生态环境学报 ›› 2023, Vol. 32 ›› Issue (7): 1226-1236.DOI: 10.16258/j.cnki.1674-5906.2023.07.006
宫亮1,2(), 金丹丹1,2, 牛世伟1,2, 王娜1,2, 邹晓锦1,2, 张鑫1,2, 隋世江1,2, 解占军1,2, 韩瑛祚1,2
收稿日期:
2023-01-07
出版日期:
2023-07-18
发布日期:
2023-09-27
作者简介:
宫亮(1981年生),男,研究员,主要从事农业资源利用相关工作。E-mail: gongliang1900@sina.com
基金资助:
GONG Liang1,2(), JIN Dandan1,2, NIU Shiwei1,2, WANG Nan1,2, ZOU Xiaojin1,2, ZHANG Xin1,2, SUI Shijiang1,2, Xie Zhanjun1,2, HAN Yingzuo1,2
Received:
2023-01-07
Online:
2023-07-18
Published:
2023-09-27
摘要:
水稻生产是碳排放的主要来源,辽宁省是中国重要的优质水稻主产区,探明稻田减排固碳潜力对实现碳达峰碳中和具有重要意义。遵循《IPCC国家温室气体清单指南2019修订版》的基本框架和要求,按照《省级温室气体清单编制指南》规定,估算分析了辽宁省稻田减排固碳潜力。结果表明,辽宁省稻田CH4排放量(CO2-eqv)为2.13-3.39 Tg·a-1,N2O直接和间接排放量(CO2-eqv)分别为0.37-0.40 Tg·a-1和0.08-0.09 Tg·a-1。常规施肥碳排放总量(CO2-eqv)为2.61 Tg·a-1,优化施肥可减少碳排放(CO2-eqv)0.03 Tg·a-1,有机培肥和秸秆还田碳排放(CO2-eqv)分别增加0.42 Tg·a-1和1.36 Tg·a-1,具有明显的增排效应,稻田单位面积碳排放强度和单位产量碳排放强度均以秸秆还田最高,较常规施肥分别增加了49.96%-52.68%和50.30%-52.46%。稻田单位面积碳排放强度(CO2)以辽河三角洲稻区最高,达到5.17-8.08 t·hm-2·a-1。单位产量碳排放强度(CO2)则以东南部山地丘陵稻区最高,达到0.66-1.01 t·t-1·a-1。不同水稻主产区以辽河三角洲稻区碳(CO2-eqv)减排空间最大,达5.50×104-1.42×105 t·a-1,不同化学肥料以氮肥减施带来的碳(CO2-eqv)减排潜力最大,达0.18×104-1.20×105 t·a-1,不同养分管理措施以有机无机配施碳(CO2-eqv)减排空间最大,达3.78×104-1.42×105 t·a-1。有机无机配施和秸秆还田土壤固碳量(CO2-eqv)分别为0.10-0.28 Tg·a-1和0.22-0.65 Tg·a-1,其碳增排对土壤固碳抵消率分别为56.68%-82.52%和89.34%-99.03%,均能通过土壤固碳抵消其增加的碳排放。有机无机配施是辽宁省水稻生产碳减排最优养分管理措施。
中图分类号:
宫亮, 金丹丹, 牛世伟, 王娜, 邹晓锦, 张鑫, 隋世江, 解占军, 韩瑛祚. 辽宁省水稻田固碳减排潜力分析[J]. 生态环境学报, 2023, 32(7): 1226-1236.
GONG Liang, JIN Dandan, NIU Shiwei, WANG Nan, ZOU Xiaojin, ZHANG Xin, SUI Shijiang, Xie Zhanjun, HAN Yingzuo. Potential Analysis of Carbon Sequestration and Emission Reduction in Rice Fields in Liaoning Province[J]. Ecology and Environment, 2023, 32(7): 1226-1236.
水稻主产区 | 行政区域 | 气候条件 | 土壤类型 | 种植面积/ (104 hm-2) | 平均产量/ (t·hm-2) |
---|---|---|---|---|---|
辽河三角洲 稻作区 | 营口、盘锦、 锦州 | 水稻生长季平均气温在21 ℃以上, 降雨量在450-500 mm之间, 日照时长1100 h以上, ≥10 ℃活动积温在3700 ℃以上 | 盐渍型水稻土 | 18.46 | 9.5 |
辽宁中北部 平原稻作区 | 铁岭、沈阳、 辽阳、鞍山 | 水稻生长季平均气温在20-22 ℃之间, 降雨量在400-550 mm之间, 日照时长1100-1300 h, ≥10 ℃活动积温在3300-3800 ℃ | 草甸型水稻土 | 23.49 | 7.1 |
辽宁东南部部 山地丘陵稻作区 | 丹东、大连、 本溪、抚顺 | 水稻生长季平均气温在18-20 ℃之间, 降雨量在550-800 mm之间, 日照时长900-1000 h, ≥10 ℃活动积温在2000-3500 ℃ | 草甸型水稻土、 盐渍型水稻土 | 8.75 | 8.5 |
表1 辽宁省水稻主产区划分
Table 1 Division of main rice producing areas in Liaoning Province
水稻主产区 | 行政区域 | 气候条件 | 土壤类型 | 种植面积/ (104 hm-2) | 平均产量/ (t·hm-2) |
---|---|---|---|---|---|
辽河三角洲 稻作区 | 营口、盘锦、 锦州 | 水稻生长季平均气温在21 ℃以上, 降雨量在450-500 mm之间, 日照时长1100 h以上, ≥10 ℃活动积温在3700 ℃以上 | 盐渍型水稻土 | 18.46 | 9.5 |
辽宁中北部 平原稻作区 | 铁岭、沈阳、 辽阳、鞍山 | 水稻生长季平均气温在20-22 ℃之间, 降雨量在400-550 mm之间, 日照时长1100-1300 h, ≥10 ℃活动积温在3300-3800 ℃ | 草甸型水稻土 | 23.49 | 7.1 |
辽宁东南部部 山地丘陵稻作区 | 丹东、大连、 本溪、抚顺 | 水稻生长季平均气温在18-20 ℃之间, 降雨量在550-800 mm之间, 日照时长900-1000 h, ≥10 ℃活动积温在2000-3500 ℃ | 草甸型水稻土、 盐渍型水稻土 | 8.75 | 8.5 |
稻作区 | 推荐施肥量 | 习惯施肥量 | 化肥减施量 | 有机肥替代化肥量 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
N | P2O5 | K2O | N | P2O5 | K2O | N | P2O5 | K2O | N | P2O5 | K2O | ||||
辽河三角洲 | 234 | 111 | 101 | 271 | 117 | 96 | 37 | 6 | -5 | 47 | 35 | 40 | |||
辽东南山地丘陵 | 179 | 83 | 76 | 192 | 102 | 82 | 13 | 19 | 6 | 36 | 27 | 30 | |||
辽中北部平原 | 210 | 80 | 91 | 211 | 81 | 95 | 1 | 1 | 4 | 42 | 32 | 36 |
表2 不同稻作区肥料施用量
Table 2 Fertilizer partial productivity in different rice producing area kg·hm-2
稻作区 | 推荐施肥量 | 习惯施肥量 | 化肥减施量 | 有机肥替代化肥量 | |||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
N | P2O5 | K2O | N | P2O5 | K2O | N | P2O5 | K2O | N | P2O5 | K2O | ||||
辽河三角洲 | 234 | 111 | 101 | 271 | 117 | 96 | 37 | 6 | -5 | 47 | 35 | 40 | |||
辽东南山地丘陵 | 179 | 83 | 76 | 192 | 102 | 82 | 13 | 19 | 6 | 36 | 27 | 30 | |||
辽中北部平原 | 210 | 80 | 91 | 211 | 81 | 95 | 1 | 1 | 4 | 42 | 32 | 36 |
图6 不同养分管理条件下稻田碳增排与土壤固碳特征
Figure 6 Characteristics of carbon increase and release and soil carbon sequestration in rice field under different nutrient management conditions
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