III. CEMA Applicability and Reasonableness of Costs

A. Background

General Work Order

Line No.

Damage

Remedy

Repairs Begun

Repairs Completed

Costs

94190

404

Rupture 2/14/98

1) Relocate

2/26/98

3/19/98

404K

94191

1004

1) Expose/
rupture 2/17/98

2) Landslide 3/26/98

1) Relocate

2) Install Caissons after relocated

2/18/98

3/19/98

376K

94192

1004

Exposed noted 2/9813

Relocate

3/2/98

3/19/98

250K

94194

404

Rupture 3/1/98

Relocate

3/3/98

3/23/98

228K

94195

406

Rupture 3/2/98

Relocate

3/3/98

3/20/98

257K

94197

1011

1) Expose 2/9 & 2/17/98
Shutdown 2/24/98
2) Expose right of way 2/98 or 3/98

1) Relocate Downward
2) Elevate pipe

5/1/98

6/30/98

350K

94198

1005

Expose 3/26/98

Relocate

4/7/98

5/19/98

440K

94377

1001
&404

Erosion Possibly 2/98 or 3/98

Elevate pipes

1/99 or
2/99

3/99 or
4/99

110K

TOTAL

         

2,415K

B. Applicability of CEMA to Recover Costs For Damage Attributed to the El Niño-Caused Storms

C. Scope of the Disaster

D. Damage Attributable to the 1998 El Niño Storms

The damage to these pipelines occurred from earth movement, e.g., landslides, that either ruptured the pipelines or exposed them. The Ventura mountain area where these pipelines are located is geologically described as having an underlying pico formation, which means that the mud or clay stone are very fine-grained sedimentary rocks that are weak and prone to earth movement, including landslides and soil creep. (Exh.17; Kenton, Tr. Vol. 1, pp. 73-75; 164-166.) Since at least 1969, contracting geologists have prepared maps of "unstable and potentially unstable areas" for SoCalGas. The maps are done to show landslide hazards along the pipeline routes and also to provide activity status based upon a review of historic aerial photos and site observations. (Id. at p. 69.) They show landslide activities in areas where SoCalGas' pipelines are located and delineate proposed alternate routes for pipelines that are adjacent to active landslides. The landslides are classified on a scale from active to inactive.

For the pipelines at issue in this case, SoCalGas has two maps, one of the area north of the Ventura River and the other of the area south of the Ventura River. (Exh. 10.) Both maps were created in 1969 and updated in 1981 or 1982, 1988, and 1992. The maps were updated again in 1999. The 1969, 1981, 1982, and 1988 maps were done by geologist Henry Neel and the 1992 and 1999 maps were done by geologist Frank Kenton after Mr. Neel retired. SoCalGas also maintains engineering maps showing specific pipeline locations and elevations.

Together with the mapping, the contract geologists also prepared reports containing their observations of the stability of the area traversed by SoCalGas pipelines and making recommendations for further action, including pipeline relocation. Reports were made in 1969, 1981, 1989, 1992, 1995 (limited) and 1998.

SoCalGas clearly had prior knowledge that these pipelines were situated in a geologically unstable area prone to earth movement and soil creep. Further, the record reflects that SoCalGas had prior knowledge of the risks to these specific pipelines damaged during the 1998 rains. The geologic maps and reports, at least back to 1969, show that all the damaged sections of the referenced pipelines, except for those portions of Lines 404 and 406 that cross through the Butler Property (Work Orders 94194 and 94195),15 were situated immediately adjacent to active landslides and were susceptible to future damage from such landslides. And, some of the pipelines had remedial work done because of damage from prior landslides.

The record reflects that SoCalGas also had prior knowledge of ways to mitigate the risks to these pipelines. In the mapping and reports prior to 1998, SoCalGas was advised of recommended alternate routes for relocating each of the damaged portions of the specified pipelines to prevent future damage, again with the exception of those portions of Lines 404 and 406 that cross through the Butler Property. And, despite its attempts to downplay the hazard presented by the adjacent landslides and to minimize the stated recommendations for pipeline relocation set forth on the maps and in the reports, after the 1998 damage occurred, SoCalGas, for the most part, relocated the portions of the damaged pipelines as originally recommended.16 In the one case where SoCalGas chose a different location (Line 1004-Work Order 94191), additional work had to be performed after the relocation was completed to stabilize the line and to protect the pipeline from further landslide activity.

SoCalGas contends that the damage to these pipelines was caused by landslides precipitated by the El Niño storm-related rainfall that occurred in 1998 and that these rains were so severe that land movement and pipeline damage from the storms could occur for a long time into the future. SoCalGas' argument is predicated upon its belief that the 1998 rainfall was "extraordinary." It points out that the 21.08 inches of rain that fell in February of 1998 was greater than the rainfall of any other month going back to 1957, and in fact was greater than the total annual rainfall occurring during 32 of the preceding 43 years. (Exhibit 21.) SoCalGas also argues that the total rainfall for January through May of 1998 (31.24 inches) was greater than that recorded during any other January through May time period and that the total annual 1998 rainfall (42.09 inches) was the largest annual rainfall recorded in this area by a margin of 8 inches.

SoCalGas points out that, while many factors contribute to landslides, they are particularly sensitive to rainfall. (Kenton, Tr. Vol. 1, pp. 75-79.) Landslides occur more frequently when there is a lot of rain, but once the earth becomes saturated, and the land begins to move, it will continue moving until its movement is blocked by a resisting force. (Id., at pp. 78-79.) If an area on a hillside has been subject to a landslide once, it is more prone to movement again. (Id., at pp. 164-166.)

Clearly, the February 1998 rainfall and, thus, the annual rainfall for water year 199817 was excessive. However, the Ventura County Department of Public Works' Hall Canyon rainfall gauge #167, as reflected on Exhibit 21, also shows that this area experienced excessive rainfall in several other years. For example, the area experienced double the average annual rainfall total in 1995, 1983, and 1978, as well as substantial rains greatly exceeding the average annual totals (over 50%) in 1993, 1986, 1980, and 1958. Most importantly, we note that January of 1995 was almost as wet as February of 1998 (17.33 inches v. 21.08 inches) and the January through May time period shows almost identical rainfall totals in 1995 (30.27 inches) and 1978 (31.08 inches), as experienced in 1998 (31.24 inches).While SoCalGas downplays the 1995 storms, it is clear that the 1995 rains were virtually equivalent in amount to the 1998 storms. The record reflects that SoCalGas sustained pipeline damage in 1995 from landslide activity on some of the same pipelines damaged in 1998, albeit to possibly different sections of pipe. Pipelines in geologically difficult areas, adjacent to active landslides, were impacted by landslides due to the 1995 rains, one on Lines 404 and 1011 in the microwave/Hall Canyon area, to the west of the area where the pipeline ruptured in 1998, and another on Line 1005 north of the Ventura River, in Mabranio Canyon. (Kenton, Tr. Vol. 1, pp. 81-82; 86; 89.) Despite these substantial rains in 1995 and the damage to some of pipelines in this area, SoCalGas' maps were not updated until 1999, after this proceeding was instituted. Nor is there any evidence that any comprehensive review of the pipelines was done after the rains of 1995 and prior to the damage that occurred in 1998.

SoCalGas' argument regarding the long lasting effects of heavy rains on earth movement, which it asserts for the time period post-1998, is equally applicable to prior time periods. Thus, it is clear that this naturally weak and unstable ground was saturated and subject to continuous creep for a substantial time prior to the 1998 rains. Given the nature of the 1995 rains, it is likely that the instability was greatly exacerbated at that time and that the effects would be felt in slides and continuous creep for extended years to come. It certainly would be felt in future periods of heavy rain, as was the case in 1998. The conclusion can then be drawn that the while the ruptures and exposures occurred during the 1998 rains, they were the result of the cumulative stresses of the earth movement that started much earlier.

The continuous movement of the land masses prior to 1998 also is established in the geologic reports and in some of the company's own Pipeline Patrol reports, particularly with respect to Lines 1011 and 404. SoCalGas' testimony that all of the damage, either exposure or rupture, to these pipelines was caused solely by rainfall occurring during the winter of 1997-1998 is not credible.

In view of the above, we find that SoCalGas had prior knowledge of the instability of the soil upon which these pipelines were located, the risks to the pipelines from landslides, particularly during rainy weather, and recommended mitigation measures to reduce or eliminate the potential for pipeline exposure or eruption. Specifically, it had knowledge about the landslide risks to pipelines 1004, 1005, 1011, and portions of 404. We have an insufficient record at this time to determine whether SoCalGas knew or should have known of the landslide risk to the portion of 404 that runs parallel to Line 406 through the Butler Ranch and direct that this issue be revisited in the cost-of-service proceeding.18 And, for the most part, after sustaining the damage from the landslides triggered by the rains in 1998, SoCalGas relocated the pipelines as recommended in previous geological reports. SoCalGas also had knowledge that future rains would pose an additional risk of pipeline damage, and, indeed, the prior rains, including the heavy rains in 1995, played a role in weakening the land that gave way and caused the pipeline damage in February and March of 1998.

The record reflects that the damage occurred on these lines in February and March of 1998 and were repaired, replaced, and relocated within a short time after the damage was discovered, with two exceptions: (1) Line 1011 (Work Order 94197); and (2) Lines 1011 and 404 (Work Order 94377). SoCalGas discovered damage to Line 1011 (Work Order 94197) in March of 1998 but did not begin repairs until May of 1998. SoCalGas did not give any explanation for the delay in making the repairs on this line. We have defined the disaster as continuing through May of 1998 and it could be inferred that the effects of the earlier rain were still being felt during the next few months. However, we have insufficient evidence upon which to base such a conclusion here. This is an issue that should be explored in SoCalGas' next cost-of-service proceeding.

We also have a substantial concern regarding the work performed on Lines 404 and 1011 as set forth on Work Order 94377. These two lines run parallel for some distance, descending from the ridge down the face of the slope to the city of Ventura. SoCalGas did not reference damage to these lines in its application and did not seek recovery for costs associated with such damage, even tއ0hq-RDfo6 9W_^ ?UǏCWIm\Sl{ǩd"ٖ?-&6n@~RtR1|/ݣeS3F6bJ2[H:6t,펧>(ɪt3zZȀ^74F8坶b,mIZȊffp@N1B$D_rlFQ=>Y`|RT#qh _bV$)\up4Z{];kMaqw]4?,9!9-^=y\-&K)WBNL,p7WXFH;&X#a̴芒Ij~B$S7k&ҳ2t[4 z s5m.v5;}"B齹%sKr.;aNqh2bחc[v6qMG smXXv$,XU"!_a+0sNTD^4>` dJv&IÜ0ĩ< ! z=p#QvƓhWͥ؟9hwyUG)BPXLIfg5ivc:v (ZO3bLe1&~ $gxn5$Ĉ8ՠx :.+OYJ|\TM1GUu &"wij &e}=hlfn~uIjlƛgI!v)Kc5=5YZZu_ㅛ%wt/ګ*GmO^D}?Ո.#ߤ%\[,zДh\4yC"JbAgmS u,@-U eTH]woy_b\X-k8y=1?qEAxj+'nP =qP`/SzxU`,_AOAu]6OAŋ,I^J%BZmG[Ann>LUU&[|xd}@-ۈ.w 7"BUŌf:" *Ktz\r,!Fki)[ʑ "wgWm wT uZT5*$,*LOT#)bY B=<'"ׇ&o4gsd~ETZl:FjC&ڇscؒS'tnM)}*Qi@!$_'-āoh5:~|%̜KG87%, wbhG0[ЪCvu@1be% dv#HfbAoڿ,so~/g ҭBuWL.ӎ+GjFمvYVkG{77}SZk'r;a#hjEpB;kي߈#f]OӠЃ&ٛ:l8%t9`rFR[IRU*;+8-`0ں<1= @8p PZS4aة"xVJQЀwA3UMSuzlOsBB.< }A@ _¾krMNF$mH%#.V5p~䫋֏NCt3PPǾ'ckMQcA6唃+St/R H fD^=rŐk3RMeS}]#g2\N2'ZX^TSmb#BSm% ?l|ŠR!{nb< dR^(kUyBeij0df8(+(}?'(e+7[Z4qr]5{PJ^!iu:M ˊӃ#[w}QP=쟲쁷qw]^B+MLffr nBTX6ڼP#u<9ЍfpUlZ"FKBԄL18GmP3yhNYokpQsj?Urе)*R቎v⻆;ځYE-dy@!5H B08y(!Ĩ=Bm7-_ps^:/@ve., a8!khUטG#^1_&Ls-U8Km=r~EEtIth/QR\إUM«뜊"ґILey*U̺j/d"F1VW'֢k1T-6/ 7?~zw'nv &O֋GGXqبF&-{_\JiX?XzQ&/7"H.vYS%*s`5p0nLe/@V FbpE̥%bYY,68D⫢MS7A敷@l:X %aM[ن}9Uh5E)-j-]r2´uQl=Ȃu/F H[gT?3ı:S,| O{*؆4e_kߍ,E4hC]>5 uc_Fh1 c(B{|EsBP+`Luvb6渉̔Cؖ0E\;8y?Wlu pgu"%qLX\CNu_ wGX!c9DcA8/^lֺ80fk\W*`c^ShF-ħb5t-kЈʯu+oNǤB-{u(]jG~Btʦ.0vLwVx^$Cjȹh[[3mK~ c#{/ڧ֡d?L>[ַeGm?X), aۈ%9w9|Y$"\3esYT<>t3 "iJP =1`qYv̞ҩBX/rs-R' D=qcY{rSL;zYl<ʛ 6=f Ɗ! !dbMɤ(-F@wQ:ku5\0b0㡨y nFA!(GR&RZ6kqd>cUIc)+95Z0ktmçFCUu"V-=N yy_N !nzֽAUF/|<Ւтڝ/$YDQU;ePm._KS|p2Ͽ~@ Cpt>S# ~i,@f9OL~F_I=f=W=?K+(ҕW3U8<@N%&>]˹#1I ~ևbfq."-)Y6)upvl3ucYm/&G3Ֆ$E+cN4o{S!1^ iF&/*&r{-䱐`  TEqΒ.er+Ȧ,oy @jit/ (`I)s4clgsbEbo?W&a ִIsjȩ}ጝg`=.\b$_Kݍ.1Z D;ѵq>>w. =gDUFn$cf ۂ~?~ F|3v{IϺD ˼irp"2J7!ےHS+ˋq|˟KuYcte`'_IΎ$hines that were exposed or ruptured should have been relocated or repaired prior to these storms. (Kenton, Tr. Vol. 2 at pp. 161-62.) SoCalGas notes that while previous practice had been to select possible future pipeline relocation routes in the event of future landslide activity, it now believes that it is more prudent to monitor landslide activity and only pick out a new route when necessary to do so.

While the landslide risks to these pipelines are well established on this record, it is not clear whether relocation of all or some of these pipelines, prior to 1998, would have been cost-effective. We recognize, as both SoCalGas and ORA point out, that relocating the pipelines in anticipation of declared disasters might be as expensive to ratepayers as the remedial measures they are intended to avoid because some relocated facilities ultimately may not be damaged and the reinforcement or relocation might not be sufficient to prevent future damage. However, we have no record in this proceeding upon which to make such a determination and are left with several key questions unanswered. As we observed earlier, ORA did not review the reasonableness of these expenditures from a cost causation, cost reduction or avoidance perspective, and no other party presented such data. As a result, we have an inadequate basis here upon which to determine if these costs could have been avoided or reduced, including whether some of the pipelines should have been relocated after the 1995 storms (or in any case before 1998). Further, because of the lack of evidence about cost causation, reduction and avoidance, we cannot determine whether these costs are reasonable and incremental to normal facility repair activity. We need to evaluate the costs recorded in SoCalGas' CEMA account in the context of overall costs already in rates in order to determine the extent to which the costs are or should be included in the risk built into existing rates. This further review is critical to our ability to fulfill our responsibility under P.U. Code § 454.9 to evaluate the reasonableness of these costs before authorizing their recovery.

Because of our concern with the lack of evidence on these key issues, and given the substantial evidence in the record regarding SoCalGas' knowledge of the risks to these pipelines, we cannot determine that the stipulation as presented is reasonable and in the public interest. Because we cannot decide these critical issues based on the current record, we reject the stipulation and direct the parties to more fully develop the record in SoCalGas' cost-of-service or PBR proceeding as described more fully below.20

Finally, we note that SoCalGas and TURN submitted extensive proposals for allocating the CEMA costs to customers. We need not address allocation here as we are not deciding the reasonableness of these costs.

While we reject the stipulation and deny recovery of the costs SoCalGas seeks to recover pursuant to the stipulation and the application under the CEMA, in this proceeding, we will give SoCalGas the opportunity to seek recovery of these costs, other than those specifically denied herein, in a future cost-of-service proceeding, for consideration of incorporation into rates post-2002. We will also permit SoCalGas to seek recovery of other capital costs incurred or that may be incurred that it attributes to the El Niño-driven storms, if it decides to pursue them, at that time.21 This includes future damage caused by further earth movement resulting from the removal of "resisting forces" occurring during the 1998 landslides and in the areas weakened by the 1998 storms. We intend to carefully scrutinize these costs in accordance with the principles set forth in this decision and to incorporate the record from this proceeding into our review.

This inquiry will address the reasonableness of specific costs SoCalGas seeks to recover in rates, including whether such costs should be forecast in cost-of-service proceedings or recovered after-the-fact through a reasonableness review proceeding such as through CEMA. Future cost-of-service proceedings should conduct a similar review of costs that SoCalGas seeks to recover that were incurred because of earth movement, using the principles set forth in this decision and any decision that is issued in the next cost-of-service proceeding on these issues.

For the specific costs SoCalGas has requested in this proceeding, it should provide information on the following issues so that we can determine the appropriateness and desirability of providing separate cost recovery for repair of these pipelines:

E. Future Consideration of the CEMA

12 An issue was also raised with respect to Work Order 74983 in the amount of $29,183 for relocation of a pipeline at the request of the city of Laguna Beach. SoCalGas contends that recovery is appropriate under the CEMA because the work was done at the request of a government official and because all of its franchise agreements have language that preclude it from recovering these costs from the franchisee. As we discuss further, this and other specific requests should be more fully evaluated in SoCalGas' next cost-of-service proceeding. 13 SoCalGas presented no documents showing when damage occurred. This date is based on SoCalGas' witness' statement that he thought the exposure was probably noted by a contractor while working on the portion of Line 1004 that ruptured. (Saline, Tr. V. 2 at pp. 190-91; 202.) 14 We considered this issue very briefly in Re Pacific Gas and Electric Company (1992) D.92-12-016; 46 CPUC2d 537; 1992 Cal. PUC Lexis 846. In that case we held that it was not in the public interest to grant PG&E's application to underground electric facilities in the Oakland/Berkeley hills fire area on an expedited basis and to book all costs of conversion to CEMA for future recovery from all ratepayers. (Id., at p. 12.) While we did allow the recovery of some funds through CEMA, we did so because of the unique circumstances and expressly held that our decision was not precedential. (Id. at pp. 33-34.) 15 SoCalGas produced no reports regarding these portions of Lines 404 and 406 and they were not depicted on either of the maps produced. 16 We also reject SoCalGas' witness' attempts to downplay the hazard presented and to minimize the recommendations for pipeline relocation set forth in the reports and on the maps because the documents were admitted into the record, without objection, and they speak for themselves. We do not credit SoCalGas' witness' contrary opinions to the extent that he purports to interpret the express language of the documents. 17 Water year is measured by the City of Ventura from October through September. 18 Despite repeated requests for information, geological reports, maps, and other data, we have been provided with virtually no information about the prior history of earth movement around these sections of pipeline. At the hearing, SoCalGas' witness Saline represented that there are no geological reports or assessments related to any damage on those lines in 1998 or prior and that there were no geological reports or surveys done on these lines 404 and 406 because there were no foreseeable problems in that area (Saline, Tr. Vol. 2, pp. 207-208). Mr. Kenton also testified that the ruptures were caused by a new landslide, from which we are supposed to infer that there were no active landslides adjacent to these sections of the pipelines. (Kenton, Tr. Vol. 2, pp. 149-150.) We would like to explore this issue further.

19 Another issue was presented with respect to Pipeline 1011. In his prehearing declaration, Mr. Saline testified that this pipeline was built in 1937. (Exh. 7.) For several years prior to 1996, SoCalGas had a "Special Pipeline Replacement Program," which identified and assessed various pipelines that were prone to leakage and susceptible to damage from earthquakes, including, specifically, transmission lines constructed prior to World War II located in urban areas. Based on a 1991 Value Chain Analysis (VCA), from 1993 through 1996, SoCalGas replaced or reclassified all pre-WWII pipelines, using replacement criteria that targeted pipelines in seismic hazard zones, areas of potential high consequence, e.g., close to hospitals, schools, high-density housing, and shopping, and Class 3 (high density urban) areas having a high flame potential.

20 Further, we cannot find, as argued by both ORA and SoCalGas, that approval of the stipulation would avoid further proceedings. As drafted, the stipulation only compromises specific capital costs purportedly related to the 1998 El Niño-driven storms from recovery in this CEMA proceeding. Given the ongoing nature of pipeline repairs necessitated by rain and landslides, and that the stipulation thus does not prevent SoCalGas from making future rate requests for other repairs, we believe this benefit has little merit. 21 While we will review the reasonableness of SoCalGas' expenses that it attributes to these storms, as reflected in the application, in the cost-of-service proceeding, we will not consider other later incurred costs that are characterized as expenses as opposed to capital costs at that time. 22 In proceeding, we may also determine whether we should make a similar review of SoCalGas' pipelines in other regions. We also note that SoCalGas recovered the capital costs for repairs and relocation of the two lines damaged in the 1995 rains by including the costs in its PBR rate base. (D.97-07-054; Exh. 24.) There is no indication that any inquiry was made at this time regarding the nature of the damage or the desirability of budgeting for preventative pipeline repairs or relocations.

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