Arid Zone Research ›› 2023, Vol. 40 ›› Issue (5): 747-755.doi: 10.13866/j.azr.2023.05.07
• Land and Water Resources • Previous Articles Next Articles
WEI Yajuan1,2(),LIU Meiying3,XIE Yunhu1(),LI Xing4
Received:
2023-02-06
Revised:
2023-03-22
Online:
2023-05-15
Published:
2023-05-30
WEI Yajuan, LIU Meiying, XIE Yunhu, LI Xing. Characteristics of soil nutrient accumulation after 38 years of the Jilantai Salt Lake protection system[J].Arid Zone Research, 2023, 40(5): 747-755.
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Tab. 1
Basic information of different protection system types"
防护体系类型 | 建植方式 | 恢复年限/a | 优势种 | 灌木 | 草本 | 盖度/% | 凋落物/(g·m-2) | ||||
---|---|---|---|---|---|---|---|---|---|---|---|
株高/cm | 冠幅/m2 | 密度/(株·hm-2) | 株高/cm | 密度/(株·m-2) | |||||||
流沙固阻带 | - | - | 沙米、白刺 | - | - | - | 5.65 | 3.12 | <10 | 0 | |
封沙育草带 | 自然恢复 | - | 白刺为主,其他植被有芦苇、苦豆子和披针叶野决明。 | 30.61 | 9.68 | 25.95 | 48.23 | 20.00 | 20 | 133.25 | |
防风阻沙带 | 人工植苗 | 36 | 沙枣、梭梭、沙拐枣、花棒 | 295.33 | 19.82 | 1666.7 | 15.20 | 6.00 | 58 | 310.01 | |
盐湖防护林带 | 人工植苗 | 36 | 沙枣、花棒、梭梭、柽柳 | 259.00 | 14.48 | 1111.1 | 28.00 | 9.62 | 45 | 223.14 |
Tab. 2
The effects of protection system types and soil depths on the increase of soil nutrient"
因素 | 指标 | SOC | TN | TP | AN | AP |
---|---|---|---|---|---|---|
防护体系类型 | F | 55.01 | 8.56 | 10.44 | 2.21 | 150.72 |
P | 0.000*** | 0.000*** | 0.000*** | 0.102 | 0.000*** | |
土层深度 | F | 70.18 | 52.33 | 136.97 | 35.73 | 56.76 |
P | 0.000*** | 0.000*** | 0.000*** | 0.000*** | 0.000*** | |
防护体系类型×土层深度 | F | 9.1 | 3.35 | 2.94 | 1.52 | 7.25 |
P | 0.000*** | 0.002** | 0.005** | 0.160 | 0.000*** |
Tab. 3
Effects of protection system type and soil depth on relative interaction intensity of soil nutrients"
因素 | 指标 | RIISOC | RIITN | RIITP | RIIAN | RIIAP | RII总 |
---|---|---|---|---|---|---|---|
防护体系类型 | F | 1.92 | 1.51 | 26.01 | 28.29 | 165.13 | 59.07 |
P | 0.141 | 0.228 | 0.000*** | 0.000*** | 0.000*** | 0.000*** | |
土层深度 | F | 18.15 | 58.70 | 107.67 | 25.00 | 6.81 | 56.53 |
P | 0.000*** | 0.000*** | 0.000*** | 0.000*** | 0.000*** | 0.000*** | |
防护体系类型×土层深度 | F | 10.03 | 5.20 | 6.62 | 10.71 | 13.23 | 10.03 |
P | 0.000*** | 0.000*** | 0.000*** | 0.000*** | 0.000*** | 0.000*** |
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