Soil moisture plays an important role in land-atmosphere interactions. It is an important geophysical parameter in research on climate, hydrology, agriculture, and forestry. Soil moisture has important climatic effect...Soil moisture plays an important role in land-atmosphere interactions. It is an important geophysical parameter in research on climate, hydrology, agriculture, and forestry. Soil moisture has important climatic effects by influencing ground evapotranspi ration, runoff, surface reflectivity, surface emissivity, surface sensible heat and latent heat flux. At the global scale, the extent of its influence on the atmosphere is second only to that of sea surface temperature. At the terrestrial scale, its influence is even greater than that of sea surface temperatures. This paper presents a China Land Soil Moisture Data Assimilation System (CLSMDAS) based on EnKF and land process models, and results of the application of this system in the China Land Soil Moisture Data Assimilation tests. CLSMDAS is comprised of the following components: 1) A land process mo del—Community Land Model Version 3.0 (CLM3.0)—developed by the US National Center for Atmospheric Research (NCAR); 2) Precipitation of atmospheric forcing data and surface-incident solar radiation data come from hourly outputs of the FY2 geostationary meteorological satellite; 3) EnKF (Ensemble Kalman Filter) land data assimilation method; and 4) Observa tion data including satellite-inverted soil moisture outputs of the AMSR-E satellite and soil moisture observation data. Results of soil moisture assimilation tests from June to September 2006 were analyzed with CLSMDAS. Both simulation and assimila tion results of the land model reflected reasonably the temporal-spatial distribution of soil moisture. The assimilated soil mois ture distribution matches very well with severe summer droughts in Chongqing and Sichuan Province in August 2006, the worst since the foundation of the People’s Republic of China in 1949. It also matches drought regions that occurred in eastern Hubei and southern Guangxi in September.展开更多
高寒草甸是氮素匮乏的生态系统,氮添加和放牧都会显著改变土壤养分的有效性及高寒植物对养分的利用方式,从而影响群落生产力。为了认识氮沉降和放牧干扰对青藏高原高寒草甸的影响,在西藏当雄县高山嵩草草甸开展了氮添加及模拟放牧实验...高寒草甸是氮素匮乏的生态系统,氮添加和放牧都会显著改变土壤养分的有效性及高寒植物对养分的利用方式,从而影响群落生产力。为了认识氮沉降和放牧干扰对青藏高原高寒草甸的影响,在西藏当雄县高山嵩草草甸开展了氮添加及模拟放牧实验。在模拟放牧样地(G+N)和不放牧样地(NG+N)分别设置4个氮添加处理:0、10、20和40 kg N.hm-2.a-1,在生长季采用原位封顶埋管法测定净氮矿化速率,同时分析群落生物量分配与植物氮利用的相互关系。研究表明:氮添加与模拟放牧对植物的分配模式有不同的影响。在无放牧压力下,氮添加主要刺激植物地上部分的生长;在放牧压力下,氮添加更倾向于促进植物地下部分的生长。虽然剪草移走了15%～20%的地上生物量,但由于氮添加促进了植物的补偿生长,模拟放牧与不放牧处理的总生物量无显著差异,甚至前者高于后者。高寒草甸植物生物量分配对氮添加和模拟放牧的响应也体现在土壤供氮潜力的作用模式上,土壤净氮矿化速率在NG+N样地与植物地上生物量呈显著负相关,而在G+N样地与植物地下生物量呈显著负相关。这表明高寒草甸植物可以通过改变自身光合产物的分配模式来响应土壤养分状况和放牧干扰,在有效养分匮乏的高寒草甸添加氮素能够促进植物的补偿性生长。展开更多
Most research on micronutrients in maize has focused on maize grown as a monocrop. The aim of this study was to determine the effects of intercropping on the concentrations of micronutrients in maize grain and their a...Most research on micronutrients in maize has focused on maize grown as a monocrop. The aim of this study was to determine the effects of intercropping on the concentrations of micronutrients in maize grain and their acquisition via the shoot. We conducted field experiments to investigate the effects of intercropping with turnip (Brassica campestris L.), faba bean (Vicia faba L.), chickpea (Cicer arietinum L.), and soybean (Glycine max L.) on the iron (Fe), manganese (Mn), copper (Cu) and zinc (Zn) concentrations in the grain and their acquisition via the above-ground shoots of maize (Zea mays L.). Compared with monocropped maize grain, the grain of maize intercropped with legumes showed lower concentrations of Fe, Mn, Cu, and Zn and lower values of their corresponding harvest indexes. The micronutrient concentrations and harvest indexes in grain of maize intercropped with turnip were the same as those in monocropped maize grain. Intercropping stimulated the above-ground maize shoot acquisition of Fe, Mn, Cu and Zn, when averaged over different phosphorus (P) application rates. To our knowledge, this is the first report on the effects of intercropping on micronutrient concentrations in maize grain and on micronutrients acquisition via maize shoots (straw+grain). The maize grain Fe and Cu concentrations, but not Mn and Zn concentrations, were negatively correlated with maize grain yields. The concentrations of Fe, Mn, Cu, and Zn in maize grain were positively correlated with their corresponding harvest indexes. The decreased Fe, Mn, Cu, and Zn concentrations in grain of maize intercropped with legumes were attributed to reduced translocation of Fe, Mn, Cu, and Zn from vegetative tissues to grains. This may also be related to the delayed senescence of maize plants intercropped with legumes. We conclude that turnip/maize intercropping is beneficial to obtain high maize grain yield without decreased concentrations of Fe, Mn, Cu, and Zn in the grain. Further research is required to clarify the mechanisms underlying the展开更多
基金supported by National High Technology Research and Development Program of China (Grant Nos. 2007AA12Z144, 2009AA12Z129)Chinese COPES Project (Grant Nos. GYHY200706005, GYHY200806014)China Meteorological Administration New Technology Promotion Project (Grant No. CMATG2008Z04)
文摘Soil moisture plays an important role in land-atmosphere interactions. It is an important geophysical parameter in research on climate, hydrology, agriculture, and forestry. Soil moisture has important climatic effects by influencing ground evapotranspi ration, runoff, surface reflectivity, surface emissivity, surface sensible heat and latent heat flux. At the global scale, the extent of its influence on the atmosphere is second only to that of sea surface temperature. At the terrestrial scale, its influence is even greater than that of sea surface temperatures. This paper presents a China Land Soil Moisture Data Assimilation System (CLSMDAS) based on EnKF and land process models, and results of the application of this system in the China Land Soil Moisture Data Assimilation tests. CLSMDAS is comprised of the following components: 1) A land process mo del—Community Land Model Version 3.0 (CLM3.0)—developed by the US National Center for Atmospheric Research (NCAR); 2) Precipitation of atmospheric forcing data and surface-incident solar radiation data come from hourly outputs of the FY2 geostationary meteorological satellite; 3) EnKF (Ensemble Kalman Filter) land data assimilation method; and 4) Observa tion data including satellite-inverted soil moisture outputs of the AMSR-E satellite and soil moisture observation data. Results of soil moisture assimilation tests from June to September 2006 were analyzed with CLSMDAS. Both simulation and assimila tion results of the land model reflected reasonably the temporal-spatial distribution of soil moisture. The assimilated soil mois ture distribution matches very well with severe summer droughts in Chongqing and Sichuan Province in August 2006, the worst since the foundation of the People’s Republic of China in 1949. It also matches drought regions that occurred in eastern Hubei and southern Guangxi in September.
文摘高寒草甸是氮素匮乏的生态系统,氮添加和放牧都会显著改变土壤养分的有效性及高寒植物对养分的利用方式,从而影响群落生产力。为了认识氮沉降和放牧干扰对青藏高原高寒草甸的影响,在西藏当雄县高山嵩草草甸开展了氮添加及模拟放牧实验。在模拟放牧样地(G+N)和不放牧样地(NG+N)分别设置4个氮添加处理:0、10、20和40 kg N.hm-2.a-1,在生长季采用原位封顶埋管法测定净氮矿化速率,同时分析群落生物量分配与植物氮利用的相互关系。研究表明:氮添加与模拟放牧对植物的分配模式有不同的影响。在无放牧压力下,氮添加主要刺激植物地上部分的生长;在放牧压力下,氮添加更倾向于促进植物地下部分的生长。虽然剪草移走了15%～20%的地上生物量,但由于氮添加促进了植物的补偿生长,模拟放牧与不放牧处理的总生物量无显著差异,甚至前者高于后者。高寒草甸植物生物量分配对氮添加和模拟放牧的响应也体现在土壤供氮潜力的作用模式上,土壤净氮矿化速率在NG+N样地与植物地上生物量呈显著负相关,而在G+N样地与植物地下生物量呈显著负相关。这表明高寒草甸植物可以通过改变自身光合产物的分配模式来响应土壤养分状况和放牧干扰,在有效养分匮乏的高寒草甸添加氮素能够促进植物的补偿性生长。
基金supported by the National Natural Science Foundation of China (30890133)the National Basic Research Program of China (2011CB100405)China Agricultural University Specialized Research Fund to Support Ph.D. Candidates Innovative and Independent Scientific Subject(KYCX2010075)
文摘Most research on micronutrients in maize has focused on maize grown as a monocrop. The aim of this study was to determine the effects of intercropping on the concentrations of micronutrients in maize grain and their acquisition via the shoot. We conducted field experiments to investigate the effects of intercropping with turnip (Brassica campestris L.), faba bean (Vicia faba L.), chickpea (Cicer arietinum L.), and soybean (Glycine max L.) on the iron (Fe), manganese (Mn), copper (Cu) and zinc (Zn) concentrations in the grain and their acquisition via the above-ground shoots of maize (Zea mays L.). Compared with monocropped maize grain, the grain of maize intercropped with legumes showed lower concentrations of Fe, Mn, Cu, and Zn and lower values of their corresponding harvest indexes. The micronutrient concentrations and harvest indexes in grain of maize intercropped with turnip were the same as those in monocropped maize grain. Intercropping stimulated the above-ground maize shoot acquisition of Fe, Mn, Cu and Zn, when averaged over different phosphorus (P) application rates. To our knowledge, this is the first report on the effects of intercropping on micronutrient concentrations in maize grain and on micronutrients acquisition via maize shoots (straw+grain). The maize grain Fe and Cu concentrations, but not Mn and Zn concentrations, were negatively correlated with maize grain yields. The concentrations of Fe, Mn, Cu, and Zn in maize grain were positively correlated with their corresponding harvest indexes. The decreased Fe, Mn, Cu, and Zn concentrations in grain of maize intercropped with legumes were attributed to reduced translocation of Fe, Mn, Cu, and Zn from vegetative tissues to grains. This may also be related to the delayed senescence of maize plants intercropped with legumes. We conclude that turnip/maize intercropping is beneficial to obtain high maize grain yield without decreased concentrations of Fe, Mn, Cu, and Zn in the grain. Further research is required to clarify the mechanisms underlying the
