Remotely detecting canopy nitrogen concentration and uptake of paddy rice in the Northeast China Plain

2013 ◽  
Vol 78 ◽  
pp. 102-115 ◽  
Author(s):  
Kang Yu ◽  
Fei Li ◽  
Martin L. Gnyp ◽  
Yuxin Miao ◽  
Georg Bareth ◽  
...  
2015 ◽  
Vol 10 (1) ◽  
pp. 49-62 ◽  
Author(s):  
Cui Jin ◽  
Xiangming Xiao ◽  
Jinwei Dong ◽  
Yuanwei Qin ◽  
Zongming Wang

Author(s):  
Marie-Louise Smith ◽  
David Y. Hollinger ◽  
Scott Ollinger

2012 ◽  
Vol 4 (6) ◽  
pp. 1651-1670 ◽  
Author(s):  
Poonsak Miphokasap ◽  
Kiyoshi Honda ◽  
Chaichoke Vaiphasa ◽  
Marc Souris ◽  
Masahiko Nagai

HortScience ◽  
2001 ◽  
Vol 36 (7) ◽  
pp. 1252-1259 ◽  
Author(s):  
A. Bar-Tal ◽  
B. Aloni ◽  
L. Karni ◽  
R. Rosenberg

The objective of this research was to study the effects of N concentration and N-NO3: N-NH4 ratio in the nutrient solution on growth, transpiration, and nutrient uptake of greenhouse-grown pepper in a Mediterranean climate. The experiment included five total N levels (0.25 to 14 mmol·L-1, with a constant N-NO3: N-NH4 ratio of 4) and five treatments of different N-NO3: N-NH4 ratios (0.25 to 4, with a constant N concentration of 7 mmol·L-1). Plants were grown in an aero-hydroponic system in a climate-controlled greenhouse. The optimum N concentrations for maximum stem and leaf dry matter (DM) production were in the range of 8.0 to 9.2 mmol·L-1. The optimum N-NO3: N-NH4 ratio for maximal stem DM production was 3.5. The optimum value of N concentration for total fruit DM production was 9.4 mmol·L-1. Fruit DM production increased linearly with increasing N-NO3: N-NH4 ratio in the range studied. The N concentration, but not N source, affected leaf chlorophyll content. Shorter plants with more compacted canopies were obtained as the N-NO3: N-NH4 ratio decreased. The effect of N concentration on transpiration was related to its effect on leaf weight and area, whereas the effect of a decreasing N-NO3: N-NH4 ratio in reducing transpiration probably resulted from the compacted canopy. Nitrogen uptake increased as the N concentration in the solution increased. Decreasing the N-NO3: N-NH4 ratio increased the N uptake, but sharply decreased the uptake of cations, especially Ca.


Water ◽  
2020 ◽  
Vol 12 (11) ◽  
pp. 3292
Author(s):  
Xinqiang Du ◽  
Jing Feng ◽  
Min Fang ◽  
Xueyan Ye

As one of the largest agricultural areas, the Sanjiang Plain of Northeast China has faced serious inorganic nitrogen pollution of groundwater, but the sources and the formation mechanism of pollution in the regional shallow groundwater remain unclear, which constrains the progress of pollution control and agricultural development planning. An investigation on potential nitrogen sources, groundwater inorganic nitrogen compounds (NH4+, NO3−, NO2−), and topsoil total nitrogen concentration (TN) was conducted in a typical paddy irrigation area of Sanjiang Plain. Multivariate statistical analysis combined with geospatial-based assessment was applied to identify the sources, determine the governing influencing factors, and analyze the formation process of inorganic nitrogen compounds in shallow groundwater. The results show that the land use type, oxidation-reduction potential (Eh), groundwater depth, NO2− concentration, and electrical conductivity (EC) are highly correlated with the NO3− pollution in groundwater, while DO and Eh affected the distribution of NH4+ most; the high concentrations of NO3− in sampling wells are most likely to be found in the residential land and are distributed mainly in densely populated areas, whereas the NH4+ compounds are most likely to accumulate in the paddy field or the lands surrounded by paddy field and reach the highest level in the northwest of the area, where the fields were cultivated intensively with higher fertilization rates and highest values of topsoil TN. From the results, it can be concluded that that the NO3− compounds in groundwater originated from manure and domestic waste and accumulated in the oxidizing environment, while the NH4+ compounds were derived from N fertilization and remained steady in the reducing environment. NO2− compounds in groundwater were the immediate products of nitrification as a result of microorganism activities.


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