CHANGES IN VILLAGE-SCALE NITROGEN STORAGE IN CHINA'S TAI LAKE REGION

2000 ◽  
Vol 10 (4) ◽  
pp. 1074-1089 ◽  
Author(s):  
Erle C. Ellis ◽  
Rong Gang Li ◽  
Lin Zhang Yang ◽  
Xu Cheng
2009 ◽  
Vol 9 (5) ◽  
pp. 433-442 ◽  
Author(s):  
Song Li ◽  
Hua Li ◽  
Xingqiang Liang ◽  
Yingxu Chen ◽  
Zhihong Cao ◽  
...  

2011 ◽  
Vol 141 (1-2) ◽  
pp. 224-229 ◽  
Author(s):  
Yuhua Tian ◽  
Linzhang Yang ◽  
Bin Yin ◽  
Zhaoliang Zhu
Keyword(s):  

2008 ◽  
Vol 5 (6) ◽  
pp. 4867-4896
Author(s):  
L. Zhang ◽  
D. Yu ◽  
X. Shi ◽  
L. Zhao ◽  
W. Ding ◽  
...  

Abstract. China's paddy rice accounts for about 22% of the world's rice fields, therefore it is crucial to accurately estimate the CH4 emissions at regional scale to gauge their contribution to global greenhouse gas effect. This paper reports an application of a biogeochemical model, DeNitrification and DeComposition or DNDC, for quantifying CH4 emissions from rice fields in Tai-Lake region of China by linking DNDC to a 1:50 000 soil database, which was derived from 1107 paddy soil profiles in the Second National Soil Survey of China in the 1980s–1990s. The modeled results estimate that the 2.34 M ha of paddy rice fields in Tai-Lake region emitted about CH4 of 5.67 Tg C for the period of 1982–2000, with the average CH4 flux ranged from 114 to 138 kg C ha−1y−1. The highest emission rate (659.24 kg C ha−1 y−1) occurred in the subgroup of "gleyed paddy soils", while the lowest (90.72 kg C ha−1y−1) were associated with the subgroup "degleyed paddy soils". The subgroup "hydromorphic paddy soils" accounted for about 52.82% of the total area of paddy soils, the largest of areas of all the soil subgroups, with the CH4 flux rate of 106.47 kg C ha−1y−1. On a sub-regional basis, the annual average CH4 flux in the Tai-Lake plain soil region and alluvial plain soil region was higher than that in low mountainous and hilly soil region and polder soil region. The model simulation was conducted with two databases using polygon or county as the basic unit. The county-based database contained soil information coarser than the polygon system built based on the 1:50 000 soil database. The modeled results with the two databases found similar spatial patterns CH4 emissions in Tai-Lake region. However, discrepancies exist between the results from the two methods, the relative deviation is −42.10% for the entire region, and the relative deviation ranged from −19.53% to 97.30% for most counties, which indicates that the more precise soil database was necessary to better simulate CH4 emissions from rice fields in Tai-Lake region using the DNDC model.


Geoderma ◽  
2007 ◽  
Vol 142 (1-2) ◽  
pp. 136-141 ◽  
Author(s):  
Xiaomin Chen ◽  
Huashan Wu ◽  
Fei Wo

2015 ◽  
Vol 8 (3) ◽  
pp. 2653-2689 ◽  
Author(s):  
H. D. Zhang ◽  
D. S. Yu ◽  
Y. L. Ni ◽  
L. M. Zhang ◽  
X. Z. Shi

Abstract. Matching soil grid unit resolution with polygon unit map scale is important to minimize uncertainty of regional soil organic carbon (SOC) pool simulation as their strong influences on the uncertainty. A series of soil grid units at varying cell sizes were derived from soil polygon units at the six map scales of 1:50 000 (C5), 1:200 000 (D2), 1:500 000 (P5), 1:1 000 000 (N1), 1:4 000 000 (N4) and 1:14 000 000 (N14), respectively, in the Tai lake region of China. Both format soil units were used for regional SOC pool simulation with DeNitrification–DeComposition (DNDC) process-based model, which runs span the time period 1982 to 2000 at the six map scales, respectively. Four indices, soil type number (STN) and area (AREA), average SOC density (ASOCD) and total SOC stocks (SOCS) of surface paddy soils simulated with the DNDC, were attributed from all these soil polygon and grid units, respectively. Subjecting to the four index values (IV) from the parent polygon units, the variation of an index value (VIV, %) from the grid units was used to assess its dataset accuracy and redundancy, which reflects uncertainty in the simulation of SOC. Optimal soil grid unit resolutions were generated and suggested for the DNDC simulation of regional SOC pool, matching with soil polygon units map scales, respectively. With the optimal raster resolution the soil grid units dataset can hold the same accuracy as its parent polygon units dataset without any redundancy, when VIV < 1% of all the four indices was assumed as criteria to the assessment. An quadratic curve regression model y = −8.0 × 10−6x2 + 0.228x + 0.211 (R2 = 0.9994, p < 0.05) was revealed, which describes the relationship between optimal soil grid unit resolution (y, km) and soil polygon unit map scale (1:x). The knowledge may serve for grid partitioning of regions focused on the investigation and simulation of SOC pool dynamics at certain map scale.


2011 ◽  
Vol 25 (2) ◽  
pp. n/a-n/a ◽  
Author(s):  
D. S. Yu ◽  
H. Yang ◽  
X. Z. Shi ◽  
E. D. Warner ◽  
L. M. Zhang ◽  
...  

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