量随氮肥用量的增加呈指数趋势增加,硝态氮含量与施氮量的相关性秸秆移除处理高于秸秆还田处理;秸秆还田处理的铵态氮含量随施氮量增加成指数趋势增加,而秸秆移除处理呈指数趋势减小,相关性均不显著。秸秆还田条件下,小麦和玉米获得高产的年氮肥用量分别为630、696 kg N hm-2a-1,秸秆移除为579、627 kg N hm-2a-1。经作用力分析,秸秆还田是影响土壤物理性质的最重要因素,作物产量受秸秆还田和施氮量的影响,但氮肥水平大于秸秆还田。展开更多
文摘To analyze the bacterial communities in lime concretion black soil upon the incorporation of crop residues for two years in wheat-maize system, total DNA was directly extracted and PCR-amplified with the F357GC and R518 primers targeting the 16S rRNA genes of V3 region. The amplified fragments were analyzed by perpendicular DGGE. Analyzing of species richness index S and Shannon diversity index H revealed that there was a high diversity of soil bacterial community compositions among all treatments after incorporation of crop residues and fertilizing under field conditions. Eleven DGGE bands recovered were re-amplified, sequenced. Phylogenetic analysis of the representative DGGE fingerprints identified four groups of the prokaryotic communities in the soil by returning wheat residues and fertilizing under field conditions. The bacterial communities belonged to gamma proteobacterium, Cupriavidus sp, halophilic eubacterium, Acidobacterium sp, Sorangium sp, delta proteobacterium, Streptococcus sp and Streptococcus agalactiae were main bacterial communities. Principal Component Analysis (PCA) showed that there were the differences in DNA profiles among the six treatments. It showed that wheat residue returning, maize residue returning and fertilizing all can improve bacterial diversity in varying degrees. As far as improvement of bacterial diversity was concerned, wheat residue returning was higher than fertilizing, and fertilizing higher than maize residue returning.
基金financially supported by“the Fundamental Research Funds for the Central Universities”of Hefei University of Technology(No.JZ2014HGBZ0040)the National Natural Science Foundation of China(No.51509064+2 种基金No.51309071No.51309155)the National Key Research and Development Programs of China(Grand 2016YFA0601601,2016YFA0601501)
文摘When the soil condition and depth to water table stay constant, climate condition will then be the only determinant of evaporation intensity of phreatic water from bare soil. Based on a series of long-term quality-controlled data collected at the Wudaogou Hydrological Experiment Station in the Huaibei Plain, Anhui, China, the variation trends of the evaporation rate of phreatic water from bare soil were studied through the Mann-Kendall trend test and the linear regression trend test, followed by the study on the responses of evaporation to climate change. Results indicated that in the Huaibei Plain during 1991-2008, evaporation of phreatic water from bare soil tended to increase at a rate of 5% on monthly scale in March, June and July while in other months the increase was minor. On the seasonal basis, the evaporation saw significant increase in spring and summer. In addition, annual evaporation tended to grow evidently over time. When air temperature rises by 1 °C, the annual evaporation rate increases by 7.24–14.21%, while when the vapor pressure deficit rises by 10%, it changes from-0.09 to 5.40%. The study also provides references for further understanding of the trends and responses of regional evapotranspiration to climate change.
文摘通过安徽省蒙城县砂姜黑土上连续4a的冬小麦-夏玉米连作长期定位试验,研究了秸秆还田配合施用不同量氮肥对土壤理化性质及作物产量的影响。结果表明,秸秆还田可降低土壤容重2.5%—9.2%,提高含水量8.2%—28.5%和表层土壤贮水量4.1%—19.9%;增加土壤总孔隙度1.1%—8.9%、毛管孔隙度18.9%—41.0%,非毛管孔隙度降低6.4%—38.8%,土壤毛管孔隙度占土壤总孔隙度的比例增加。秸秆还田所有处理耕层的土壤硝态氮含量高于秸秆移除处理,施氮540、630、720 kg N hm-2a-1时,秸秆还田处理的硝态氮含量显著高于秸秆移除,而铵态氮含量无明显变化规律。无论秸秆还田还是秸秆移除,耕层土壤的硝态氮含量随氮肥用量的增加呈指数趋势增加,硝态氮含量与施氮量的相关性秸秆移除处理高于秸秆还田处理;秸秆还田处理的铵态氮含量随施氮量增加成指数趋势增加,而秸秆移除处理呈指数趋势减小,相关性均不显著。秸秆还田条件下,小麦和玉米获得高产的年氮肥用量分别为630、696 kg N hm-2a-1,秸秆移除为579、627 kg N hm-2a-1。经作用力分析,秸秆还田是影响土壤物理性质的最重要因素,作物产量受秸秆还田和施氮量的影响,但氮肥水平大于秸秆还田。
