地理研究 ›› 2019, Vol. 38 ›› Issue (11): 2778-2789.doi: 10.11821/dlyj020181424
赵海鹏1,4, 宋宏权1,2,3,4,*(), 刘鹏飞2,4, 李霄阳1,4, 王团徽1,4
收稿日期:
2018-12-26
修回日期:
2019-05-25
出版日期:
2019-11-20
发布日期:
2019-12-02
通讯作者:
宋宏权
作者简介:
赵海鹏(1995-),男,河南禹州人,硕士,研究方向为空间分析、地理建模。E-mail: 基金资助:
ZHAO Haipeng1,4, SONG Hongquan1,2,3,4,*(), LIU Pengfei2,4, LI Xiaoyang1,4, WANG Tuanhui1,4
Received:
2018-12-26
Revised:
2019-05-25
Online:
2019-11-20
Published:
2019-12-02
Contact:
SONG Hongquan
摘要:
中国北方干旱/半干旱区是全球主要的沙尘源区之一,风蚀造成的沙尘排放可导致大量的土壤有机质(SOM)与养分流失,并通过传输与沉降过程对其进行空间再分配,对空气质量、气候变化、植被生长及生物地球化学过程等具有重要影响。本文利用WRF/Chem(Weather Research Forecasting with Chemistry)v3.7.1大气化学传输模型,对1980—2015年间中国北方沙尘排放及其引起的SOM、全氮(TN)与全磷(TP)的时空变化过程进行了精细化模拟,探究了中国北方风蚀引起的SOM、TN与TP养分流失的时空变化特征。结果表明:① 1980—2015年来平均每年约有66.59 Tg的沙尘颗粒排放至大气;② 沙尘排放具有较大的时空差异,沙尘排放源区主要集中在新疆东部、内蒙古西部的巴丹吉林沙漠和腾格里沙漠等地区;③ 每年因沙尘排放引起的SOM、TN和TP流失量分别约为0.07 Tg、0.004 Tg和0.005 Tg;④ 1980—2015年间中国北方沙尘排放及其引起的SOM、TN与TP的流失量具有较强的年际波动,未呈现显著的趋势性变化特征。本研究对于认知风蚀在碳循环与养分循环过程中的作用,以及对深入了解中国北方的土地退化机理具有重要意义。
赵海鹏, 宋宏权, 刘鹏飞, 李霄阳, 王团徽. 1980—2015年风蚀影响下中国北方土壤有机质与养分流失时空特征[J]. 地理研究, 2019, 38(11): 2778-2789.
ZHAO Haipeng, SONG Hongquan, LIU Pengfei, LI Xiaoyang, WANG Tuanhui. Spatio-temporal variations of soil organic matter and nutrient losses resulted from wind erosion in northern China from 1980 to 2015[J]. GEOGRAPHICAL RESEARCH, 2019, 38(11): 2778-2789.
表2
WRF/Chem气象参数模拟结果评估"
气象参数(单位) | 季节 | 平均观测值 | 平均模拟值 | MB | NMB(%) | NME(%) | RMSE | R |
---|---|---|---|---|---|---|---|---|
T2 (℃) | 冬季 | -0.8 | -1.9 | -1.1 | -0.5 | 2.6 | 3.5 | 0.9 |
春季 | 6.1 | 5.2 | -0.9 | -15.1 | 37.9 | 3.4 | 0.9 | |
夏季 | 21.9 | 21.7 | -0.2 | -0.1 | 8.9 | 3.3 | 0.9 | |
秋季 | 18.7 | 17.8 | -0.9 | -4.6 | 9.3 | 3.1 | 0.9 | |
WSP10 (m/s) | 冬季 | 1.9 | 3.2 | 1.3 | 69.0 | 76.1 | 1.7 | 0.4 |
春季 | 2.5 | 3.5 | 1.0 | 43.0 | 51.1 | 1.5 | 0.5 | |
夏季 | 2.2 | 3.2 | 1.0 | 42.1 | 49.8 | 1.3 | 0.5 | |
秋季 | 1.9 | 2.9 | 1.0 | 49.4 | 56.4 | 1.3 | 0.5 | |
WDR10(°) | 冬季 | 210.5 | 190.1 | -20.4 | -12.7 | 46.9 | 189.0 | 0.2 |
春季 | 206.4 | 185.2 | -21.3 | -13.4 | 47.3 | 165.2 | 0.2 | |
夏季 | 201.5 | 167.3 | -34.2 | -15.6 | 47.3 | 194.7 | 0.2 | |
秋季 | 211.4 | 172.7 | -38.7 | -16.3 | 48.6 | 192.7 | 0.2 | |
PCP(mm/d) | 冬季 | 0.9 | 0.7 | -0.2 | -10.6 | 107.3 | 6.4 | 0.5 |
春季 | 2.8 | 2.4 | -0.4 | -17.2 | 97.8 | 9.5 | 0.4 | |
夏季 | 3.5 | 4.3 | 0.8 | 12.2 | 139.7 | 7.3 | 0.5 | |
秋季 | 1.8 | 2.1 | 0.3 | 7.2 | 123.6 | 8.5 | 0.3 |
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