Contribution of urban runoff in Taipei metropolitan area to dissolved inorganic nitrogen export in the Danshui River, Taiwan

2016 ◽  
Vol 24 (1) ◽  
pp. 578-590 ◽  
Author(s):  
Nae-Wen Kuo ◽  
Shih-Hao Jien ◽  
Nien-Ming Hong ◽  
Yao-Te Chen ◽  
Tsung-Yu Lee
2014 ◽  
Vol 11 (2) ◽  
pp. 2497-2536
Author(s):  
T.-Y. Lee ◽  
Y.-T. Shih ◽  
J.-C. Huang ◽  
S.-J. Kao ◽  
F.-K. Shiah ◽  
...  

Abstract. Dissolved inorganic nitrogen (DIN, including ammonium, nitrite and nitrate) export from land to ocean is becoming dominated by anthropogenic activities and severely altering the aquatic ecosystem. However, rare observational analyses have been conducted in the Oceania, the hotspot of global DIN export. In this study a whole watershed monitoring network (20 stations) was conducted in 2003 to investigate the controlling factors of DIN export in the Danshui River of Taiwan. The results showed that DIN concentration ranged from ∼16 μM in the headwater and up to ∼430 μM in the estuary. However, the dominating DIN species transformed gradually from NO3− in the headwater (∼97%) to NH4+ in the estuary (∼70%), which well followed the descending dissolved oxygen (DO) distribution (from ∼8 mg L−1 to ∼1 mg L−1). NO2− was observed in the transition zone from high to low DO. DIN yield was increasing downstream, ranging from ∼160 to ∼6000 kg N km−2 yr−1 as population density increases toward the estuary, from ∼15 pop km−2 to ∼2600 pop km−2. Although the individual DIN export, ∼2.40 kg N person−1 yr−1, was comparable to the global average, the close-to-top DIN yield was observed owing to abundant rainfall, dense population, and the sensitive response to population increase. The Danshui River occupies 1.8 × 10−3% of the land surface area of the Earth but discharges disproportionately high percentage, ∼60 × 10−3% (∼14 000 t N yr−1) of the annual global DIN export to the ocean. Through this study, regulating factors and the significance of human population on DIN export were identified, and the regional databases were supplemented to promote the completeness of global models.


2013 ◽  
Vol 38 ◽  
pp. 134-146 ◽  
Author(s):  
Peter K. Swart ◽  
William T. Anderson ◽  
Mark A. Altabet ◽  
Courtney Drayer ◽  
Sarah Bellmund

2014 ◽  
Vol 11 (19) ◽  
pp. 5307-5321 ◽  
Author(s):  
T.-Y. Lee ◽  
Y.-T. Shih ◽  
J.-C. Huang ◽  
S.-J. Kao ◽  
F.-K. Shiah ◽  
...  

Abstract. Human-induced excess nitrogen outflowing from land through rivers to oceans has resulted in serious impacts on terrestrial and coastal ecosystems. Oceania, which occupies < 2.5% of the global land surface, delivers 12% of the freshwater and dissolved materials to the ocean on a global scale. However, there are few empirical data sets on riverine dissolved inorganic nitrogen (DIN) fluxes in the region, and their dynamics are poorly understood. In this study, a river monitoring network covering different types of land uses and population densities was implemented to investigate the mechanism of DIN export. The results show that DIN concentration/yield varied from ∼20 μM/∼300 kg-N km−2 yr−1 to ∼378 μM/∼10 000 kg-N km−2 yr−1 from the relatively pristine headwaters to the populous estuary. Agriculture and population density control DIN export in less densely populated regions and urban areas, respectively, and runoff controls DIN at the watershed scale. Compared to documented estimates from global models, the observed DIN export from the Danshui River is 2.3 times larger, which results from the region-specific response of DIN yield to dense population and abundant runoff. The dominating DIN species change gradually from NO3− in the headwaters (∼97%) to NH4+ in the estuary (∼60%) following the urbanization gradient. The prominent existence of NH4+ is probably the result of the anaerobic water body and short residence time, unlike in large river basins. Given the analogous watershed characteristics of the Danshui River to the rivers in Oceania, our study could serve as a first example to examine riverine DIN fluxes in Oceania.


2011 ◽  
Vol 347-353 ◽  
pp. 2302-2307 ◽  
Author(s):  
Hong Xiang Wang ◽  
Yi Shi ◽  
Jian Ma ◽  
Cai Yan Lu ◽  
Xin Chen

A field experiment was conducted to study the characteristics of non-point source nitrogen (N) in the surface runoff from sloping croplands and the influences of rainfall and cropland slope gradient. The results showed that dissolved total N (DTN) was the major form of N in the runoff, and the proportion occupied by dissolved inorganic nitrogen (DIN) ranged from 45% to 85%. The level of NH4+-N was generally higher than the level of NO3--N, and averaged at 2.50 mg·L-1and 1.07 mg·L-1respectively. DIN was positively correlated with DTN (R2=0.962). Dissolved organic N (DON) presented a moderate seasonal change and averaged at 1.40 mg·L-1. Rainfall amount and rainfall intensity significantly affected the components of DTN in the runoff. With the increase of rainfall amount and rainfall intensity, the concentrations of DTN, NH4+-N and NO3--N presented a decreased trend, while the concentration of DON showed an increased trend. N loss went up with an increase in the gradient of sloping cropland, and was less when the duration was longer from the time of N fertilization.fertilization.


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