起伏地形中目标生物炭修正的土壤水分路径模型:生物炭对水流影响的分析

IF 1.6 Q4 ENVIRONMENTAL SCIENCES
Adam O'Keeffe, Erin Brooks, Chad Dunkel, Dev S. Shrestha
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引用次数: 0

摘要

生物炭对水文通量的影响是使用一个单一的坡面网格土壤水分路径(SMR)模型来估计的。五个网格单元与不同的斜坡线性排列,以模拟土壤剖面下有或没有限制层的小起伏山坡。按干土质量将浓度为0%、4%和7%的生物炭改良剂(红木锯末和小麦秸秆生物炭)施用于最上面的网格细胞。模拟的受限和非受限土壤剖面的水流曲线是用实测的帕卢斯河水流数据手动校准的。蒸散发、渗透、侧流、基流和径流都是每年模拟的。文献中两个通常报道的- 6和- 33 kPa的田间容量(FC)被用来评估生物炭的效果。−6 kPa时考虑的现场容量对应较高的含水率,因此比−33 kPa时FC到永久萎蔫点之间的储水容量更高。在−6 kPa FC下,生物炭有效地增加了系统的蒸散量,减少了系统的侧流量。生物炭改性提高了土壤孔隙度,提高了土壤和植物有效水分的持水量。这些机制影响了系统产生的流量,表明生物炭在限制和非限制土壤剖面中都有积极的结果。与−6 kPa FC相比,−33 kPa FC对生物炭改性的影响要小一个数量级;在较低的现场容量值下,孔隙度增加的影响较小。此外,过量施用粗质生物炭可能对土壤水分保持产生不利影响。这些发现表明,如果在本研究中施用少于7%的生物炭作为水管理策略,将取得积极的结果,但需要进一步探索不同生物炭和土壤性质的最佳生物炭水平。</p> /abstract>
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil moisture routing modeling of targeted biochar amendment in undulating topographies: an analysis of biochar's effects on streamflow

The effect of biochar on hydrologic fluxes was estimated using a single hillslope version of a gridded soil moisture routing (SMR) model. Five grid cells were aligned linearly with varied slopes to simulate a small undulating hillslope with or without a restrictive layer beneath the soil profile. Biochar amendments (redwood sawdust and wheat straw biochar) at concentrations of 0%, 4%, and 7% were applied to the topmost grid-cell by mass of dry soil. Simulated streamflow hydrographs for restricted and non-restricted soil profiles were manually calibrated with measured Palouse River streamflow data. Evapotranspiration, percolation, lateral flow, baseflow, and streamflow were all modeled yearly. Two generally reported field capacities (FC) in literature at −6 and −33 kPa were considered to assess the effect of biochar. Field capacity considered at −6 kPa corresponds to higher moisture content, and hence higher moisture storage capacity between FC and permanent wilting point than at −33 kPa. At −6 kPa FC, biochar effectively increased evapotranspiration and reduced the lateral flow of the system. Increased soil porosity from biochar amendment enhanced the water holding capacity of the soil and plant available water. These mechanisms impacted the streamflow generated from the system indicating positive outcomes from biochar amendment in both restricted and non-restricted soil profiles. Biochar amendment showed an order of magnitude smaller effects with −33 kPa FC compared to −6 kPa FC; the increased porosity appeared to be less influential at lower field capacity values. Additionally, the results showed that the over-application of coarse biochar might negatively affect retaining soil moisture. These findings point to positive results for using biochar as a water management strategy if applied less than 7% in this study, but further exploration is needed to find the optimum level of biochar with different biochar and soil properties.

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来源期刊
AIMS Environmental Science
AIMS Environmental Science ENVIRONMENTAL SCIENCES-
CiteScore
2.90
自引率
0.00%
发文量
31
审稿时长
5 weeks
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